Fossil fuels, which include petroleum, natural gas, and coal, supply nearly 90 percent of the energy needs of the United States and other industrialized nations. Because of their high demand, these nonrenewable energy resources are rapidly being consumed. Coal supplies are expected to last about a thousand years.


We must find other sources of energy to meet the increasing fuel demands of modern society. Important alternate sources of energy include: solar, wind, biomass, hydroelectric, geothermal, nuclear, and tidal energy.


One of the benefits of using alternate sources of energy is that many of them are “clean.” This means that they do not cause pollution. Also, many alternative energy sources are renewable energy sources. They are replaced naturally-such as plant life-or are readily available – such as the sun and wind. In addition, the use of renewable forms of energy will allow us to stretch out our current supply of fossil fuels so they will last longer.


In this chapter you will learn how biomass, or organic matter, can be an important energy source. Plants are the most important biomass energy source. Plant material can be burned directly-as with wood-or it can be converted into a fuel by other means. In the experiments that follow you will explore: how water can be heated by composting grass, how a peanut burns, and how corn syrup can be made into ethyl alcohol.
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Materials


  • Freshly cut grass clippings
  • Cooking thermometer (optional)
  • Empty two-liter plastic drink bottle
  • Rake
  • Water
  • Styrofoam cup

Procedure


Ask an adult to help you collect freshly cut grass clippings. You will need enough grass clippings to fill about two large grocery bags. Rake the grass clippings into a pile on a shady spot in the yard. In some parts of the country you will only be able to do this in the spring and summer months when grass grows.


Fill a two-liter plastic bottle with cold water. Starting at the top of the pile dig a hole down into the grass clippings just large enough for the plastic bottle. Place the plastic bottle in the hole, and then fill around it with grass clippings. The top of the plastic bottle should stick out of the pile of grass clippings slightly.


Check the water in the bottle after it has been in the pile of grass clipping for at least twenty-four hours. If you have a cooking thermometer, place it in the bottle for thirty seconds and then read the temperature on the thermometer. If you do not have a cooking thermometer, carefully remove the bottle of water from the pile of grass clippings. Feel the sides of the plastic bottle. CAUTION-THE BOTTLE MAY BE VERY WARM, SO AVOID BURNING YOURSELF. Pour some of the water into a Styrofoam cup and look for water vapor rising from the cup. Place the bottle back into the pile of grass clippings and check it again each day for several days.


Observations


After twenty-four hours in the grass clippings, is the water in the plastic bottle warm when you check it? If you check the water with a thermometer, what is the temperature of the water?


When you pour some of the water into a Styrofoam cup, do you see water vapor rising from the cup?


How many days does the water remain warm?


Does the pile of grass clippings become smaller after a few days? What does the pile of grass clippings look like when the water is no longer warm?


Discussion


The water in the plastic bottle should be warm after the bottle has been in the pile of grass clippings for twenty-four hours. The heat that warms the water comes from the pile of grass clippings, which is decomposing or composting.


The decomposition of dead plant and animal material is nature’s way of recycling important chemical substances. Complex chemical substances in dead plant and animal material are broken down into simple chemical substances during the process. These simpler chemical substances then become nutrients for living plants and soil animals.


Heat is given off during the decomposition process. The more material that is decomposing, the more heat is produced. In this experiment, a large amount of heat is given off by the decomposing grass clippings. This is because you started with a large pile of grass clippings, and grass clippings decompose quickly.


A pile of decomposing grass clippings can reach a temperature of over 71°C (160°F). The water in the bottle may absorb enough heat from the decomposing grass to reach a temperature as high as 60°C (140°F) after a day or two. For comparison, most household hot water heaters are set to deliver hot water with a temperature between 54°C (130°F) and 71°C (160°F).


Other Things to Try


How much water can you heat with composting grass clippings? To find out, repeat this experiment with a one-gallon plastic milk jug filled with water. Does the water in the jug become warm?


Repeat this experiment, but remove the bottle of water from the pile of grass clippings after twenty-four hours. Fill a second two-liter plastic bottle with cold water from a sink faucet and place it into the pile of grass clippings. Does the water in this bottle become warm after a couple of hours?


Is there a minimum amount of grass clippings that are needed to make enough heat to heat the water in a two-liter plastic bottle? To find out, surround a two-liter plastic bottle filled with water with just enough grass clippings to cover it. Does the water become warm after twenty-four hours?
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A peanut is not a nut, but actually a seed. In addition to containing protein, a peanut is rich in fats and carbohydrates. Fats and carbohydrates are the major sources of energy for plants and animals.


The energy contained in the peanut actually came from the sun. Green plants absorb solar energy and use it in photosynthesis. During photosynthesis, carbon dioxide and water are combined to make glucose. Glucose is a simple sugar that is a type of carbohydrate. Oxygen gas is also made during photosynthesis.


The glucose made during photosynthesis is used by plants to make other important chemical substances needed for living and growing. Some of the chemical substances made from glucose include fats, carbohydrates (such as various sugars, starch, and cellulose), and proteins.


Photosynthesis is the way in which green plants make their food, and ultimately, all the food available on earth. All animals and nongreen plants (such as fungi and bacteria) depend on the stored energy of green plants to live. Photosynthesis is the most important way animals obtain energy from the sun.


Oil squeezed from nuts and seeds is a potential source of fuel. In some parts of the world, oil squeezed from seeds-particularly sunflower seeds-is burned as a motor fuel in some farm equipment. In the United States, some people have modified diesel cars and trucks to run on vegetable oils.


Fuels from vegetable oils are particularly attractive because, unlike fossil fuels, these fuels are renewable. They come from plants that can be grown in a reasonable amount of time.
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Materials


  • Shelled peanut
  • Small pair of pliers
  • Match or lighter
  • Sink


Download Student Worksheet & Exercises


Procedure


ASK AN ADULT TO HELP YOU WITH THIS EXPERIMENT. DO NOT DO THIS EXPERIMENT BY YOURSELF. The fuel from the peanut can flare up and burn for a longer time than expected.


Close the drain in the kitchen sink. Fill the sink with water until the bottom of the sink is just covered.


Using a small pair of pliers, hold the peanut over the sink containing water. Ask an adult to hold the flame of a lit match or lighter directly under the peanut. When the peanut starts to burn, the lit match or lighter can be removed.


Allow the peanut to burn for one minute. MAKE SURE AN ADULT REMAINS PRESENT AND MAKE SURE TO HOLD THE PEANUT OVER THE SINK. To extinguish the burning peanut, drop it into the water. After you have extinguished the peanut, allow it to cool and then examine it carefully.


Observations


How long does it take for the peanut to start to burn? Does the peanut burn with a clean flame or a sooty flame? What color is the flame? What color does the peanut turn when it burns? Did the size of the peanut change after it has burned for several minutes?


Discussion



You should find that the peanut ignites and burns after a lit match or lighter is held under it for a few seconds. Although you only let the peanut burn for one minute as a safety measure, the peanut would burn for many minutes.


In this experiment, when the peanut burns, the stored energy in the fats and carbohydrates of the peanut is released as heat and light. When you eat peanuts, the stored energy in the fats and carbohydrates of the peanut is used to fuel your body.


Other Things to Try


Hold one end of a piece of uncooked spaghetti in a pair of pliers. Ask an adult to hold the flame of a lit match or lighter under the other end of the spaghetti. When the spaghetti starts to burn, place it in an aluminum pie pan that is in the sink. Make sure to extinguish the burning spaghetti with water when you are finished with the experiment. How does the burning of the spaghetti compare with the burning of the peanut?


Exercises 


  1. What is the process called where plants get food from the sun?
    1. Osteoporosis
    2. Photosynthesis
    3. Chlorophyll
    4. Metamorphosis
  2. Where does all life on the planet get its food?
  3. List two ways that we could use the energy in a peanut:

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Yeast is a simple living organism that can break down sugars into ethyl alcohol (ethanol) and carbon dioxide. The process by which yeast breaks down sugars into ethyl alcohol and carbon dioxide is called fermentation.


The tiny gas bubbles rising in the liquid mixture in the bottle are carbon dioxide gas bubbles that are made during the fermentation. The balloon on the bottle expands and becomes inflated because it traps the carbon dioxide gas being produced.


The ethyl alcohol that is made during fermentation stays in the liquid mixture. When fermentation is finished, the liquid mixture usually contains about 13 percent ethyl alcohol. The rest of the liquid is mostly water.


The ethyl alcohol can be concentrated by a process called distillation. During distillation, the liquid fermentation mixture is heated to change the ethyl alcohol and some of the water into a vapor. The vapor is then cooled to change it back into a liquid. This distilled liquid contains 95 percent ethyl alcohol and 5 percent water. The remaining water can be removed by special distillation methods to give pure ethyl alcohol.


In some areas of the United States, ethyl alcohol is blended with gasoline to make a motor fuel known as gasohol. About 8 percent of the gasoline sold in the United States is gasohol.


Gasohol burns more cleanly than pure gasoline. This results in fewer pollutants being released into the air. The use of gasohol as a motor fuel is particularly important in cities that have a lot of smog.


Corn syrup is a mixture of simple and complex sugars and water. It is made by breaking down the starch in corn into sugars. The process is called digestion. In this experiment you changed the sugars in corn syrup using yeast. Much of the ethyl alcohol used to prepare gasohol is made by fermenting corn and corn sugar.


Over one billion gallons of ethyl alcohol are made each year by fermentation of sugars from grains such as corn. Ethyl alcohol is a renewable energy source when it is made by fermenting grains such as corn. This is because the grains, such as corn, are easily grown.


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Materials


  • One package of yeast
  • Balloon
  • Water
  • Measuring spoons
  • Corn syrup
  • Measuring cup
  • Empty, two-liter plastic drink bottle
  •  Funnel (optional)
  • Sink or bucket


 Procedure


Remove the paper label from around an empty, two-liter, plastic drink bottle. Add two cups of water and one package of yeast to the bottle. Swirl the bottle to mix the water and yeast.


Next, add one-quarter cup of corn syrup to the bottle. You may want to use a small funnel to help you add the corn syrup to the bottle. Swirl the bottle to mix the contents.


Place a deflated balloon over the neck of the bottle. Make sure the balloon fits securely over the neck. Place the bottle in a sink or bucket. Check the bottle and balloon after two hours, and then again after four hours. Finally, check the bottle and balloon after twenty-four hours.


When you have finished with the experiment, pour the contents of the bottle down the sink. Then rinse the bottle and sink with water.


Observations


What color is the yeast mixture? Does the balloon start to inflate after an hour or two? Can you see gas bubbles rising to the surface of the yeast mixture? Does the balloon grow larger with time?


Discussion


You should find that soon after you mix together the yeast, water, and corn syrup, changes start to take place in the bottle. You should notice that a foam forms on top of the liquid mixture. You should also see tiny gas bubbles rising to the surface of the liquid. Also, you should notice that the balloon begins to inflate and become large.


Other Things to Try


Repeat this experiment using one tablespoon of table sugar instead of corn syrup. You should find that yeast can also ferment table sugar into ethyl alcohol and carbon dioxide. Table sugar is made from sugar cane and sugar beets. Since sugar cane and sugar beets are renewable plants, ethyl alcohol made from fermenting sugar from these plant products is another renewable energy source.


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penny-structureThe atoms in a solid, as we mentioned before, are usually held close to one another and tightly together. Imagine a bunch of folks all stuck to one another with glue. Each person can wiggle and jiggle but they can’t really move anywhere.


Atoms in a solid are the same way. Each atom can wiggle and jiggle but they are stuck together. In science, we say that the molecules have strong bonds between them. Bonds are a way of describing how atoms and molecules are stuck together.


There’s nothing physical that actually holds them together (like a tiny rope or something). Like the Earth and Moon are stuck together by gravity forces, atoms and molecules are held together by nuclear and electromagnetic forces. Since the atoms and molecules come so close together they will often form crystals.


Try this experiment and then we will talk more about this:
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Here’s what you need:


  • 50 pennies
  • ruler


 
Download worksheet and exercises


Lay about 20-50 pennies on the table so that they are all sitting flat on the table. Now, use the ruler (or your hand) to push the pennies toward one another so that you have one big glob of pennies on the table all touching one another. Don’t push so hard that they pile on top of one another. Just get one nice big flat blob of pennies.


Pretty simple huh? However, take a look at the pennies, do you notice anything? You may notice that the pennies form patterns. How could that happen? You just shoved them together you didn’t lay them out in any order. Taa daa! That’s what often happens when solids form.


The molecules are pulled so close to one another that they will form patterns, also known as matrices. These patterns are very dependent on the shape of the molecule so different molecules have a tendency to form different shaped crystals. Salt has a tendency to be “cubey”. Go take a look… and you’ll find that they are like little blocks!


Water has a tendency to from triangle or hexagon shapes which is why snowflakes have six sides. Your pennies also form a hexagon shape. Solids don’t always form crystals but they are more common than you might think. A solid that’s not in a crystalline form is called amorphous. Before you put your pennies away I want you to notice one more thing.


Here’s what you do:


1. Take your pennies and lay them flat on the table.


2. Push them together so they all touch without overlapping.


3. Place your ruler on the right hand side of your penny blob so that it’s touching the bottom half of your pennies.


4. Slowly push the ruler to the left and watch the pennies.


You may have noticed that the penny “crystal” split in quite a straight line. This is called cleavage. Since crystals form patterns the way they do they will tend to break in pretty much the same way you saw your pennies break.


Break an ice cube and take a look. You may see many straight sections. This is because the ice molecules “cleave” according to how they formed. The reason you can write with a pencil is due to this concept. The pencil is formed of graphite crystal. The graphite crystal cleaves fairly easily and allows you to write down your amazing physics discoveries!


(The image here is a graphite crystal.) [/am4show]


Crystals are formed when atoms line up in patterns and solidify.  There are crystals everywhere — in the form of salt, sugar, sand, diamonds, quartz, and many more!


To make crystals, you need to make a very special kind of solution called a supersaturated solid solution.  Here’s what that means: if you add salt by the spoonful to a cup of water, you’ll reach a point where the salt doesn’t disappear (dissolve) anymore and forms a lump at the bottom of the glass.


The point at which it begins to form a lump is just past the point of saturation. If you heat up the saltwater, the lump disappears.  You can now add more and more salt, until it can’t take any more (you’ll see another lump starting to form at the bottom).  This is now a supersaturated solid solution.  Mix in a bit of water to make the lump disappear.  Your solution is ready for making crystals.  But how?


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Here’s what you need:


  • pencil or wooden skewer
  • string
  • glass jar (cleaned out pickle, jam or may jars work great)
  • 8 cups of sugar
  • 3 cups water
  • paper clip
  • adult help and a stove
  • food coloring  is optional but fun!

If you add something for the crystals to cling to, like a rock or a stick, crystals can grow.  If you “seed” the object (coat it with the stuff you formed the solution with, such as salt or sugar), they will start forming faster. If you have too much salt (or other solid) mixed in, your solution will crystallize all at the same time and you’ll get a huge rock that you can’t pull out of the jar.  If you have too little salt, then you’ll wait forever for crystals to grow. Finding the right amount takes time and patience.



 
Download Student Worksheet & Exercises


1. If you plan on eating the sugar crystal when you’re done you probably want to boil water with the jar and the paper clip in it to get rid of any nasties. Be careful, and don’t touch them while they are hot.


2. Tie one end of the string to the pencil and the opposite end to the paper clip.  (You can alternatively use a skewer instead of a piece of string to make it look more like the picture above, but you’ll need to figure out a way to suspend the skewer in the jar without touching the sides or bottom of the jar.)


3. Wet the string a bit and roll it in some sugar. This will help give the sugar crystals a place to start.


4. Place the pencil across the top of the jar. Make sure the clip is at the bottom of the jar and that the string hangs straight down into the jar. Try not to let the sting touch the side of the jar.


5. Heat 3 cups of water to a boil


6. Dissolve 8 cups of sugar in the boiling water (again be careful!). Stir as you add. You should be able to get all the sugar to dissolve. You can add more sugar until you start to see undissolved bits at the bottom of the pan.  If this happens, just add a bit of water until they disappear.


7. Feel free to add some food coloring to the water.


rockcandy8. Pour the sugar water into the jar. Put the whole thing aside in a quiet place for 2 days to a week. You may want to cover the jar with a paper towel to keep dust from getting in.


You should see crystals start to grow in about 2 days. They should get bigger and bigger over the few days. Once you’re happy with how big your crystals get, you can eat them! It’s nothing but sugar! (Be sure to brush your teeth!)  This one (left) us about 6 months old.


There you go! Next time you hold a pencil, throw a ball, or put on a shoe try to keep in mind that what you’re doing is using an object that is made of tiny strange atoms all held tightly together by their bonds.


[/am4show]


Popcorn rocks are different than regular dolomite samples because they have a lot more magnesium inside. This was first discovered by a geology professor in the 1980s who was dissolving the limestone around fossils he was studying in his rock samples. When he placed samples of this type in the acid to dissolve, it didn’t dissolve but instead grew new crystals!


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Materials:


  • “Flowering Rock” dolomite samples
  • Distilled white vinegar (acetic acid)
  • Disposable cup or glass jar
  • Penny
  • Nail
  • Streak plate
  • Water in a graduated container
  • Scale that measures in grams
  • Longwave UV light source
  • Sunlight


Download worksheet and exercises


Dolomite is made of calcium magnesium carbonate (CaMg(CO3)2 and is both a mineral and a rock. Dolomite comes in all kinds of colors, including white, gray, pink, peach, yellow and orange … even colorless. Dolomite gives a white streak, which is hard to see on a white streak plate, and the hardness ranges from 3.4 to 4 on the Moh’s hardness scale. Specific gravity for dolomite is 2.8 to 3, with a vitreous (glassy), pearly luster and rhombohedra cleavage on two planes and conchoidal fracture on the third. It’s brittle (think tenacity), and is usually found around limestone. Dolomite is a chemical rock, since it reacts to acid. Dolomite fluoresces bluish-white when placed under a longwave UV light, and pink when exposed to a shortwave UV light.


  1. You’re first going to classify dolomite and test it for certain properties, and then you’ll grow crystals all over it. If you don’t have a UV light, skip it and perform the rest of the tests.
  2. Complete the first data table for the sample before following the instructions on the video. You are looking for the color, streak, hardness, density, luster, cleavage, fracture, tenacity, acid reaction, and fluorescence.
  3. Don’t wash your dolomite sample. You want the dust layer on top so the crystals start growing more quickly.
  4. Place the sample in your glass jar.
  5. Pour the vinegar into the cup (not directly on your sample) until it’s nearly submerged.
  6. Move your experiment to a warm location.
  7. Observe your rock formation over the next week and record your observations in the second data table. You can opt to take pictures and paste them into the data table.
  8. When all the vinegar has evaporated, remove the sample and put on display (after recording your last observation).

Exercises


  1. What would happen if you warmed the vinegar first, and placed it on a heating pad during your experiment?
  2. What is it in the dolomite samples that make the aragonite crystals grow?
  3. What else can you try instead of vinegar?

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Luster is the way a mineral reflects light, and it depends on the surface reflectivity.


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Materials


  • Sunlight
  • Rock samples (in the video: pyrite, fluorite, and serpentine)


Download worksheet and exercises


Every mineral has a particular luster, but some have different luster on different samples. Since it’s gauged by eye and not a scientific instrument, there’s quite a lot to be left to the observer when describing it. Luster is not usually used to identify minerals, since it’s so subjective.


That said, it is useful when describing a sample’s surface, so hold up yours to the light and use the descriptions below to find the one that best describes what you see.


  • Metallic or splendent luster are found in highly reflective minerals, like gold.
  • Submetallic luster is found in minerals that have a similar luster to metal, but it’s a bit duller and less reflective. These minerals are opaque and reflect light well. You’ll find submetallic luster in the thin splinter sections of minerals, such as sphalerite, cinnabar, and cuprite.
  • Vitreous or glassy luster describes 70% of all minerals, and they have the luster of glass. Quartz, calcite, topaz, beryl, tourmaline, and fluorite are examples of glassy luster.
  • Adamantine lusters (brilliant, like a cut diamond) are for transparent materials that show a very bright shine because they have a high refractive index.
  • Resinous lusters are usually yellow, orange, or brown minerals that have high refractive indices (like the way sunlight goes through honey).
  • Silky lusters have very fine fibers aligned in parallel, so it looks like a cloth of silk. Minerals like asbestos, ulexite, and a variety of gypsum called satin spar all have silky luster. If a sample has fibrous luster, it is coarser than a silky luster.
  • Pearly luster minerals look like the way light reflects off pearls, like the inside an oyster shell. These types of minerals have perfect cleavage, like muscovite and stilbite. Mica also has a pearly luster. Some pearly luster minerals also have an iridescent hue.
  • Greasy or oily luster looks like fat, and is found in minerals that have a lot of microscopic inclusions, like opal and cordierite. Most greasy luster minerals also feel oily.
  • Pitchy luster looks a lot like tar, and is found in radioactive minerals.
  • Waxy luster resembles wax, the way jade and chalcedony look on their surface.
  • Dull or earthy luster minerals have very little or no luster at all, because they have a surface that scatters the light in all directions, like with Kaolinite. Some geologists say that earthy luster means less luster than dull, but it’s really a close call between the two.

When light strikes a surface, it can be reflected off the surface, like a mirror, or it can pass through, like a window, or both. Metallic luster has most of the light bouncing off the surface, whereas calcite has most passing through the mineral. When light travels through a mineral, it refracts, or changes speed, as it crosses the new material boundary. This is what makes the luster appear different for different materials.


Refraction is how light bends when it travels from one substance to another. When light moves through a prism, it bends, and the amount that it bends is seen as color that comes out the other side. Each color represents a different amount of bending that it went through as it traveled through the prism.


  1. Label and number each of your samples and record this on your data table.
  2. Hold your mineral in the sunlight.
  3. Use the list to find the word that best describes what you see. Look particularly on your sample for a surface that is clean and not tarnished, discolored, or coated. Look at cleaved surfaces and on uneven parts.
  • Metallic
  • Submetallic (duller than metallic)
  • Vitreous or glassy
  • Adamantine (like a cut diamond)
  • Resinous (like honey)
  • Silky (like a silk cloth)
  • Pearly
  • Greasy or oily
  • Pitchy (like tar)
  • Waxy (like a candle)
  • Dull or earthy
  1. Record your observations in the data table.

Exercises


  1. What is refraction?
  2. Feldspar has perfect cleavage on two surfaces but fractured on a third. What kind of luster would you say it has?
  3. What type of luster is found on mica?

[/am4show]


Tenacity is a measure of how resistive a mineral is to breaking, bending, or being crushed. When you exceed that limit, fracture is how the mineral breaks once the tenacity (or tenacious) limit has been exceeded.


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Materials


  • Hammer (if your piece of coal is large)
  • Rock samples (in the video: copper, mica, selenite, sulfur)


Download worksheet and exercises


Tenacity is a measure of how a mineral behaves when under stress, like being crushed, bent, torn, or hammered. Minerals will react differently to each type of stress. Minerals can have more than one type of tenacity, since it’s possible for a mineral to have different (or several at the same time) reactions to the stress. Here’s a way to classify their response to stress:


  • Brittle: The sample crumbles or turns into a powder. Most minerals are brittle, like quartz.
  • Sectile: These minerals can be separated with a knife, like wax, like gypsum.
  • Malleable: When you hammer the mineral and it flattens instead of breaks, it’s malleable like silver and copper.
  • Ductile: A mineral that can be stretched into a wire is called ductile. All true metals are ductile, like copper and gold.
  • Flexible-Inelastic: When you bend a mineral and release it, it stays in the new shape. It was flexible enough to bend, but it didn’t snap back into its original shape when released, like copper.
  • Flexible-Elastic: When you bend a mineral and release it, it springs back into its original shape. Minerals that are flexible-elastic are fibrous, like chrysotile serpentine.
  1. Label and number each of your samples with your data table.
  2. Use a hammer and try to break the copper sample. Make sure you do this on a hard surface (like the concrete) so you don’t damage your floor or table!
  3. To test for brittleness, like for sulfur, do a scratch test to see if it leaves a fine powder. Use your streak plate if you think your specimen has a hardness of less than 7.
  4. For sectile tenacity, like with mica, carefully insert a knife into the mineral to see if it goes through. If the knife can penetrate through the sample (be careful with this!), then it’s sectile.
  5. To check for flexibility, like mica and selenite, use only slight pressure so you don’t break your sample. Notice if the sample springs back or retains its new shape when released.
  6. Complete the data table with your observations.

Exercises


  1. What are four different types of tenacity?
  2. How is elastic different from inelastic tenacity?
  3. How many types of tenacity can a mineral have?

[/am4show]


By the end of this lab, you will be able to line up rocks according to how hard they are by using a specific scale. The scale goes from 1 to 10, with 10 being the hardest minerals.
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Materials


  • Steel nail
  • Penny
  • Small plate of glass (optional)
  • Rock samples (minerals in the video: talc, selenite, calcite, fluorite, apatite, feldspar, quartz)


Download worksheet and exercises


The sample’s hardness is determined by trying to scratch and be scratched by known materials, like pennies, steel, glass, and so forth. If the material leaves a mark on the mineral, then we know that the material is harder than the mineral is. We first start with a fingernail since it’s easy to use and very accessible. If it leaves a mark, that means that your fingernail is harder than the mineral and you know it’s pretty soft. Talc is one of the softest minerals, making it easy to scratch with your fingernail.


However, most minerals can’t be scratched with a fingernail, so we can try other objects, like copper pennies (which have a hardness of 2.5-3.5), steel nail (3.5-5.5), steel knife (5.5), and even quartz (7). The most difficult part of this experiment is keeping track of everything, so it’s a great opportunity to practice going slowly and recording your observations for each sample as you go along.


  1. Number your samples on the data table and place each rock on the table. If you have the same samples listed above, you can scratch each rock with every other rock to find where they are on the Mohs’ Hardness Scale, where 1 is the softest and 10 is the hardest:
    Mohs’ Scale of Hardness Talc


    1. Selenite
    2. Calcite
    3. Fluorite
    4. Apatite
    5. Feldspar
    6. Quartz
    7. Topaz
    8. Corundum
    9. Diamond
  2. If you don’t have one of each from the following scale (at least up to quartz), then you’ll need to do this experiment a different way – the way most geologists do it in the field. Here’s how:
  3. Scratch one of the rocks with your fingernail. If you can leave a mark, then write “Y” in the second column of the data table. Now skip over to the last column and estimate the hardness to be less than 2.5.
  4. If you can’t scratch it with your fingernail, try using the mineral to scratch a copper penny. If it doesn’t leave a mark on the penny, skip over to the last column and estimate the hardness to be between 2.5-3.5.
  5. If it does leave a scratch on the penny, then try scratching the mineral with a steel nail. If the nail leaves a scratch, skip over to the last column and estimate the hardness between 3.5-5.5.
  6. If you can’t scratch the sample with the nail, see if the mineral can make a scratch on the plate glass. Glass has a hardness of 6-7. If it doesn’t make a scratch on the glass, then it’s between 5.5-6.5. If it does, it’s higher than 6.5. For example quartz will make a scratch on the plate, and its hardness has been recorded at 7.

Exercises


  1. If a mineral scratches a penny but doesn’t get scratched by a nail, can you approximate its hardness?
  2. Give examples of the hardest and softest minerals on the Mohs’ Scale.
  3. Is feldspar harder or softer than quartz?

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You will be able to identify minerals by their colors and streaks, and be able to tell a sample of real gold from the fake look-alike called pyrite.


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Materials


  • 1 handheld magnifying lens
  • Unglazed porcelain tile
  • Rock samples (the ones in the video are: graphite, pyrite, talc, iron, and jasper)


Download worksheet and exercises


Every mineral has a set of unique characteristics that geologists use to test and identify them. Some of those tests include looking at the color of the surface, seeing if the mineral is attracted to a magnet, dripping weak acids on the rock to see if they chemically react, exposing them to different wavelengths of light to see how they respond, scratching the rocks with different kinds of materials to see which is harder, and many more. There are more than 2,000 different types of minerals and each is unique. Some are very hard like diamonds, others come in every color of the rainbow, like quartz and calcite, and others are very brittle like sulfur.


The color test is as simple as it sounds: Geologists look at the color and record it along with the identification number they’ve assigned to their mineral or rock. They also note if the color comes off in their hands (like hematite). This works well for minerals that are all one color, but it’s tricky for multi-colored minerals. For example, azurite is always blue no matter where you look. But quartz can be colorless, purple, rose, smoky, milky, and citrine (yellow).


Also, some minerals look different on the surface, but are really the same chemical composition. For example, calcite comes in many different colors, so surface color isn’t always the best way to tell which mineral is which. So geologists also use a “streak test”.


For a streak test, a mineral is used like a pencil and scratched across the surface of a ceramic tile (called a streak plate). The mineral makes a color that is unique for that mineral. For example, pink calcite and white calcite both leave the same color streak, as does hematite that comes in metallic silvery gray color and also deep red. This works because when the mineral, when scratched, is ground into a powder. All varieties of a given mineral have the same color streak, even if their surface colors vary. For example, hematite exists in two very different colors when dug up, but both varieties will leave a red streak. Pyrite, which looks a lot like real gold, leaves a black streak, while gold will leave a golden streak.


The tile is rough, hard, and white so it shows colors well. However, some minerals are harder than the mineral plate, like quartz and topaz, and you’ll just get a scratch on the plate, not a streak.


  1. Number your rock samples by placing them on your data table.
  2. Using your data table, record the color of each sample.
  3. Now use your streak plate. Take a rock and draw a short line across your streak plate (unglazed porcelain tile).
  4. Record the color of the streak in your data table. Are there any surprises?

Exercises


  1. What does it mean if there’s no streak left?
  2. Give an example of a kind of rock that leaves a streak a different color than its surface color.
  3. What is a mineral that appears in two different colors, yet leaves the same color streak?

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This is a recording of a recent live teleclass I did with thousands of kids from all over the world. I've included it here so you can participate and learn, too! Learn about the world of rocks, crystals, gems, fossils, and minerals by moving beyond just looking at pretty stones and really being able to identify, test, and classify samples and specimens you come across using techniques that real field experts use. While most people might think of a rock as being fun to climb or toss into a pond, you will now be able to see the special meaning behind the naturally occurring material that is made out of minerals by understanding how the minerals are joined together, what their crystalline structure is like, and much more.

Materials:

 
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If you’ve ever eaten fruits or vegetables (and let’s hope you have), you have benefited from plants as food.  Of course, the plants we eat have been highly modified by growers to produce larger and sweeter fruit, or heartier vegetables.


There are three basic ways to create plants with new, more desirable traits:


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Grafting

Grafting takes advantage of the fact that trees have the ability to heal themselves.  In this method, a branch of a tree is cut off and replaced with the branch of a different tree.  Wait a season and, voila, a new tree with the traits of the branch that was added on, or grafted, is growing on the original tree.


There are many reasons for grafting.  First, it allows growers to produce a tree with more than one type of fruit.  Peaches, plums, and apricots can all be found on the same tree after grafting has occurred.  Grafting of the same fruit can also beneficial.  Sweet oranges are preferred for taste, but trees that produce these types of oranges are at greater risk for disease.  Also, sweet oranges often have no seeds, making it impossible for them to reproduce naturally.  By grafting sweet oranges onto sour orange trees, both problems can be avoided.


 Hybridization

You’ve probably noticed that children look like their parents, and that brothers and sisters tend to look alike as well.  We share more traits with the people we are most closely related to.  This is the basic idea of the branch of science called genetics.  It’s not just true with people, though.  Plants will share traits with their offspring.


Breeders have been using the ideas of genetics for years.  They have been forcing plants with traits people find desirable to breed, hoping that the offspring will share those traits.  Traits such as resistance to disease, large size, and sweetness, are bred for.  When breeders began doing this, they didn’t know about genes, the factors that carry traits from parents to offspring.  As this became known, breeders became better at making crosses that would produce the traits they were looking for.


Transgenics

Every living thing has a genome.  A genome is the complete sequence of genes the organism has.  The genes of each organism are different, which is why a bacterium is different than, say, a tomato.  For the most part, that’s a good thing.  We wouldn’t want our tomatoes to be much like bacteria.  But what if we did?  At least a little.  If there was something in bacteria that would be helpful to tomatoes, would there be a way to add the bacteria gene to the tomato genome?  It turns out that the answer is yes, and transgenics refers to the process of adding something helpful to another organism’s genome.


In the case of the bacteria and the tomato, some bacteria have a gene that would give tomatoes resistance to disease.  This gene has been placed in many tomatoes.  Some people have concerns about transgenics, worrying that adding to genomes could have unintended consequences.  Nevertheless, this process has become very common.


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Six-foot zucchini? Ten-foot carrots? Are giant veggies just a photography trick, or are they real?


The happy news is that yes, they’re real! Expert horticulturists have accumulated a great wealth of knowledge about different climates and dirt conditions. They must know about the different chemical, physical and biological properties of gardens and do multiples of experiments dozens of plants. We found an incredible horticulturist, John Evans, who has accumulated over 180 first places in both quality and giant vegetable categories, with 18 State and 7 World Records.


According to John Evans: “If you could, imagine what it would be like to dig up a carrot from your garden and not knowing how big it is until the last minute, and then finding out that it’s 19 lbs. Now that’s exciting!”


John has spent many years developing fertilizers, bio-catalysts, and growing techniques to grow 76-lb cabbages (photo shown left), 20-lb carrots, 29-lb kale, 60-lb zucchini,  43-lb beets, 35-lb broccoli and cauliflowers, and 70-lb swiss chard that was over 9 feet tall and took three people to carry it to the trailer!


Here’s a video on growing giant flowers by a passionate community gardening club:
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So what makes the plants grow so large? Apart from good soil and climate conditions, there are a few tricks you can do in order to encourage growth in plants.The video above shows the effects of using gibberellic acid. So what is that stuff, anyway?


Hormones are chemicals that send messages causing changes in living things.  Gibberellic acid is a hormone that makes some pretty noticeable changes. This hormone changes the RNA of plants.  RNA is an important molecule that affects which proteins are produced by an organism.  By changing proteins, the characteristics of the organism can be changed.  In the case of Gibberellic acid, the change in RNA makes cells grow faster and longer. When added to a plant, it makes the plant grow larger than it otherwise would grow.  See for yourself!


  1. Plant two lettuce seeds in similar soil in the same general area.
  2. Spray one seed with Gibberellic Acid.
  3. Make daily observations.
  4. How did the control plant (no acid) compare to the experimental plant (with acid)?

Gibberellic acid is very potent, and does occur naturally in plants to controls their development. This is a place where a little bit goes a long way. In fact, if you use only a couple of drops, you’ll see a big effect… too much and the reverse will happen (hardly any growth at all).


Gibberellic acid can do several things, including stimulate rapid growth in the root and stem and trigger mitosis in the leaves. Scientists have used gibberellic acid to start germination in dormant seeds. You’ll also find it used by farmers who need larger clusters of grapes and cherries. Since plants get ‘used to’ gibberellic acid and become less responsive to it over time, you’ll want to use only a little bit on your plants.


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If you’re thinking sunlight, you’re right. Natural light is best for plants for any part of the plant’s life cycle. But what can you offer indoor plants?


In Unit 9 we learned how light contains different colors (wavelengths), and it’s important to understand which wavelengths your indoor plant prefers.


Plants make their food through photosynthesis: the chlorophyll transforms carbon dioxide into food. Three things influence the growth of the plant: the intensity of the light, the time the plant is exposed to light, and the color of the light.


When plants grow in sunlight, they get full intensity and the full spectrum of all wavelengths. However, plants only really use the red and blue wavelengths. Blue light helps the leaves and stems grow (which means more area for photosynthesis) and seedlings start, so fluorescent lights are a good choice, since they are high in blue wavelengths.


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For my fourth grade science project, I placed a box over a plant and poked different colored lights into each upper corner to see which way the plant grew. It turned out that my plant grew toward the blue light the most.  When I turned off the red light, my little plant stopped flowering, but started flowering again when the red light turned on.


After doing my homework, I learned that chemicals in my plant respond to light and dark conditions, which means that my little plant could “tell time” by using chemistry. Not the 12-hour clock that we use to tell time with, but they know time over a longer period, like when to flower in a season and when to conserve energy for winter.


I know now that if I had indoor plants, I’d choose fluorescent bulbs high in the blue wavelengths, and I’d also add an incandescent bulb if my plant had flowers I wanted to blossom. Since incandescent also produces heat, I’d also try playing with red LED lights which weren’t available to me when I did my project, but would make an interesting study today!


Here’s a video on what happens if you use a black light with indoor plants:



The scientific method is used by scientists to answer questions and solve problems. Often, good scientific questions are best on things we already know. For example, we know plants need light to grow because the light allows them to make their own food, but what color of light is best? Use the scientific method in the lab below to figure it out.


Experiment:


  • Place four plants in an area that will get minimal natural lighting.
  • Do some colors of light help plants grow better than plain white light? Make a hypothesis about this question.
  • To test things out, grow one plant with plain white light. Grow the other plants with colored light, either by using colored bulbs or by covering white bulbs with tissue paper.
  • Make daily observations. Which plant grew best? Was your hypothesis correct?

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Broccoli, like all plants, has chlorophyll, making it green. You can really “see” the chlorophyll when you boil broccoli. This is such a simple experiment that you can do this as you prepare dinner tonight with your kids. Make sure you have an extra head of broccoli for this experiment, unless you really like to eat overcooked broccoli.


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First, boil a pot of water. Add some cut up broccoli, and immediately observe the color. Allow the broccoli to cook for 15 minutes, and observe the color again.


What’s happening? When you first put the broccoli in the boiling water, the hot water allowed air bubbles to escape. This allowed you to clearly view chlorophyll, the chemical that makes broccoli green, so the broccoli should have appeared very bright. After 15 minutes of cooking, chlorophyll undergoes a chemical change. More acid has entered the broccoli, and it is a duller color.


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Mass and energy are conserved. This means you can’t create or destroy them, but you can change their location or form.


Most people don’t understand that the E energy term means all the energy transformations, not just the nuclear energy.


The energy could be burning gasoline, fusion reactions (like in the sun), metabolizing your lunch, elastic energy in a stretched rubber band… every kind of energy stored in the mass is what E stands for.


For example, if I were to stretch a rubber band and somehow weigh it in the stretched position, I would find it weighed slightly more than in the unstretched position.


Why? How can this be? I didn’t add any more particles to the system – I simply stretched the rubber band. I added energy to the system, which was stored in the electromagnetic forces inside the rubber band, which add to the mass of the object (albeit very slightly). Read more about this in Unit 7: Lesson 3.


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For plants, this means that energy from captured sunlight, combined with carbon dioxide and water, both of which have mass, make the plant heavier. Let’s find out how Einstein would have planted a garden while thinking about his big ideas.


Materials:


  • scale for weighing your plant
  • pot with soil
  • plant (not potted yet)
  • water
  • time
  • notebook and pencil to record your findings



Download Student Worksheet & Exercises


  1. Prepare a pot with dirt. Add a measured amount (like 1 cup) of water to dampen the soil. Weigh the pot filled with soil (but no plant).
  2. Add a plant to the pot and weigh the whole thing.
  3. Subtract the weight you found in step 1 from step 2 to find out how much the plant weighs.
  4. You’ll be weighing your pot each day. Weigh the plant before watering (water it the same amount each day) and write it down in your notebook . If you’re giving it water and sunlight, the plant should be getting heavier.
  5. Where does this mass come from? You can’t create mass, and yet the plant is getting heavier. How?

You and I get heavier when we eat food. You aren’t giving the plant food, but it is getting food. How? Where does its food come from? The energy from the sun is changed to sugars during photosynthesis, increasing the mass of the plant.


Exercises


  1. Where does this mass come from? You can’t create mass, and yet the plant is getting heavier. How?
  2. Can energy be created?
  3. Can energy be destroyed?

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silverwareGrab a handful of buttons. Make sure there are all different kinds and colors.


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If you don’t have buttons, use any pile of objects, like matchbox cars, coins, nuts, etc.


Now group the buttons according to size, color, texture, number of holes, shape, etc.


You can do this activity with shells, peanuts, plant leaves, or the back of your desk drawer. Is it easier to organize the non-living or the living things?


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Why do families share similar features like eye and hair color? Why aren’t they exact clones of each other? These questions and many more will be answered as well look into the fascinating world of genetics!


Genetics asks which features are passed on from generation to generation in living things. It also tries to explain how those features are passed on (or not passed on). Which features are stay and leave depend on the genes of the organism and the environment the organism lives in. Genes are the “inheritance factors “described in Mendel’s laws. The genes are passed on from generation to generation and instruct the cell how to make proteins. A genotype refers to the genetic make-up of a trait, while phenotype refers to the physical manifestation of the trait.


We’re going to create a family using genetics!


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Materials
• Paper or use this Genetics Table
• Two different coins
• Scissors
• Glue or Tape



Download Student Worksheet & Exercises


Step one: Creating the Parent Generation

  1. First you’re going to create the genetic make-up of the parents. Here’s how:
  2. Take out the Genetics Data Table, and flip the first coin to create the genetic profile for the mother.
  3. Flip the coin and in the Mother’s Hair trait column, write D for dominant if the coin reads heads, and R for recessive if tails in the table.
  4. Flip the coin again. In the Mother’s Hair trait column right after the first trait, write D for dominant if the coin reads heads, and R for recessive if tails in the table.
  5. If you flipped heads the first time and tails the second, you’d write “DR” in the Mother’s Hair box.
  6. Continue this process for all of Mother’s traits. You should have two letters in each box for the entire column.
  7. Repeat steps 3-6 for Father. When you’ve completely filled out Mother’s and Father’s columns, you’ve completed the paternal genetic profile. Now you’re ready for the next part:

Step two: The Child

  1. Will the child be a boy or a girl? To determine this, flip the second coin. Heads for a boy, tails for a girl. After this is decided, circle boy or girl under “child 1” on the Genetics Data Table.
  2. Now the first coin will represent the gene from the mother and the second coin will represent the gene from the father.
  3. Start with the Hair trait: Flip both coins. If the first coin is tails, take the first trait from the mother. If the first coin is heads, take the second trait.
    1. For example, if the first coin is tails, and the mother’s code is DR, then write “D” in the child one column for hair.
    2. Do the same thing for the father’s traits with the second coin. For example, if the second coin is heads, and the father’s code is DR, then write “R” in the Hair Trait column of child 1.
    3. By the end of this step, child 1 should have one letter from the mother, and one letter for the father in child 1’s hair trait column.
  4. Use the same steps used to find the genetic code for the hair trait to find the code for the rest of the traits. By the end all the traits should have one letter from the mother’s genetic code and one letter from the father’s genetic code.

Step 3: What the Child Looks Like

Grab a sheet of paper and start drawing the child. If the genetic code for a trait has a “D” in it, then the dominant trait is used.


For example, if the hair color is DD, DR, or RD then the hair color is dark. If the hair color code is RR, then the hair color is light. Draw the traits on your paper!


You can repeat this for as many children as you would like in your family.


Step 4: Make another family and compare!

Are all families alike? What if you try this process again for another family? Do you see any similarities or differences? Do similar features come from dominant genes? Do differences come from recessive genes? What other traits would you include? Write this in your science journal!


Conclusions:

In fact, most similarities should come from the dominant genes because they are expressed more often. The recessive genes are expressed less often, so the create the differences.


Extra credit:

What percent of the children expressed the dominant allele of each trait? Did you get Mendel’s results? Do the calculations and check it out!


Exercises


  1. What is the difference between a genotype and a phenotype?
  2. What is a dominant trait?
  3. What is a recessive trait?
  4. Assume B=Black hair and b=blond hair.  Make a Punnet square to cross Bb with bb. Tell what the possibilities are for offspring hair color.
  5. Why don’t traits simply average out in offspring.  For example, why does a tall plant crossed with a short plant not yield a bunch of average-sized plants?
  6. In your activity, what percent of the children expressed the dominant allele of each trait? Did you get Mendel’s results? Do the calculations and check it out!

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Insects are not only the most diverse subgroup of arthropods, but with over a million discovered species it is the most diverse group of animals on earth. Although they can’t all be as beautiful as a butterfly, they all play important roles in their ecosystems—just think of where we would be without bees!


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The segmented exoskeletons of insects have a hard, inner layer called the cuticle, and a water-resistant outside layer called the exocuticle. Insects are divided into two major groups: winged insects and wingless insects. Air is taken in through structures called spirials, and delivered directly to the body.



Most insects reproduce sexually and are oviparous (hatch from eggs after the eggs are laid), although some insects reproduce asexually.


You can grow your own butterflies using a premade kit from Home Training Tools!


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Some insects are just too small! Even if we try to carefully pick them up with forceps, they either escape or are crushed. What to do?


Answer: Make an insect aspirator! An insect aspirator is a simple tool scientists use to collect bugs and insects that are too small to be picked up manually. Basically it’s a mini bug vacuum!


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Download Student Worksheet & Exercises


Here’s what we’ll need:


  • A small vial or test tube with a (snug fitting) two-holed rubber stopper.
  • Two short pieces of stiff plastic tubing. We’ll call them tube A and tube B.
  • Fine wire mesh (very small holes because this is what will stop the bugs from going into your mouth!)
  • A cotton ball.
  • One to two feet of flexible rubber tubing.
  • Duct tape or a rubber band.

Here’s how we make it:


  • Insert the tube A and Tube B into the stopper such that the stopper is in the middle of both pieces.
  • Bend both A and B plastic tubing 90 degrees away from each other. Their ends should be pointing away from each other.
  • Cut a square of mesh large enough to the end of the plastic tubing. Tape (or rubber-band) the mesh over bottom of tube A only. Remember, if you cover both of the tubes the bugs won’t be able to enter the aspirator.
  • Insert a small amount of cotton ball into the other side of tube A (not enough to block airflow, just enough to help filter the dust and particles entering the vial.
  • Cut another piece of mesh and cover the other end of Tube A. Secure that mesh with another piece of tape/rubber band.
  •  Fit the rubber tubing over the top of tube B (the bent side).
  • Fit the stopper into the vial/test tube.

How it works: To use the aspirator, hold the end of the rubber tubing near the insects you want to collect, and suck through the top of tube A. The vacuum you create sucks the insects into the vial/test tub (make sure they can fit in the tube!).


Troubleshooting: The bugs aren’t being pulled into the vial! In that case the suction may not be strong enough. Remove the cotton ball and try again. If it still is not working check to make sure the aspirator is air-tight (is the stopper fitting snuggly into the vial? Are there cracks/holes around or in the plastic tubes?).


TIP: I kept eating bugs! Make sure your wire mesh is very fine (the holes are smaller than the bugs you’re trying to collect). Otherwise you may be ordering a lunch you don’t want!


Exercises


  1. Why don’t we use a large vacuum to suck up the bugs?
  2.  Why do we need a small mesh covering on the end of the straw that we suck on?
  3.  Why do we need to be careful about catching ants?
  4.  What insects did you catch that you rarely see?
  5.  What familiar insects did you catch? (answers may vary).

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The way animals and plants behave is so complicated because it not only depends on climate, water availability, competition for resources, nutrients available, and disease presence but also having the patience and ability to study them close-up.


We’re going to build an eco-system where you’ll farm prey stock for the predators so you’ll be able to view their behavior. You’ll also get a chance to watch both of them feed, hatch, molt, and more! You’ll observe closely the two different organisms and learn all about the way they live, eat, and are eaten.


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This experiment comes in two parts. The materials you need for both parts are:


  • four 2-liter soda bottles, empty and clean
  • 2 bottle caps
  • one plastic lid that fits inside the soda bottle
  • small piece of fruit to feed fruit flies
  • aluminum foil
  • plastic container with a snap-lid (like an M&M container or film can)
  • scissors and razor with adult help
  • tape
  • ruler
  • predators: spiders OR praying mantis OR carnivorous plants (if you’re using carnivorous plants, make sure you do this Carnivorous Greenhouse experiment first so you know how to grow them successfully)
  • soil, twigs, small plants

Fruit Fly Trap

In order to build this experiment, you first need prey. We’re going to make a fruit fly trap to start your prey farm, and once this is established, then you can build the predator column. Here’s what you need to do to build the prey farm:



Download Student Worksheet & Exercises


Did you know that fruit flies don’t really eat fruit? They actually eat the yeast that growing on the fruit. Fruit flies actually bring the yeast with them on the pads of their feet and spread the yeast to the fruit so that they can eat it. You can tell if a fruit fly has been on your fuit because yeast has begun to spread on the skin.


When you have enough fruit flies to transfer to the predator-prey column, put the entire fruit fly trap in the refrigerator for a half hour to slow the flies down so you can move them.


If you find you’ve got way too many fruit flies, you might want to trap them instead of breed them. Remove the foil buckets every 4-7 days or when you see larvae on the fruit, and replace with fresh ones and toss the fruit away. Don’t toss the larvae in the trash, or you’ll never get rid of them from your trash area! Put them down the drain with plenty of water.


Predator-Prey Column

You can use carnivorous plants, small spiders, or praying mantises. If you use plants, choose venus flytraps, sundews, or butterworts and make sure your soil is boggy and acidic. You can add a bit of activated charcoal to the soil if you need to change the pH. Since the plants like warm, humid environments, keep the soil moist enough for water to fog up the inside on a regular basis. You know you’ve got too much moisture inside if you find algae on the plants and dirt. (If this happens, poke a couple of air holes.) Don’t forget to only use distilled water for the carnivorous plants!


Keep the column out of direct sunlight so you don’t cook your plants and animals.



Exercises


  1. What shape is the head of the mantis?
  2.  How many eyes does a praying mantis have?
  3.  How else has the mantis head evolved to stalk their prey?
  4.  How does a praying mantis hold its food?
  5.  Do fruit flies eat fruit?
  6.  How do predators and prey change over time?

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When you hear “roach” you might not immediately think of something that would make a good pet, but not all roaches are like the cockroaches you might have seen in your house!


Species such as the Orange Spotted Roach (Blaptica dubia) make excellent insect pets: they don’t cost much, they have an interesting life cycle and habits, and they do not require much effort to care for. Their average lifespan is about 18 months and you’ll be able to learn more about their fascinating life cycle (from egg to adult) if you allow them to breed!


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A pet roach isn’t a pest?


It may seem like all roaches are pests, but of 4,000 species, only 4 or 5 live in homes and are considered pests (such as the American cockroach). Most roaches live in tropical environments far from domesticated areas. They are very different from the kind of household pest you might think of when you hear “roach.”


You might think roaches would make pretty boring pets, but they are surprisingly fast and fun to watch. You can learn a lot about insect anatomy and what makes roaches unique by taking care of them. The species that make good pets do not smell, are not noisy, cannot fly, and generally are very easy to clean up after. They typically are most active at night, because they prefer a dark environment like they have on the floor of the rainforest. They love to hide during the day, but will come out to eat.



Can I touch them?  They are meant to be pets, and are perfectly safe to handle. A good environment for roaches is a small aquarium or plastic cage with cardboard egg cartons for them to hang out in. You might try picking up one of the egg cartons where a roach is hiding, then either hold the carton so the roach can crawl around on it or let the roach crawl in to your hands. Hold out your hand, keeping your fingers together and flat. Let the roach crawl on you, then slowly lift out your hand and cup it slightly. Remember to wash your hands afterwards, using warm water and soap. Although these insects don’t cause diseases in humans, they may be carrying harmful bacteria, so it is important to wash your hands so that you don’t get sick.


How long do they live? It varies, but species like Orange Spotted Roaches have a lifespan of 18-24 months. The female gives live birth, usually to 20-30 babies at a time. The babies reach maturity in 3-4 months after they are born. While they are growing into adults, they will molt – shedding their outer hard shell, or exoskeleton, and then growing a bigger one.


Will my roaches breed? If you get one male and one female, there is a good chance that they will breed under the right circumstances. If you do not want baby roaches, keep the temperature of the habitat around 70 degrees, or normal room temperature. Adult Orange Spotted Roaches will be fine at this temperature, but they will not mate because their young need higher temperatures to survive. If you would like to see the complete life cycle, you will need to ensure that their habitat has enough heat and humidity.


Feeding Time: What does a pet roach eat? They are omnivores – they eat plants and meat. So a good basic diet contains protein from plants and animals and fiber from grains. You can buy special roach food for them and then to supplement their diet give them fresh fruits and vegetables once a week. Try putting a slice of apple, banana, orange, carrot, potato, or zucchini, or a few spinach leaves in a shallow plastic dish and put it in their habitat. This will provide vitamins and minerals for your pets. Be sure to take the uneaten produce out of the habitat within 48 hours to prevent mold from growing, or attracting ants or fruit flies. A great roach diet would be dry food every day and a fresh food supplement once a week.


Be sure to keep their water dish full. Roaches can live a long time without food, but usually only survive three days without water. The water dish also helps make their habitat more moist and humid. For easiest care, use water absorbent crystals that hold water. You can keep an airtight container of prepared water crystals in a cool place, and add another crystal to the water dish whenever needed (usually every 2-3 days).


If the habitat is hot and humid, the roaches will be more active, which means they will also eat and drink more.


Cleaning Time: You should periodically clean out your pet roach’s habitat to make sure there is no mold growing. Cleaning out the habitat takes only a few minutes and will prevent any bad odors coming from your insects. When is the right time to clean the habitat? When you see small dark roach droppings starting to collect on the bottom, you should clean the habitat out. Usually about once a month is a good time. The minimum should be once every other month.


To clean out the habitat, first remove the roaches. Place them in a container that has smooth sides to prevent them from climbing out. Pick up the roaches one at a time and transfer them to the carton or other container. If a roach is hiding in an egg carton, carefully lift out the carton, then let the roach crawl off into the container or onto your hand. Wash your hands with soap and warm water after touching the roaches.


Take the food and water dishes out, as well as the egg cartons, and place them on paper towels. Rinse the container out and then wash it with a solution of 10 parts warm water to 1 part bleach. Rinse the container again and dry it thoroughly. Place the food and water dishes back in the container. If the cardboard egg cartons seem clean, put them back into the container. Don’t use foam egg cartons. You can also use cardboard tubes in different sizes (mailing tubes, toilet paper tubes, or wrapping paper tubes cut down to shorter lengths) so the roaches can crawl in them. When you’re finished cleaning, throw the used egg cartons away as well as the paper towels. Transfer your roaches back to their habitat, using a flat hand so they can crawl off.


Building a Roach Ranch: If you decide to get a pet roach, you can create a habitat to be as simple or creative as you like. If you wish to make a more natural-looking habitat for your pet roaches to enjoy, you can buy peat moss or coconut husk mulch from a pet store (in the Reptile section). Put in a layer of moss or mulch (about one inch), then add pieces of bark for the roaches to climb on and hide under. This type of Roach Ranch will be similar to the Orange Spotted Roaches’ natural environment in the rainforests of South America.


You can make a Roach Ranch out of cardboard, which can easily be thrown away when it gets dirty. Make a multi-level mansion for your roaches by cutting 3-4 identical shapes (square, rectangle, L-shape) from cardboard. Put separators in between each level – use stacked cardboard strips that are one inch wide and several inches long. Each level should be separated about ½” or three strips of cardboard stacked together. Use Elmer’s glue to attach the separators and flat levels, and let it dry completely (may take up to 24 hours) before putting it in your roach habitat. Add cardboard tubes or crumpled newspaper to complete your Roach Ranch. Remember that it will be easier to clean if roach droppings can fall freely to the ground. When you clean your habitat, check to see if your Roach Ranch is staying clean. Throw away any parts that have been well-used and add new cardboard material for the roaches to climb.


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This experiment is for advanced students.


ACID!!! The word causes fear to creep in and get our attention.


BASIC!!! The word causes nothing to stir in most of us.


The truth is, a strong acid (pH 0-1) is dangerous, but a strong basic (pH 13-14) is just as dangerous. In this lab, we will get comfortable with the basics of bases and the acidity of acids along with how you can use both and tell the difference between them.


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Familiar acidic solutions:


  • pH 1: Stomach acid
  • pH 2: Lemon juice
  • pH 3: Vinegar
  • pH 4: Soda pop
  • pH 5: Rainwater (serious acid rain could have a pH of 2-4)
  • pH 6: Milk
  • pH 7: Distilled water
  • pH 8: Egg whites
  • pH 9: Baking soda
  • pH 10: Antacid
  • pH 11: Ammonia
  • pH 12: Limewater
  • pH 13: Drano
  • pH 14: Sodium hydroxide (NaOH)

Materials:


  • Lemon
  • Apple
  • Blue litmus paper
  • White vinegar
  • Clear glass cup
  • Tartaric acid (C4H6O6)
  • Measuring spoon
  • Measuring syringe
  • Water
  • Test tube rack
  • Test tube
  • Cool water
  • Sodium hydroxide (NaOH) (MSDS)
  • Dropper pipette
  • Calcium hydroxide (CaOH) (MSDS)
  • Erlenmeyer flask
  • Solid rubber stopper
  • Storage bottle
  • Stick-on label
  • Permanent marker

Acids usually taste sour and turn blue litmus paper red. There are exceptions. One exception to this is with apples. They contain malic acid. Malic acid does in fact taste sour by itself, but apples produce so much sugar that the sour taste of the acid is overpowered with sweetness. Making lemonade is a good example as well.


NaOH – Be very careful working with sodium hydroxide (NaOH). It isn’t an acid, so it shouldn’t be very harmful, right? WRONG! A strong base is just as dangerous as a strong acid. Please be careful when using them.


Don’t get confused and don’t forget what litmus paper indications mean. Acids turn blue litmus paper red, and bases turn red litmus paper blue. If you are testing a substance and the paper doesn’t change color, try the other type. The substance might not be neutral, but an acid or base that you used the wrong color litmus paper.


When testing with litmus paper, don’t dip the litmus paper into the chemical bottle. Use a clean dropper to transfer the chemical to the paper. Dipping into the chemical can and will, eventually, contaminate the chemical.


When shaking a liquid in a test tube or flask, put a solid rubber stopper on top. If you just start shaking from there, your stopper may fly across the room and scare your dog unnecessarily. The hot, or acidic, or basic contents of the container will find a place on the salad waiting to be served. The paramedics will be puzzled when they find the entire family, heads down, lettuce hanging from their mouths. With the stopper firmly inserted, wrap your hand around the container with your thumb over the stopper, pushing down to hold it in place while you shake.


After we finish the experiment, don’t discard the contents of the Erlenmeyer flask. It now contains limewater, a substance that we want to save for later experiments. Carefully pour the liquid into a storage bottle and discard the solids in the trash. Place a sticker on the bottle and/or use a permanent marker to label the bottle for future use. Keep the storage bottle out of direct sunlight when storing it.


We will explore for ourselves some of the properties of acids and bases. If we consider the acid-base theory discussed below, it will help us to further understand what we are experiencing in our lab.


C3000: Experiments 5-18


Download Student Worksheet & Exercises


Cleanup: We must clean everything thoroughly after we finish with the lab. After cleaning with soap and water, we need to rinse everything thoroughly. Chemists use the rule of “three” in cleaning glassware and tools. After washing, chemists rinse out all visible soap and then rinse three times more.


Storage: Place cleaned tools and glassware in their respective storage places.


Disposal: Liquids can be washed down the drain, and solids put in the trash.


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Cobalt chloride (CoCl2) has a dramatic color change when combined with water, making it a great water indicator. A concentrated solution of cobalt chloride is red at room temperature, blue when heated, and pale-to-clear when frozen. The cobalt chloride we’re using is actually cobalt chloride hexahydrate, which means that each CoCl2 molecule also has six water molecules (6H2O) stuck to it.


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For this experiment you’ll need:


  • cobalt chloride
  • cotton swab
  • goggles
  • test tube with stopper
  • index card
  • distilled water
  • hair dryer


Download Student Worksheet & Exercises


Fill your test tube partway with water and add 1 teaspoon of cobalt chloride. Cap and shake until the solids dissolve. Continue to add cobalt chloride, 1 teaspoon at a time, until you cannot dissolve any more into your solution. (You have just made a saturated solution.)


Using your cotton swab like a paintbrush, dip into the solution (your “paint”) and write on the index card. Use a hair dryer to blow across the solution. (Be careful not to scorch the paper!) What happens? Stick it in the freezer. Now what happens? What if you blow dry it after it comes out of the freezer? What else can you come up with? What happens if you spritz it with water?


What’s Going On? The cobalt changes color when hydrated/dehydrated – think of it as an indicator for water. It should be red when you first mix it, but blue when hit with the hair dryer. It doesn’t react to acids and bases the way the anthocyanin (in red cabbage juice) or universal indicator does, but rather with humidity.


Bonus Experiment Idea! You can grow red crystals by cooling off a cup of hot water. Here’s how: into a test tube, add 40 drops of hot water and 2 small spoon measure of cobalt chloride. Suspend a small pebble attached to a thread into the test tube (this is your starter-seed for your crystals to attach to). If after a day or two your crystals aren’t growing, just reheat the solution and add a little bit more of the chemical.


ANOTHER Bonus Experiment Idea! By soaking a strip of tissue or crepe paper (it’s got to be thin) in the cobalt chloride solution, you can create your own weather forecaster! Simply let dry and when it turns blue, you’re in for blue skies and pink means it’s going to rain. (It’s basically a humidity gauge.)


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You can go your whole life without paying any attention to the chemistry behind acids and bases. But you use acids and bases all the time! They are all around you. We identify acids and bases by measuring their pH.


Every liquid has a pH. If you pay particular attention to this lab, you will even be able to identify most acids and bases and understand why they do what they do. Acids range from very strong to very weak. The strongest acids will dissolve steel. The weakest acids are in your drink box. The strongest bases behave similarly. They can burn your skin or you can wash your hands with them.


Acid rain is one aspect of low pH that you can see every day if you look for it. This is a strange name, isn’t it? We get rained on all the time. If people were dissolving, if the rain made their skin smoke and burn, you’d think it would make headlines, wouldn’t you? The truth is acid rain is too weak to harm us except in very rare and localized conditions. But it’s hard on limestone buildings.


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Acids are liquids with a pH less than seven. A pH of seven is considered neutral. Bases are liquids with a pH greater than seven.


The combustion of fossil fuels such as oil, gasoline, and coal, create acid rain. Rain, normally at a pH of about 5.6, is always at least slightly acidic. Carbon dioxide is released into the air reacts with moisture in the air to form carbonic acid (HCO3). Sulfur dioxide and nitrogen oxides are released into the air by fossil fuel combustion. They react with the slightly acidic rain and form sulfuric acid (H2SO4) and nitric acid (HNO3).


We’re going to have fun with color changes in this experiment. We will make magic paper that changes color to tell us important things about liquids. It’s called litmus paper.


Litmus is harvested from a plant called a lichen, and bottled up as a powder. We’ll take the powder and make an acid-base indicator with it. Then we will use what we make to test solutions. And if you exercise your mind a bit, you will discover ways to use your litmus paper to discover things about the house and the world around you.


Materials:


  • Test tube rack
  • 2 Test tubes
  • Test tube stopper
  • Distilled water
  • Ruler
  • Litmus powder (MSDS)
  • Measuring spoon
  • Denatured alcohol (MSDS)
  • Pipette
  • Sodium carbonate (Na2CO3) (MSDS)
  • Sodium hydrogen sulfate (NaHSO4) (MSDS) Sodium hydrogen sulfate is very toxic. Respect it, handle it carefully and responsibly. Do not take it for granted.
  • Scissors
  • Filter paper (or paper towel or coffee filter)
  • Impervious surface

NOTE: Be very careful when handling the sodium hydrogen sulfate – it’s highly corrosive and dangerous when wet.  Handle this chemical only with gloves, and be sure to read over the MSDS before using.


We will be using a ruler to measure the amount of water in a test tube. Ordinarily, chemists use more accurate measurement tools than a ruler. For the first part of this lab, making litmus solution, all we need is an approximate volume of water.


We will also be shaking a liquid in a test tube. Ever leave the top of a blender off when the “on” button is depressed? If not, just believe that it’s not a good idea. There is a certain technique t use when shaking up a liquid. We’ll place a stopper on a test tube and shake vigorously. Remember to do that as a chemist would do.


In a laboratory, whenever a chemist stoppers a solution and shakes it, it will be done the same way no matter if it is a toxic substance or just salt and water. That way, they are in the habit of doing it one way, the right way, so a mistake is not made at any time. A mistake at the wrong time could even be fatal.


Stopper the test tube firmly. Seat it well, but don’t grind down on the stopper. A test tube is thin-walled glassware, and as we grip harder it could collapse in our hand and now we have open cuts, blood, and toxic chemical is now entering your bloodstream. Stoppered firmly, we hold the test tube in our hand and place our thumb over the stopper for added security. To top off our safety measures, point the test tube, with a thumb firmly on top, away from us or anyone else and shake to our heart’s content.


We need to be careful with our chemicals. After using a chemical, cap the container to prevent spillage and contamination. Clean everything thoroughly after you are finished with the lab, or if you are going to reuse a tool. To dip a measuring spoon into one chemical after another, contaminates the chemicals and will affect your results.


C1000: Experiments 1-10
C3000: Experiments 5-18


Download Student Worksheet & Exercises


Clean everything thoroughly after you are finished with the lab. After cleaning with soap and water, rinse thoroughly. Chemists use the rule of “three” in cleaning glassware and tools. After washing, chemists rinse out all visible soap and then rinse three times more.


Place all chemicals, cleaned tools, and glassware in their respective storage places.


Dispose of all solid waste in the garbage. Liquids can be washed down the drain with running water. Let the water run awhile to ensure that they have been diluted and sent downstream.


You can test how acidic different substances are with an acid-base indicator like litmus paper.


Using the litmus powder in the chemistry set, we will make litmus paper. Our litmus paper is going to start out blue, and will turn red when an acid is placed on it. You can turn it back to blue by placing a few drops of a basic solution on it.


Let’s look a little further into the chemistry behind acids and bases. An acid produces hydronium ions (example: H3O+) when dissolved in water. The + or notation on a molecule tells us that after a chemical reaction creates it, the molecule is left with a net positive (electrons have been lost) or net negative charge (electrons have been added). Now, the ion could have more than just a +1 or -1 charge. Often, we will discover molecules with positive or negative charges of 2, 3, or 4.


Every liquid has a pH, and some of them may surprise you. Fruits contain citric acid, malic acid, and ascorbic acids, and the distilled white vinegar in your kitchen is a weak form of acetic acid. You’ll find carbonic acids in sodas, and lactic acid in buttermilk. And remember that acids taste sour and bases taste bitter? Don’t taste your chemicals, but the sour taste of vinegar and lemons and the bitter taste of club soda water and baking soda are familiar to people.


Generally, acids are sour in taste, change litmus paper from blue to red, react with metals to produce a metal salt and hydrogen, react with bases to produce a salt and water, and conduct electricity. Strong acids often produce a stinging feeling on mucus membranes (don’t ever taste an acid, or any chemical for that matter!).


Acids are proton donors (they produce H+ ions). Strong acids and bases all have one thing in common: they break apart (completely dissociate) into ions when placed in water.  This means that once you dunk the acid molecule in water, it splits apart and does not exist as a whole molecule in water. Strong acids form H+ and an anion, such as sulfuric acid:


H2SO4 –> H++ HSO4


There are six strong acids:


  • hydrochloric acid (HCl)
  • nitric acid (HNO3) used in fireworks and explosives
  • sulfuric acid (H2SO4) which is the acid in your car battery
  • hydrobromic acid (HBr)
  • hydroiodic acid (HI)
  • perchloric acid (HClO4)

The record-holder for the world’s strongest acid are the carborane superacids (over a million times stronger than concentrated sulfuric acid). Carborane acids are not highly corrosive even though are super-strong. Here’s the difference between acid strength and corrosiveness: the carborane acid is quick to donate protons, making it a super-strong acid.  However, it not as reactive (negatively charged) as hydrofluoric (HF) acid, which is so corrosive that it will dissolve glass, many metals, and most plastics.


What makes the HF so corrosive is the highly reactive Fl ion. Even though HF is super-corrosive, it’s not a strong acid because it does not completely dissociate (break apart into H+ and Fl) in water. Do you see the difference? Weak acids only partly dissociate in water, such as acetic acid (CH3COOH).


On the other hand, bases taste bitter (again, don’t even think about putting these in your mouth!), feel slippery (don’t touch bases with your bare hands!), don’t change the color of litmus paper, but can turn red litmus back to blue, conduct electricity when in a solution, and react with acids to form salts and water. Soaps and detergents are usually bases, along with house cleaning products like ammonia.


Bases are also electron pair donors (they produce OH ions). Strong bases also completely dissociate into the OH (hydroxide ion) and a cation. LiOH (lithium hydroxide), NaOH (sodium hydroxide), KOH (potassium hydroxide), RbOH (rubidium hydroxide), CsOH (cesium hydroxide), Ca(OH)2 (calcium hydroxide), Sr(OH)2 (strontium hydroxide), and Ba(OH)2 (barium hydroxide).  Weak bases only partly dissociate in water, such as ammonia (NH3)


pH stands for “power of hydrogen” and is a measure of how acidic a substance is.  We can make homemade indicators to test how acidic (or basic) something is by squeezing out a special kind of juice (dye) called anthocyanin. Certain flowers have anthocyanin in their petals, which can change color depending on how acidic the soil is (hibiscus, hydrangeas, and marigolds for example).  The more acidic a substance, the more red the indicator will become.


Going Further

Experiment: What household items are acidic or basic? Test various liquids to see. You may be surprised. Liquids you should be sure to test are vinegar, lemon or orange juice, baking soda, and cola. Use a dropper to place drops onto the paper instead of dunking the strip into your entire carton of orange juice. Litmus flavored orange juice is not my first choice in the morning.


Experiment: Collect soil samples from various places. Not the types of plants growing in the immediate area you are sampling from. Place about an inch of dirt in the bottom of a test tube. Fill the test tube near the top with water. Use distilled water if you have it for more accuracy. Stopper the tube and shake vigorously. Use your pipette to place drops of the water on your litmus paper and see if the soil is acidic or basic. Is there a correlation between the acidity of the soil and the plants that grow there?


Note: Litmus paper will not be able to indicate how acidic the rain in your area is, because the acid content in the water droplet is not high enough to register on the indicator. The effects of acid rain take time to develop and require more sensitive equipment to detect. [/am4show]


Mars is coated with iron oxide, which not only covers the surface but is also present in the rocks made by the volcanoes on Mars.


Today you get to perform a chemistry experiment that investigates the different kinds of rust and shows that given the right conditions, anything containing iron will eventually break down and corrode. When iron rusts, it’s actually going through a chemical reaction: Steel (iron) + Water (oxygen) + Air (oxygen) = Rust
Materials


  • Four empty water bottles
  • Four balloons
  • Water
  • Steel wool
  • Vinegar
  • Water
  • Salt

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Download Student Worksheet & Exercises


  1. This lab is best done over two consecutive days. Plan to set up the experiment on the first day, and finish up with the observations on the next.
  2. Line up four empty bottles on the table.
  3. Label your bottles so you know which is which: Water, Water + Salt, Vinegar, Vinegar + Salt
  4. Fill two bottles with water.
  5. Fill two with vinegar.
  6. Add a tablespoon of salt to one of the water bottles.
  7. Add one tablespoon of salt to one of the vinegar bottles.
  8. Stuff a piece of steel wool into each bottle so it comes in contact with the liquid.
  9. Stretch a balloon across the mouth of each bottle.
  10. Let your experiment sit (overnight is best, but you can shorten this a bit if you’re in a hurry).
  11. The trick to getting this one to work is in what you expect to happen. The balloon should get shoved inside the bottle (not expand and inflate!). Check back over the course of a few hours to a few days to watch your progress.
  12. Fill in the data table.

What’s Going On?

Rust is a common name for iron oxide. When metals rust, scientists say that they oxidize, or corrode. Iron reacts with oxygen when water is present. The water can be liquid or the humidity in the air. Other types of rust happen when oxygen is not around, like the combination of iron and chloride. When rebar is used in underwater concrete pillars, the chloride from the salt in the ocean combines with the iron in the rebar and makes a green rust.


Mars has a solid core that is mostly iron and sulfur, and a soft pastel-like mantle of silicates (there are no tectonic plates). The crust has basalt and iron oxide. The iron is in the rocks and volcanoes of Mars, and Mars appears to be covered in rust.


When iron rusts, it’s actually going through a chemical reaction:
Steel (iron) + Water (oxygen) + Air (oxygen) = Rust


There are many different kinds of rust. Stainless steel has a protective coating called chromium (III) oxide so it doesn’t rust easily.


Aluminum, on the other hand, takes a long time to corrode because it’s already corroded — that is, as soon as aluminum is exposed to oxygen, it immediately forms a coating of aluminum oxide, which protects the remaining aluminum from further corrosion.


An easy way to remove rust from steel surfaces is to rub the steel with aluminum foil dipped in water. The aluminum transfers oxygen atoms from the iron to the aluminum, forming aluminum oxide, which is a metal polishing compound. And since the foil is softer than steel, it won’t scratch.


Exercises


  1. Why did one balloon get larger than the rest?
  2. Which had the highest pressure difference? Why?

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This experiment is for advanced students.Have you ever taken a gulp of the ocean? Seawater can be extremely salty! There are large quantities of salt dissolved into the water as it rolled across the land and into the sea. Drinking ocean water will actually make you thirstier (think of eating a lot of pretzels). So what can you do if you’re deserted on an island with only your chemistry set?


Let me show you how to take the salt out of water with this easy setup.


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Materials:


  • salt
  • water
  • alcohol burner
  • flask with one-hole stopper
  • stand with wire mesh screen
  • two 90-degree glass pipes
  • flexible tubing
  • ring stand with clamp
  • lighter with adult help


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This experiment is for advanced students.


Don’t put this in your car….yet. Hydrogen generation, capture, and combustion are big deals right now. The next phase of transportation, and a move away from fossil fuels in not found in electric cars. Electric cars are waiting until hydrogen fuel cell vehicles become practical. It can be done and is being done.


Cars being powered by hydrogen are here, but not on the market yet. Engineers and chemists are always finding new ways to improve the chemical reaction that produces hydrogen and making the vehicles more efficiently use the fuel. Hydrogen fuel is not just easy to make, it is inexpensive, and the “exhaust” is water.


We will generate hydrogen in this lab. We will also see how combustible it is. Just let your imagination wander….just a bit and you will see noiseless cars and trucks zipping along the streets and interstates, carrying people and cargo. The Indianapolis 500 wouldn’t be quite the same, though. “And there they go, roaring, I mean quietly entering turn two…”


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Materials:


  • Goggles
  • Gloves
  • Measuring syringe
  • Water
  • Test tube rack
  • One-hole rubber stopper
  • Alcohol burner
  • Lighter
  • Test tube
  • Test tube holder
  • Water bath
  • Chemistry stand
  • Rubber tubing
  • 90 degree bend glass tubing
  • Zn powder (MSDS)
  • Copper sulfate CuSo4 (MSDS)
  • Sodium hydrogen sulfate NaHSO4 (MSDS) Sodium hydrogen sulfate is very toxic. Respect it, handle it carefully and responsibly. Do not take it for granted.

NOTE: Be very careful when handling the sodium hydrogen sulfate – it’s highly corrosive and dangerous when wet. Handle this chemical only with gloves, and be sure to read over the MSDS before using.


We will combine sodium hydrogen sulfate, water, and zinc. As soon as they are all together in our test tube, bubbles will begin forming in the solution. The bubbles will continue coming off, but we can speed up the reaction by adding a little copper sulfate. Now, instead of leisurely coming off, the gas is being given off quickly and we must act quickly ourselves to capture as much of the gas as possible. We can aid the gas movement ourselves by swirling the solution gently.


C3000: Experiment


Download Student Worksheet & Exercises


Here’s what’s going on in this experiment:


NaHSO4 + H2O + Zn + CuSO4 –> H2 + NaSO4 + CuHSO4 + ZnO


Sodium hydrogen sulfate is added to water and dissolved completely. Zinc is added and hydrogen gas is generated by the chemical reaction. Copper sulfate is added as a catalyst to speed up the generation of hydrogen.


Double replacement occurs where the compounds are broken apart and the pieces realign and re-bond with different parts of the original molecules, and zinc oxide is left as a byproduct of the oxidation of the zinc powder. Hydrogen gas is freed in the reaction.


Cleanup: We are going to clean everything thoroughly after we finish the lab. After cleaning with soap and water, rinse thoroughly. Chemists use the rule of “three” in cleaning glassware and tools. After washing, chemists rinse out all visible soap and then rinse three times more.


Storage: Place cleaned tools and glassware in their respective storage places.


Disposal: Liquids must be neutralized before they can be washed down the drain. Solids are thrown in the outside trash.


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Guar gum comes from the guar plant (also called the guaran plan), and people have found a lot of different and interesting uses for it.  It's one of the primary substitutes for fat in low-fat and fat-free foods. Cooks like to  use guar gum in foods as it has 8 times the thickening power of cornstarch, so much less is needed for the recipe. Ice cream makers use it to keep ice crystals from forming inside the carton. Doctors use it as a laxative for their patients.

When we teach kids how to make slime using guar gum, they call it "fake fat" slime, mostly because it's used in fat-free baking.  You can find guar gum in health food stores or order it online. We're going to whip up a batch of slime using this "fake fat". Ready?

Here's what you do:
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Download Student Worksheet & Exercises

  1. Fill a cup with 7 tablespoons of cold water.
  2. Stir in 1/4 teaspoon of guar gum, stir with a popsicle stick 10 times and stop, leaving the stick in.
  3. Cautiously dip a pinkie into the cup, then rub it in their fingers. Does it smell?
  4. Leave it for 2 minutes to thicken.
  5. In a fresh cup, mix 1 teaspoon borax (sodium tetraborate) in one tablespoon water.
  6. Add ½ teaspoon of the Borax Solution to the Guar solution. Stir and it will form a gel that looks like real boogers!

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The glue is a polymer, which is a long chain of molecules all hooked together like tangled noodles. When you mix the two solutions together, the water molecules start linking up the noodles together all along the length of each noodle to get more like a fishnet. Scientists call this a polymetric compound of sodium tetraborate and lactated glue. We call it bouncy putty.


Here’s what you do:


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  1. Combine ½ cup water with one teaspoon of Borax in a cup and stir with a popsicle stick.
  2. In another cup, mix equal parts white glue and water.
  3. Add in a glob of glue mixture to the borax.
  4. Stir for one second with a popsicle stick, then quickly pull the putty out of cup and play with it until it dries enough to bounce on table (3-5 minutes).
  5. Pick up an imprint from a textured surface or print from a newspaper, bounce and watch it stick, snap it apart quickly and ooze apart slowly.


Download Student Worksheet & Exercises
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This is looks like a chemical reaction but it’s not – it’s really just a physical change. It’s a really neat trick you can do for your friends or in a magic show. Here’s how it works:


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Download Student Worksheet & Exercises


You can use styrofoam beads, packing peanuts, styrofoam packing materials, or even a styrofoam cup and place it in your glass jar containing acetone. Styrofoam is made up of polystyrene foam, which is mostly air (that’s why foam is so lightweight). When you add the foam cup to the acetone, you’re removing the air in the foam which makes it look like you’re dissolving this huge amount of cups (you can go through a whole stack with only a cup of acetone).


Why does this work? You are removing the structure that supports the shape of the foam, and are left with only the foam molecules at the bottom of the container (it will look like a blob). Think about a camping tent: when you take away the poles, what happens to the tent? It loses its support structure and collapses down. The same thing is happening to the foam when you place it in the acetone – you are removing the structure that holds the shape. Acetone is found in most nail polish removers.
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This experiment is for advanced students.


Lewis and Clark did this same experiment when they reached the Oregon coast in 1805. Men from the expedition traveled fifteen miles south of the fort they had built at the mouth of the Columbia River to where Seaside, Oregon now thrives.


In 1805, however, it was just men from the fort and Indians. They built an oven of rocks. For six weeks, they processed 1,400 gallons of seawater, boiling the water off to gain 28 gallons of salt.


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Lewis and Clark National Historic Park commemorates the struggles of the expedition. (The reconstructed fort is also there to visit.) It is Fort Clatsop National Memorial, and is quite an experience to go through the fort.


Lewis and Clark went to great lengths to obtain salt. The men had been complaining that fish without salt had become something to avoid. Salt is important to us as well. It is a condiment, an addition to food that brings out the food’s natural flavor. Besides its food value, salt is used as a food preservative. It destroys bacteria in food by removing moisture from their “bodies” and killing them.


Sodium chloride, table salt, NaCl….they’re all acceptable names for salt. If NaCl is broken down into its component elements, the elements don’t act like our friend salt. Its components are sodium and chlorine.


Sodium is a highly reactive alkali metal, element #11 on the periodic table. It is exothermic in water, which means that is gives of heat as it reacts with water. Small pieces tossed into water will react with it. The sodium particles give off heat that melts them into round balls. The sodium particles bounce and scurry around the surface at a high rate of speed. If you ever get the chance to observe this, do it. The reaction continues until the sodium is gone. Sodium, as it reacts with the water, changes chemically into sodium hydroxide. These cool things that sodium does are also dangerous. Sodium and sodium hydroxide are caustic…they are so pH basic that they will burn you.


Chlorine is a halogen, group 17, element #17. Chlorine is used in bleach, disinfectants, and in swimming pool maintenance. It seems that anywhere you want to remove color or life, chlorine is your element. This property of chlorine to kill was used in war. (It would react with the mucous linings in their throat, undergoing a chemical reaction to turn into hydrochloric acid in their throats. Hydrochloric acid is a very dangerous acid, usually fatal once inside you.) Chlorine is known as bleach at home. Never, never, drink it or breathe its fumes.


Materials:


  • Goggles
  • Gloves
  • Jar or glass
  • 2 90o glass tubes
  • Chemistry stand
  • Rubber tubing
  • Test tube clamp
  • Erlenmeyer flask
  • One-hole rubber stopper
  • Wire screen
  • Alcohol burner
  • Lighter
  • Test tube
  • Water
  • Saltwater
  • Heating rod

Look out for the hot flask and other glassware. Allow everything to cool before cleaning.


When done heating, move the rubber tubing out of the water. There is a difference in pressure between the heated glassware and the water bath. That difference in pressure will cause the water to enter the tubing and cool water will flow into the hot glassware and could cause catastrophic damage to the glassware.


Never…Never!….drink the results of an experiment. Yeah, I know that plain old water is supposed to be in the test tube, but follow the experiment’s safety guidelines. You’ve had other stuff in that test tube, too.


C3000: Experiment 83


Here’s what’s going on in this experiment:


That flask of saltwater will start to boil, and water vapor will leave the flask and travel to the test tube. There is no chemical change occurring in this experiment, but a physical one. A physical change involves a change in state (melting, freezing, vaporization, condensation, sublimation). Physical changes are things like crushing a can, melting an ice cube, breaking a bottle, or boiling saltwater until there is nothing left but salt and steam.


Cleanup: Clean everything thoroughly after you are finished with the lab. After cleaning with soap and water, rinse thoroughly. Chemists use the rule of “three” in cleaning glassware and tools. After washing, chemists rinse out all visible soap and then rinse three times more.


Storage: Place cleaned tools and glassware in their respective storage places.


Disposal: Liquids can be washed down the drain


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Have you ever tried washing dishes without soap? It doesn’t work well, especially if there’s a lot of grease, fat, or oil on the dish!


The oils and fats are slippery and repel water, which makes them a great choice for lubration of bearing and wheels, but lousy for cleaning up after dinner.


So what’s inside soap that makes it clean off the dish? The soap molecule looks a lot like a snake, with a head and a tail. The long tail loves oil (hydrophobic) and the head loves water (hydrophilic). The hydrophilic end dissolves in water and the hydrophobic end wraps itself around fat and oil in the dirty water, cleaning it off your dishes.


Let’s do an experiment that will really make you appreciate soap and fat:


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Materials:


  • whole milk (if you have it – otherwise, use lowfat)
  • food dye
  • bowl
  • liquid soap


 


Download Student Worksheet & Exercises


While it may not look like it (or taste like it), milk is mostly water with minerals, proteins, and fat trapped inside. When you add a drop of soap, the hydrophobic end races around and grabs the fat and links up with other tail ends of soap molecules, forming the colors you see in the dish. The higher the fat content of your milk, the longer the show.
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If you’ve ever burped, you know that it’s a lot easier to do after chugging an entire soda. Now why is that?


Soda is loaded with gas bubbles — carbon dioxide (CO2), to be specific. And at standard temperature (68oF) and pressure (14.7 psi), carbon dioxide is a gas. However, if you burped in Antarctica in the wintertime, it would begin to freeze as soon as it left your lips. The freezing temperature of CO2 is -109oF, and Antarctic winters can get down to -140oF. You’ve actually seen this before, as dry ice (frozen burps!).


Carbon dioxide has no liquid state at low pressures (75 psi or lower), so it goes directly from a block of dry ice to a smoky gas (called sublimation). It’s also acidic and will turn cabbage juice indicator from blue to pink. CO2 is colorless and odorless, just like water, but it can make your mouth taste sour and cause your nose to feel as if it’s swarming with wasps if you breathe in too much of it (though we won’t get anywhere near that concentration with our experiments).


The triple point of CO2 (the point at which CO2 would be a solid, a liquid, and a gas all at the same time) is around five times the pressure of the atmosphere (75 psi) and around -70oF. (What would happen if you burped then?)


What sound does a fresh bottle of soda make when you first crack it open? PSSST! What is that sound? It’s the CO2 (carbon dioxide) bubbles escaping. What is the gas you exhale with every breath? Carbon dioxide. Hmmm … it seems as if your soda is already pre-burped. Interesting.


We’ll actually be doing a few different experiments, but they all center around producing burps (carbon dioxide gas). The first experiment is more detective work in finding out where the CO2 is hiding. With the materials we’ve listed (chalk, tile, limestone, marble, washing soda, baking soda, vinegar, lemon juice, etc. …) and a muffin tin, you can mix these together and find the bubbles that form, which are CO2. (Not all will produce a reaction.) You can also try flour, baking powder, powdered sugar, and cornstarch in place of the baking soda. Try these substitutes for the vinegar: water, lemon juice, orange juice, and oil.


Materials:


  • baking soda
  • chalk
  • distilled white vinegar
  • washing soda
  • disposable cups and popsicle sticks

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Download Student Worksheet & Exercises


The next video (below) is a BONUS video for you – can you find the items around your house so you can make your own scale? (If you generate a lot of CO2, you can simply use paper grocery bags suspended on both ends of a broom handle (disconnect the broom part first). Suspend the center of the broom handle from a length of string for pin-point accuracy.


The second part of this experiment (video below) compares the weight of air with the weight of carbon dioxide. Make sure your balance is free to move easily when the lightest touch (your breath) is applied to one of the scales. You can use grocery bags attached to the ends of a broom handle for a larger scale, or modify tiny cups with string and pencils (as shown in the video). Either one works, but you’ll want to be sure the bubbles are (mostly) popped before you pour. And pour carefully or you’ll slosh out the invisible CO2 gas.


You can create the CO2 gas in a variety of ways (the image at right shows dry ice submerged in water), including the standard vinegar and baking powder method. Here is another option: Open a 2-liter bottle of soda and quickly pour it into a big pitcher so that it foams up to the top of the container. Carefully pour the gas from the pitcher into the balance. What happens?


Fire extinguisher variation: You can create a fire extinguisher by “pouring” the CO2 gas onto a lit candle to snuff it out.


Materials:


  • baking soda
  • distilled white vinegar
  • two disposable cups
  • large container
  • two water bottles or stacks of books
  • two long pencils or skewers
  • string


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This experiment is for advanced students. This lab builds on concepts from the previous carbon dioxide lab.


Limewater….carbon dioxide…indicators. We don’t know too much about these things. Sure, we know a little. Carbon dioxide is exhaled by us and plants need it to grow. Burning fossil fuels produces carbon dioxide.


Indicators…something we observe that confirms to us that something specific is happening. Lime water turns cloudy and forms a precipitate in the presence of carbon dioxide. Blue litmus paper turns red in the presence of an acid. The dog barking at the door and dancing around indicates that you better let the dog out, and quick, to avoid….a pet spill?


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Materials:


  • Limewater from a previous lab (MSDS)
  • One-hole rubber stopper
  • 900 bend glass tubing
  • Test tube rack
  • 2 Test tubes
  • Sodium hydrogen sulfate (NaHSO4) (MSDS) Sodium hydrogen sulfate is very toxic. Respect it, handle it carefully and responsibly. Do not take it for granted.
  • Sodium carbonate (Na2CO3) (MSDS)

NOTE: Be very careful when handling the sodium hydrogen sulfate – it’s highly corrosive and dangerous when wet.  Handle this chemical only with gloves, and be sure to read over the MSDS before using.


When pouring our limewater into the test tube, be careful! Limewater is dangerous to your skin and your nasal passages. Pour just the limewater into the test tube, not any solids that may have gotten into the limewater container.


A chemical reaction will occur between sodium hydrogen sulfate, sodium carbonate, and water. We could have used any combination of chemicals for this lab that will produce carbon dioxide (CO2), but these chemicals are already in our kits, so……


The reaction will create a gas, that gas, we think, is carbon dioxide. If we are right, we will be bubbling CO2 gas into lime water. If we observe the limewater becoming cloudy and if a precipitate forms on the bottom of the test tube, that is a positive indicator that CO2 is present.


C3000: Experiment 31


Here’s what’s going on in this experiment:


Some combination of chemicals will produce carbon dioxide –> CO2 + ?


Notice that specific chemicals are not in the chemical equation? The actual chemistry of the chemical reaction is not our focus in this lab. We want to experience how an indicator can test for a particular compound or element.


Instead of sodium hydroxide and sodium carbonate and water, we could choose to combine vinegar and baking soda for example. Even simple household supplies can be chemicals for our experiments.


Cleanup: We are going to clean everything thoroughly after we finish the lab. After cleaning with soap and water, rinse thoroughly. Chemists use the rule of “three” in cleaning glassware and tools. After washing, chemists rinse out all visible soap and then rinse three times more.


Storage: Place cleaned tools and glassware in their respective storage places.


Disposal: Liquids can be washed down the drain. Solids are thrown in the trash.


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CAUTION!! Be careful with this!! This experiment uses a knife AND a microwave, so you’re playing with things that slice and gets things hot. If you’re not careful you could cut yourself or burn yourself. Please use care!


We’re going to create the fourth state of matter in your microwave using food.  Note – this is NOT the kind of plasma doctors talk about that’s associated with blood.  These are two entirely different things that just happen to have the same name.  It’s like the word ‘trunk’, which could be either the storage compartment of a car or an elephant’s nose.  Make sense?


Plasma is what happens when you add enough energy (often in the form of raising the temperature) to a gas so that the electrons break free and start zinging around on their own.  Since electrons have a negative charge, having a bunch of free-riding electrons causes the gas to become electrically charged.  This gives some cool properties to the gas.  Anytime you have charged particles (like naked electrons) off on their own, they are referred to by scientists as ions.  Hopefully this makes the dry textbook definition make more sense now (“Plasma is an ionized gas.”)


So here’s what you need:


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  • microwave (not a new or expensive one)
  • a grape
  • a knife with adult help


 
Download Student Worksheet & Exercises


1. Carefully cut the grape almost in half. You want to leave a bit of skin connecting the two halves.


2. Open the grape like a book. In other words, so that the two halves are next to one another still attached by the skin.


3. Put the grape into the microwave with the outside part of the grape facing down and the inside part facing up.


4. Close the door and set the microwave for ten seconds. You may want to dim the lights in the room.


s2You should see a bluish or yellowish light coming from the middle section of the grape. This is plasma! Be careful not to overcook the grape. It will smoke and stink if you let it overcook. Also, make sure the grape has time to cool before taking it out of the microwave.


Other places you can find plasma include neon signs, fluorescent lights, plasma globes, and small traces of it are found in a flame.


Note: This experiment creates a momentary, high-amp short-circuit in the oven, a lot like shorting your stereo with low-resistance speakers. It’s not good to operate a microwave for long periods with little to nothing in them.  This is why we only do it for a few seconds. While this normally isn’t a problem in most microwaves, don’t do this experiment with an expensive microwave or one that’s had consistent problems, as this might push it over the edge.


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We're going to watch how density works by making a simple lava lamp that doesn't need electricity! If you like to watch blob-type shapes shift and ooze around, then this is something you're going to want to experiment with.  but don't feel that you have to use the materials mentioned below - feel free to experiment with other liquids you have around the house, and be sure to let me know what you've found in the comment section below.

All you need is about 10 minutes and a few quick items you already have around the house.  Are you ready?

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  • empty glass jar with straight sides (if possible)
  • vegetable oil
  • salt
  • water
  • food dye


Fill a water glass halfway with colored water, and add a 1/2" layer of oil on top. Shake salt over the oil layer and watch the lava lamp start to work! You'll see the bottom oil layer move as a salt-oil-drop falls to the bottom of the glass. Over a few minutes, the oil breaks free of the salt and moves back up to rejoin the oil layer on top.



Download Student Worksheet

What's happening? You're actually watching the salt itself fall through the oil. However, the oil sticks to the salt to form a larger object, and since the salt is heavier than oil and water, the whole mess plunks to the bottom of the glass. At the bottom of your cup, the oil breaks free of the salt (eventually) and rises back up. Does it matter if you heat the oil, chill the water, or vice versa? Is there anything that works better than salt?

Going Further: Unscrew the camp and add a broken-up effervescent tablet (like alka-seltzer) to your bottle. Cap it and watch what happens! Did it react with water, oil or both? What if you turn off the lights and shine a flashlight through it? [/am4show]

Density is basically how tightly packed atoms are. (Mathematically, density is mass divided by volume.) For example, take a golf ball and a ping pong ball. Both are about the same size or, in other words, take up the same volume.


However, one is much heavier, has more mass, than the other. The golf ball has its atoms much more closely packed together than the ping pong ball and as such the golf ball is denser.


These are quick and easy demonstrations for density that use simple household materials:
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Density Jar

You will need to find:


  • glass jar
  • water
  • vegetable oil
  • liquid dish soap
  • honey
  • corn syrup
  • molasses
  • rubbing alcohol
  • lamp oil (optional)

Fill a clear glass partway with water. Drizzle in cooking oil. What do you see happening? Try adding in liquid dish soap (make sure it’s a different color form the water and the oil for better visibility.)


What else can you add in? What about honey, corn syrup, molasses, rubbing alcohol, or lamp oil? Use a turkey baster to help you pour the liquids in very slowly so they don’t mix. You’ll get the best results if you start with the heaviest liquids.



 
Download Student Worksheet & Exercises


Hot & Cold Swirl

To clearly illustrate how hot and cold air don’t mix, find two identical glasses.  Fill one glass to the brim with hot water.  Add a drop or two of red food coloring and watch the patterns.  Now fill the other glass to the top with very cold water and add drops of blue dye.  Do you notice a difference in how the food coloring flows?


Get a thick sheet of heavy paper (index cards work well) and use it to cap the blue glass.  Working quickly, invert the glass and stack it mouth-to-mouth with the red glass.  This is the tricky part: When the glasses are carefully lined up, remove the card.  Is it different if you invert the red glass over the blue?


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Did you know that most people can’t crack an egg with only one hand without whacking it on something? The shell of an egg is quite strong! Try this over a sink and see if you can figure out the secret to cracking an egg in the palm of your hand…(Hint: the answer is below the video – check it out after you’ve tried it first!)


How can you tell if an egg is cooked or raw? Simply spin it on the counter and you’ll get a quick physics lesson in inertia…although you might not know it. A raw egg is all sloshy inside, and will spin slow and wobbly. A cooked egg is all one solid chunk, so it spins quickly. Remember the Chicken and the Clam experiment?


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Materials:


  • hard-boiled egg
  • glass
  • water
  • salt


Download Student Worksheet & Exercises
This experiment is all about density. Density is basically how tightly packed atoms are. Mathematically, density is mass divided by volume. In other words, it is how heavy something is, divided by how much space it takes up. If you think about atoms as marbles (which we know they’re not from the last lessons but it’s a useful model), then something is more dense if its marbles are jammed close together.


For example, take a golf ball and a ping pong ball. Both are about the same size or, in other words, take up the same volume. However, one is much heavier, has more mass, than the other. The golf ball has its atoms much more closely packed together than the ping pong ball and as such the golf ball is denser.


Here’s a riddle: Which is heavier, a pound of bricks or a pound of feathers? Well, they both weigh a pound so neither one is heavier! Now, take a look at it this way, which is denser, a pound of bricks or a pound of feathers? Aha! The pound of bricks is much denser since it takes up much less space. The bricks and the feathers weigh the same but the bricks take up a much smaller volume. The atoms in a brick are much more squooshed together then the atoms in the feathers.


Back to the experiment – have you ever noticed you how float a lot easier in the ocean than the lake? If so, then you already know how salt can affect the density of the water. Saltwater is more dense that regular water, and your body tissues contain water (among other things).


Did you know that thinner people are more dense than heavier people? For example, championship swimmers will sink and have to work harder to stay afloat, but the couch potato next door will float more easily in the water.
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soapWhen you warm up leftovers, have you ever wondered why the microwave heats the food and not the plate? (Well, some plates, anyway.) It has to do with the way microwaves work.


Microwaves generate high energy electromagnetic waves that when aimed at water molecules, makes these molecules get super-excited and start bouncing around a lot.


We see this happen when we heat water in a pot on the stove. When you add energy to the pot (by turning on the stove), the water molecules start vibrating and moving around faster and faster the more heat you add. Eventually, when the pot of water boils, the top layer of molecules are so excited they vibrate free and float up as steam.


When you add more energy to the water molecule, either by using your stove top or your nearest microwave,  you cause those water molecules to vibrate faster. We detect these faster vibrations by measuring an increase in the temperature of the water molecules (or in the food containing water). Which is why it’s dangerous to heat anything not containing water in your microwave, as there’s nowhere for that energy to go, since the electromagnetic radiation is tuned to excite water molecules.


To explain this to younger kids (who might confuse radio waves with sounds waves) you might try this:


There’s light everywhere, some of which you can see (like rainbows) and others that you can’t see (like the infrared beam coming from your TV remote, or the UV rays from the sun that give you a sunburn). The microwave shoots invisible light beams at your food that are tuned to heat up the water molecule.


The microwave radiation emitted by the microwave oven can also excite other polarized molecules in addition to the water molecule, which is why some plates also get hot. The soap in this experiment below will show you how a bar of Ivory soap contains air, and that air contains water vapor which will get heated by the microwave radiation and expand. Are you ready?


Here’s what you need:


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  • bar of Ivory soap
  • microwave (not a new or expensive one)
  • plate (optional)

The following experiment is a quick example of this principle using a naked bar of Ivory soap. The trick is to use Ivory, which contains an unusually high amount of air. Since air contains water moisture, Ivory also has water hidden inside the bar of soap. The microwave will excite the water molecules and your kids will never look at the soap the same way again.



 
Download Student Worksheet & Exercises


Toss a naked bar of Ivory soap onto a glass or ceramic plate and stick it into the microwave (don’t use a new or expensive microwave!) on HIGH for 2-3 minutes. Watch intently and remove when it reaches a “maximum”. Be careful when you touch it after taking it out of the microwave oven – it may still hold steam inside. You can still use the soap and the microwave after this experiment!


Note: Scientists refer to ‘light’ as the visible part of the electromagnetic spectrum, where radio and microwaves are lower energy and frequency than light (and the height of the wave can be the size of a football field). Gamma rays and x-rays are higher energy and frequency than light (these tend to pass through mirrors rather than bounce off them. More on that in Unit 9.)


Exercises


  1.  What is it in your food (and the soap) that is actually heated by the microwave?
  2.  How does a microwave heat things?
  3.  Touch the soap after it has been allowed to cool for a few minutes and record your observations.

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If you soak chicken bones in acetic acid (distilled vinegar), you’ll get rubbery bones that are soft and pliable as the vinegar reacts with the calcium in the bones. This happens with older folks when they lose more calcium than they can replace in their bones, and the bones become brittle and easier to break. Scientists have discovered calcium is replaced more quickly in bodies that exercise and eating calcium rich foods, like green vegetables.


This is actually two experiments in one – here’s what you need to do:


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Materials:


  • hard boiled egg
  • glass or clean jar
  • distilled white vinegar


Download Student Worksheet & Exercises


When you first plop the egg in the vinegar, do you notice the tiny bubbles? The acetic acid (distilled vinegar) reacts with the calcium carbonate in the eggshell, and you may even notice a color change over a couple of days.


How high does your egg bounce? Does it matter how long you leave it in the vinegar for?


The second part of this experiment is to try this again, but now use a raw egg (wash your hands after handling your egg due to salmonella!) You’ll get a difference result – the eggshell will become flexible, but don’t bounce them.


Exercises


  1. Describe what the eggshell looked like before the reaction.
  2. Describe the acetic acid
  3. The product you witnessed in this chemical reaction was carbon dioxide, a colorless, odorless gas. How can you tell there really was a chemical reaction?
  4. Why did the egg turn to “rubber?”

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A non-Newtonian fluid is a substance that changes viscosity, such as ketchup.  Ever notice how ketchup sticks to the bottom of the bottle one minute and comes sliding out the next?


Think of viscosity as the resistance stuff has to being smeared around.   Water is “thin” (low viscosity); honey is “thick” (high viscosity).  You are about to make a substance that is both (low and high viscosity), depending on what ratio you mix up. Feel free to mix up a larger batch then indicated in the video – we’ve heard from families that have mixed up an entire kiddie pool of this stuff!


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  • cornstarch (about 2 cups)
  • water (about 1 cup)
  • sand (about 2 cups)

Your first step is to create a 2:1 ratio of cornstarch to water (2 cups cornstarch to 1 cup water).  (This is your non-Newtonian fluid.)  Grab it with your fist and it will turn rock-solid and crumble; open your hand and it will flow right between your fingers. It’s both a solid and a liquid (it changes viscosity depending on its environment, which is your hand right now).  By adding sand to this concoction, you can make moon sand.



 
Download Student Worksheet & Exercises


Moon sand is basically clay with a beach twist.  If you’ve ever tried making a sand castle, you know the disappointment of having the structure crumble after hours of work.  Moon sand adds the best properties of clay to the sand for a moldable, sandy texture that’s easy to work with — and it’s dirt cheap to mix up your weight in moon sand.


Your task is to find the perfect ratio of the three ingredients to make this weird substance.  If you have too much water, you’ll get a substance that is both a liquid and a solid (as you did before with the non-Newtonian fluid).  Too much solid, and it crumbles.


Troubleshooting: The smaller the grain of sand you have, the easier it is to form intricate shapes.  If you find white sand, it’ll make better colors when you add food dye to the mixture. Use a large enough bowl and try to keep one hand clean so you can add more (of whatever you need) as you go along.  The ideal mixture is approximately 2 cups sand, 2 cups cornstarch, and 1 cup water, give or take a bit.  Notice how adding just a small amount of water turns it into a liquid, and adding a tiny bit more cornstarch (or sand) makes it crumble as if it were solid?  Take your time to get this mixture just right. (We’ve filled up an entire plastic kiddie pool with this stuff!)
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Can we really make crystals out of soap?  You bet!  These crystals grow really fast, provided your solution is properly saturated.  In only 12 hours, you should have sizable crystals sprouting up.


You can do this experiment with either skewers, string, or pipe cleaners.  The advantage of using pipe cleaners is that you can twist the pipe cleaners together into interesting shapes, such as a snowflake or other design.  (Make sure the shape fits inside your jar. )


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Here’s what you need:


  • pipe cleaners (or string or skewer)
  • cleaned out pickle, jam, or mayo jar
  • water
  • borax (AKA sodium tetraborate)
  • adult help, stove, pan, and stirring spoon

Here’s what you do:


1. Cut a length of string and tie it to your pipe cleaner shape; tie the other end around a pencil or wooden skewer. You want the shape suspended in the jar, not touching the bottom or sides.


2. Bring enough water to fill the jar (at least 2 cups) to a boil on the stove (food coloring is fun, but entirely optional).


3. Add 1 cup of borax (aka sodium tetraborate or sodium borate) to the solution, stirring to dissolve. If there are no bits settling to the bottom, add another spoonful and stir until you cannot dissolve any more borax into the solution. When you see bits of borax at the bottom, you’re ready.  (You’ll be adding in a lot of borax, which is why we asked you to get a full box). You have made a supersaturated solution.  Make sure your solution is saturated, or your crystals will not grow.


4. Wait until your solution has cooled to about 130oF (hot to the touch, but not so hot that you yank your hand away). Pour this solution (just the liquid, not the solid bits) into the jar with the shape.  Put the jar in a place where the crystals can grow undisturbed overnight, or even for a few days.  Warmer locations (such as upstairs or on top shelves) is best.



Download worksheet and exercises


DO  NOT EAT!!! Keep these crystals out of reach of small kids, as they look a lot like the Rock Candy Crystals.


Here are photos from kids ages 2, 7, 9 that made their own! Great job to the Fluker Family!!


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This is a recording of a recent live teleclass I did with thousands of kids from all over the world. I’ve included it here so you can participate and learn, too! (Click here if you’re looking for the more recent version that also includes Chemical Engineering.)


When you think of slime, do you imagine slugs, snails, and puppy kisses? Or does the science fiction film The Blob come to mind? Any way you picture it, slime is definitely slippery, slithery, and just plain icky — and a perfect forum for learning real science. But which ingredients work in making a truly slimy concoction, and why do they work? Let’s take a closer look…


Materials:


  • Click to download worksheet
  • Sodium tetraborate (also called “Borax” – it’s a laundry whitener) – about 2 tablespoons
  • Clear glue or white glue (clear works better if you can find it) – about 1/2 cup
  • Yellow highlighter
  • Pliers or sharp razor (with adult help). (PREPARE: Use this to get the end off your highlighter before class starts so you can extract the ink-soaked felt inside. Leave the felt inside highlighter with the end loosely on (so it doesn’t dry out))
  • Resuable Instant Hand Warmer that contains sodium acetate (Brand Name: EZ Hand Warmer) – you’ll need two of these
  • Scissors
  • Glass half full of COLD water (PREPARE: put this in the fridge overnight)
  • Mixing bowl full of ice (PREPARE: leave in freezer)
  • Salt
  • Disposable aluminum pie place or foil-wrapped paper plate
  • Disposable cups for solutions (4-6)
  • Popsicle sticks for mixing (4-6)
  • Rubber gloves for your hands
  • Optional: If you want to see your experiments glow in the dark, you’ll need a fluorescent UV black light (about $10 from the pet store – look in cleaning supplies under “Urine-Off” for a fluorescent UV light). UV flashlights and UV LEDs will not work.

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Key Concepts

If you’ve ever mixed together cornstarch and water, you know that you can get it to be both a liquid and a solid at the same time. (If you haven’t you should definitely try it! Use a 2:1 ratio of cornstarch:water.) The long molecular chains (polymers) are all tangled up when you scrunch them together (and the thing feels solid), but the polymers are so slick that as soon as you release the tension, they slide free (and drips between your fingers like a liquid).


Scientists call this a non-Newtonian fluid. You can also fill an empty water bottle or a plastic test tube half-full with this stuff and cap it. Notice that when you shake it hard, the slime turns into a solid and doesn’t slosh around the tube. When you rotate the tube slowly, it acts like a liquid.


Long, spaghetti-like chains of molecules (called polymers) don’t clump together until you cross-link the molecule strands (polymers) together into something that looks more like a fishnet. This is how we’re going to make slime.


What’s Going On?

Imagine a plate of spaghetti. The noodles slide around and don’t clump together, just like the long chains of molecules (called polymers) that make up slime. They slide around without getting tangled up. The pasta by itself (fresh from the boiling water) doesn’t hold together until you put the sauce on. Slime works the same way. Long, spaghetti-like chains of molecules don’t clump together until you add the sauce – something to cross-link the molecule strands together.


The borax mixture holds the glue mixture together in a gloppy, gelatinous mass. In more scientific terms, the sodium tetraborate cross-links the long polymer chains in the glue to form the slime.


Why does the slime glow? Note that a black light emits high-energy UV light. You can’t see this part of the spectrum (just as you can’t see infrared light, found in the beam emitted from the remote control to the TV), which is why “black lights” were named that. Stuff glows because fluorescent objects absorb the UV light and then spit light back out almost instantaneously. Some of the energy gets lost during that process, which changes the wavelength of the light, which makes this light visible and causes the material to appear to glow.


Questions to Ask

  1. What happens when you freeze your slime? Is there a color change?
  2. How long does it take to thaw your slime in the microwave?
  3. Do you see the little bubbles in your slime?
  4. How many states of matter do you have in your slime now?
  5. Does this work with any laundry detergent, or just borax?
  6. What happens if you omit the water in the 50-50- glue-water mixture, and just use straight glue? (Hint – use the glow juice with the borax to keep the glowing feature.)
  7. Does your slime pick up newsprint from a newspaper?
  8. What other kinds of glue work well with this slime?

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Did you know you can create a compound microscope and a refractor telescope using the same materials? It’s all in how you use them to bend the light. These two experiments cover the fundamental basics of how two double-convex lenses can be used to make objects appear larger when right up close or farther away.


Things like lenses and mirrors can bend and bounce light to make interesting things, like compound microscopes and reflector telescopes. Telescopes magnify the appearance of some distant objects in the sky, including the moon and the planets. The number of stars that can be seen through telescopes is dramatically greater than can be seen by the unaided eye.


Materials


  • A window
  • Dollar bill
  • Penny
  • Two hand-held magnifying lenses
  • Ruler

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Download Student Worksheet & Exercises


  1. Place a penny on the table.
  2. Hold one magnifier above the penny and look through it.
  3. Bring the second magnifying lens above the first so now you’re looking through both. Move the second lens closer and/or further from the penny until the penny comes into sharp focus. You’ve just made a compound microscope.
  4. Who’s inside the building on an older penny?
  5. Try finding the spider/owl on the dollar bill. (Hint: It’s in a corner next to the “1”.)
  6. Keeping the distance between the magnifiers about the same, slowly lift up the magnifiers until you’re now looking through both to a window.
  7. Adjust the distance until your image comes into sharp (and upside-down) focus. You’ve just made a refractor telescope, just like Galileo used 400 years ago.
  8. Find eight different items to look at through your magnifiers. Make four of them up-close so you use the magnifiers as a microscope, and four of them far-away objects so you use the magnifiers like a telescope. Complete the data table.

What’s Going On?

What I like best about this activity is how easily we can break down the basic ideas of something that seems much more complex and intimidating, like a telescope or microscope, in a way that kids really understand.


When a beam of light hits a different substance (like a window pane or a lens), the speed at which the light travels changes. (Sound waves do this, too!) In some cases, this change turns into a change in the direction of the beam.



For example, if you stick a pencil is a glass of water and look through the side of the glass, you’ll notice that the pencil appears shifted. The speed of light is slower in the water (140,000 miles per second) than in the air (186,282 miles per second). This is called optical density, and the result is bent light beams and broken pencils.


You’ll notice that the pencil doesn’t always appear broken. Depending on where your eyeballs are, you can see an intact or broken pencil. When light enters a new substance (like going from air to water) perpendicular to the surface (looking straight on), refractions do not occur.


However, if you look at the glass at an angle, then depending on your sight angle, you’ll see a different amount of shift in the pencil. Where do you need to look to see the greatest shift in the two halves of the pencil?


Why does the pencil appear bent? Is it always bent? Does the temperature of the water affect how bent the pencil looks? What if you put two pencils in there?


Depending on if the light is going from a lighter to an optically denser material (or vice versa), it will bend different amounts. Glass is optically denser than water, which is denser than air.


Not only can you change the shape of objects by bending light (broken pencil or whole?), but you can also change the size. Magnifying lenses, telescopes, and microscopes use this idea to make objects appear different sizes.


Exercises


  1. Can light change speeds?
  2. Can you see ALL light with your eyes?
  3. Give three examples of a light source.
  4. What’s the difference between a microscope and a telescope?
  5. Why is the telescope image upside-down?

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Helioseismology is the study of wave oscillations in the Sun. By studying the waves, scientists can tell what’s going on inside the Sun. It’s like studying earthquakes to learn what’s going on inside the earth. The Sun is filled with sound, and studying these sound waves is currently the only way scientists can tell what’s going on inside, since the light we see from the Sun is just from the upper surface.


Molecules are vibrating back and forth at fairly high rates of speed, creating waves. Energy moves from place to place by waves. Sound energy moves by longitudinal waves (the waves that are like a slinky). The molecules vibrate back and forth, crashing into the molecules next to them, causing them to vibrate, and so on and so forth. All sounds come from vibrations.


Materials


  • Musical instruments: triangles, glass bottles that can be blown across, metal forks, tuning forks, recorders, jaw harps, harmonicas, etc. Whatever you have will work fine.

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Download Student Worksheet & Exercises


  1. Your teacher will pull out a bin of musical instruments of various types.
  2. Assign one student to be the noisemaker. The rest will listen with their eyes closed and record their observations.
  3. Everyone shuts their eyes except for the noise maker.
  4. The noisemaker selects an instrument and plays it once. Everyone else listens.
  5. The noisemaker selects another instrument and plays it once. Everyone listens.
  6. The noisemaker selects a third instrument and plays it once. Everyone listens.
  7. The noisemaker selects one of the three instruments and plays it as it moves. For example, if you’re playing the triangle, you can hit it and spin it. Or hit it as you are walking past the closed-eye listeners. Sound changes when the object is moving, so make the sound they hear appear to be different somehow.
  8. The noisemaker puts the instruments back and everyone opens their eyes and records their data in the table.
  9. Switch roles and find a new noisemaker for the next trial. Repeat steps 2-8.

What’s Going On?

The Sun is like the biggest musical instrument you’ve ever seen. A piano has 88 keys, which means you can play 88 different musical notes. The Sun has 10 million.


To play a guitar, you pluck one of the six strings. To play the piano, you hit a key and sound comes out. To play the flute, you blow across a hole. Drums require smacking things together. So how do you play the Sun?


Molecules are vibrating back and forth at fairly high rates of speed, creating waves. Energy moves from place to place by waves. Sound energy moves by longitudinal waves (the waves that are like a slinky). The molecules vibrate back and forth, crashing into the molecules next to them, causing them to vibrate, and so on and so forth. All sounds come from vibrations.


Waves are the way energy moves from place to place. Sound moves from a mouth to an ear by waves. Light moves from a light bulb to a book page to your eyes by waves. Waves are everywhere. As you sit there reading this, you are surrounded by radio waves, television waves, cell phone waves, light waves, sound waves and more. (If you happen to be reading this in a boat or a bathtub, you’re surrounded by water waves as well.) There are waves everywhere!


Do you remember where all waves come from? Vibrating particles. Waves come from vibrating particles and are made up of vibrating particles.


Here’s rule one when it comes to waves….the waves move, the particles don’t. The wave moves from place to place. The wave carries the energy from place to place. The particles however, stay put. Here are a couple of examples to keep in mind.


If you’ve ever seen a crowd of people do the “wave” in the stands of a sporting event you may have noticed that the people only “vibrated” up and down. They did not move along the wave. The wave, however, moved through the stands.


Another example would be a duck floating on a wavy lake. The duck is moving up and down (vibrating) just like the water particles but he is not moving with the waves. The waves move, but the particles don’t. When I talk to you, the vibrating air molecules that made the sound in my mouth do not travel across the room into your ears. (Which is especially handy if I’ve just eaten an onion sandwich!) The energy from my mouth is moved, by waves, across the room.


Convection starts the waves moving. You’ve seen convection when a hot pot of water bubbles up. You can even hear it when it starts to boil if you listen carefully. Just below the surface of the Sun, the energy that started deep in the core has bubbled up to the surface to make gigantic bubbles emerge that are bigger than the state of Alaska. It’s also a noisy process, and the sound waves stay trapped beneath the surface, making waves appear on the surface of the Sun. This makes the Sun’s surface look like it’s moving up and down.


Scientists use special cameras to watch the surface of the Sun wiggle and move, and they look for patterns so they can determine what’s going on down inside the Sun. Since the sound is inside the Sun under the part we can see, we use sound to discover what’s inside the Sun.


Have you ever heard the Sun? The video is an actual recording of the song of the Sun.


If you’ve ever been inside an unfurnished room, you’ve heard echoes indoors. Sound bounces all around the room, just like it does inside the surface of the Sun.


Can sound waves travel through space? No. Sound requires a medium to travel through, since it travels by vibrating molecules, and there aren’t enough molecules in space to do this with (there are a couple random ones floating around here and there, but way too far apart to be useful for sound waves).


If you have a slinky, take it out and stretch it out to its full length on the table or the ground, asking someone to help you hold one end. Now move the slinky quickly to the left and back again, and watch the wave travel down the length and return. Now move your end quickly up and then back down the table, making a longitudinal wave. When this wave finishes, take your end and shove it quickly toward your helper, then pull back again to make a compression wave. Point out to the student how when the wave returns, it’s an echo. That’s what happens inside the Sun when the sound waves hit the surface of the Sun. They don’t go through the surface, but get trapped beneath it as they echo off the inside surface of the Sun.


Exercises


  1.  What did you notice that is different about the sounds you heard?
  2.  How can you tell that two sounds are different that came from the same instrument? (Movement causes sound waves to sound different.)
  3. What did you notice about your guesses? What kind of instruments were you more correct about?

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A meteoroid is a small rock that zooms around outer space. When the meteoroid zips into the Earth’s atmosphere, it’s now called a meteor or “shooting star”. If the rock doesn’t vaporize en route, it’s called a meteorite as soon as it whacks into the ground. The word meteor comes from the Greek word for “high in the air.”


Meteorites are black, heavy (almost twice the normal rock density), and magnetic. However, there is an Earth-made rock that is also black, heavy, and magnetic (magnetite) that is not a meteorite. To tell the difference, scratch a line from both rocks onto an unglazed tile. Magnetite will leave a mark whereas the real meteorite will not.


Materials


  • White paper
  • Strong magnet
  • Handheld magnifying glass (optional)

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Download Student Worksheet & Exercises


  1. Imagine you are going on a rock hunt. You are to find which rocks are meteorites and which are Earth rocks. If you don’t have access to rock samples, just watch the experiment video of the different rock samples. If you’d like to make your own sample collection, here are some ideas:
    1. 8-10 different rocks, including pumice (from a volcano), lodestone (a naturally magnetized piece of magnetite, and often mistaken for meteorites), a fossil, tektite (dry fused glass), pyrite (also known as fool’s gold), marble (calcite or dolomite), and a couple of different kinds of real meteorites (iron meteorite, stony meteorite, etc.) Also add to your bag an unglazed tile and a magnet.
  2. As you watch the experiment video, record your observations on your data sheet.
    1. Since nearly all meteorites have lots of iron, they are usually attracted to a magnet. However, lodestone is an Earth rock that also has a lot of iron. Iron is heavy, and meteorites contain a lot of iron. When looking through the possibilities, remove any lightweight rocks, as they are not usually meteorites.
    2. Meteorites are small. Most never get big enough or hot enough for metal to sink into the core, so the majority are mixed with rock and dust (stony meteorites). The few that do get big and form metal cores are called iron meteorites.
    3. Most meteorites come from the Asteroid Belt. Some meteorites get a dark crust. While others look like splashed metal. They are all dark, at least on the outside. Remove any light-colored rocks.
    4. Rocks that have holes vaporize or explode when they go through the atmosphere, they don’t burn up. Only strong space rocks without holes make it to the ground. Remove any porous rocks.
    5. The ones you have left are either meteorites or lodestone. To tell the difference, scratch a line from both rocks onto an unglazed tile. Magnetite (lodestone) will leave a mark whereas the real meteorite will not.

Finding Meteorites


  1. Place a sheet of white paper outside on the ground. Do this in the morning when you first start up class.
  2. After a few hours (like just before lunchtime), your paper starts to show signs of “dust.”
  3. Carefully place a magnet underneath the paper, and see if any of the particles move as you wiggle the magnet. If so, you’ve got yourself a few bits of space dust.
  4. Use a magnifying lens to look at your space meteorites up close.

What’s Going On?

94% of all meteorites that fall to the Earth are stony meteorites. Stony meteorites will have metal grains mixed with the stone that are clearly visible when you look at a slice.


Iron meteorites make up only 5% of the meteorites that hit the Earth. However, since they are stronger, most of them survive the trip through the atmosphere and are easier to find since they are more resistant to weathering. More than half the meteorites we find are iron meteorites. They are the one of the densest materials on Earth. They stick strongly to magnets and are twice as heavy as most Earth rocks. The Hoba meteorite in Namibia weighs 50 tons.


Since nearly all meteorites have lots of iron, they are usually attracted to a magnet. However, lodestone is an Earth rock that also has a lot of iron. Iron is heavy, and meteorites contain a lot of iron. When looking through the possibilities, remove any lightweight rocks, as they are not usually meteorites.


Meteorites are small. Most never get big enough or hot enough for metal to sink into the core, so the majority are mixed with rock and dust (stony meteorites). The few that do get big and form metal cores are called iron meteorites.


Most meteorites come from the Asteroid Belt. Some meteorites get a dark crust, while others look like splashed metal. They are all dark, at least on the outside.


Rocks that have holes vaporize or explode when they go through the atmosphere, they don’t burn up. Only strong space rocks without holes make it to the ground.


Every year, the Earth passes through the debris left behind by comets. Comets are dirty snowballs that leave a trail of particles as they orbit the Sun. When the Earth passes through one of these trails, the tiny particles enter the Earth’s atmosphere and burn up, leaving spectacular meteor showers for us to watch on a regular basis. The best meteor showers occur when the moon is new and the sky is very dark.


Meteorites are black, heavy (almost twice the normal rock density), and magnetic. However, there is an Earth-made rock that is also black, heavy, and magnetic (magnetite) that is not a meteorite. To tell the difference, scratch a line from both rocks onto an unglazed tile (or the bottom of a coffee mug or the underside of the toilet tank). Magnetite will leave a mark, whereas the real meteorite will not.


If you find a meteorite, head to your nearest geology department at a local university or college and let them know what you’ve found. In the USA, if you find a meteorite, you get to keep it… but you might want to let the experts in the geology department have a thin slice of it to see what they can figure out about your particular specimen.


Exercises


  1.   Are meteors members of the solar system?
  2.  How big are meteors?
  3. Why do we have meteor showers at predictable times of the year?

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Indoor Rain Clouds

Making indoor rain clouds demonstrates the idea of temperature, the measure of how hot or cold something is. Here’s how to do it:


Take two clear glasses that fit snugly together when stacked. (Cylindrical glasses with straight sides work well.)


Fill one glass half-full with ice water and the other half-full with very hot water (definitely an adult job – and take care not to shatter the glass with the hot water!). Be sure to leave enough air space for the clouds to form in the hot glass.


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Place the cold glass directly on top of the hot glass and wait several minutes. If the seal holds between the glasses, a rain cloud will form just below the bottom of the cold glass, and it actually rains inside the glass! (You can use a damp towel around the rim to help make a better seal if needed.)


Materials:


  • glass of ice water
  • glass of hot water (see video)
  • towel
  • adult help


  Download Student Worksheet & Exercises


Bottling Clouds

On a stormy, rainy afternoon, try bottling clouds — using the refrigerator! Here’s what you do: Place an empty, clean 2-liter soda bottle in the fridge overnight. Take it out and get an adult to light a match, letting it burn for a few seconds, then drop it into the bottle. Immediately cap the bottle and watch what happens (you should see smoke first, then clouds forming inside). Squeeze the sides of the bottle. The clouds should disappear. When you release the bottle, the clouds should reappear. Materials:


  • 2L soda bottle
  • rubbing alcohol
  • bicycle pump
  • car tire valve (drill a 1/2 inch hole through a 2L soda bottle cap and pull the valve gently through with pliers)


Advanced Idea: You can substitute rubbing alcohol and a bicycle pump for the matches to make a more solid-looking cloud.  Swirl a bit of rubbing alcohol around inside the bottle, just enough to coat the insides, and then pour it out.  Cap your bottle with a rubber stopper fitted with a needle valve (so the valve is poking out of the bottle), and apply your pump.  Increase the pressure inside the bottle (keep a firm hand on the stopper or you’ll wind up firing it at someone) with a few strokes and pull out the stopper quickly.  You should see a cloud form inside.


What’s going on? Invisible water vapor is all around us, all the time, but they normally don’t stick together. When you squeezed the sides of the bottle, you increased the pressure and squeezed the molecules  together.  Releasing the bottle decreases the pressure, which causes the temperature to drop. When it cools inside, the water molecules stick to the smoke molecules, making a visible cloud inside your bottle.


Did you know that most drops of water actually form around a dust particle?  Up in the sky, clouds come together when water vapor condenses into liquid water drops or ice crystals. The clouds form when warm air rises and the pressure is reduced (as you go up in altitude). The clouds form at the spot where the temperature drops below the dew point.


The alcohol works better than the water because it evaporates faster than water does, which means it moves from liquid to vapor more easily (and vividly) than regular old water.


Questions to ask:


  • How many times can you repeat this?
  • Does it matter what size the bottle is?
  • What if you don’t chill the bottle?
  • What if you freeze the bottle instead?

Exercises


  1. Which combination made it rain the best? Why did this work?
  2. Draw your experimental diagram, labeling the different components:
  3. Add in labels for the different phases of matter. Can you identify all three states of matter in your experiment?

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One common misconception is that the seasons are caused by how close the Earth is to the Sun. Today you get to do an experiment that shows how seasons are affected by axis tilt, not by distance from the Sun. And you also find out which planet doesn’t have sunlight for 42 years.


The seasons are caused by the Earth’s axis tilt of 23.4o from the ecliptic plane.


Materials


  • Bright light source (not fluorescent)
  • Balloon
  • Protractor
  • Masking tape
  • 2 liquid crystal thermometers
  • Ruler, yardstick or meter stick
  • Marker

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Download Student Worksheet & Exercises


  1. For a light source, try lamps with 100W bulbs (without lamp shades). Make sure there’s room to walk all the way around it. You’ll want to circle the lamp at a distance of about 2 feet away.
  2. Mark on the floor with tape and label the four positions: winter, spring, summer, and fall. They should be at the 12, 3, 6, and 9 o’clock positions. Winter is directly across from summer. The Earth rotates counterclockwise around the Sun when viewed from above.
  3. Blow up your balloon so it’s roughly round-shaped (don’t blow it up all the way). Mark and label the north and south poles with your marker. Draw an equator around the middle circumference.
  4. The Earth doesn’t point its north pole straight up as it goes around the Sun. It’s tilted over 23.4o. here’s how you find this point on your balloon:
    1. Put the South Pole mark on the table, with north pointing straight up. Find the midway point between the equator and the North Pole and make a tiny mark. This is the 45o latitude point. You’ll need this to find the 23o mark.
    2. Find the midway point between the 45o and the North Pole and make another mark, larger this time and label it with 23o. When this mark is pointing up, the Earth is tilted over the right amount.
    3. You’ll need to do this three more times so you can draw a line connecting the dots. You want to draw the latitude line at 23o so you can rotate the balloon as you move around to the different seasons. The line will always be pointed up.
  5. Place the thermometers on the balloon at these locations:
    1. Find the halfway point between the South Pole and the equator. Put one thermometer on this mark.
    2. Put the other thermometer on the northern hemisphere’s 45o mark from above.
  6. Make sure your lamp is facing the balloon as you stand on summer. Let the balloon be heated by the lamp for a couple of minutes and then record the temperature in the data table.
  7. Rotate the lamp to point to fall. Move your balloon to fall, rotating the balloon so that the thermometers are facing the lamp. Wait a few more minutes and take another reading.
  8. Rotate the lamp to point to winter. Move your balloon to winter, rotating the balloon so that the thermometers are facing the lamp. Wait a few more minutes and take another reading.
  9. Rotate the lamp to point to spring. Move your balloon to spring, rotating the balloon so that the thermometers are facing the lamp. Wait a few more minutes and take another reading. You’ve completed a data set for planets with an axis tilt of about 23o, which includes the Earth, Mars, Saturn and Neptune.
  10. Repeat steps 1-9 for Mercury. Note that Mercury does not have an axis tilt, so the North Pole really points straight up. Jupiter (3.1o axis tilt) and Venus (2.7o) are very similar. The Moon’s axis tilt is 6.7o, so you can approximate these four objects with a 0o axis tilt.
  11. Repeat steps 1-9 for Uranus. Since the axis tilt is 97.8o, you can approximate this by pointing the north pole straight at the Sun during summer (90o axis tilt). The orbit for Uranus is 84 years, which means 21 years passes between each season. The north pole will experience continued sunlight for 42 years from spring through fall, then darkness for 42 years.

What’s Going On?

The north and south poles only experience two seasons: winter and summer. During a South Pole winter, the Sun will not rise for several months, and also the Sun does not set for several months in the summer. We go into more detail about how this works in a later lesson entitled: Star Trails and Planet Patterns.


At the equator, there’s a wet season and a dry season due to the tropical rain belt. Since the equator is always oriented at the same position to the Sun, it receives the same amount of sunlight and always feels like summer.


The changing of the seasons is caused by the angle of the Sun. For example, in June during summer solstice, the Sun is high in the sky for longer periods of time, which makes warmer temperatures for the Northern Hemisphere. During the December winter solstice, the Sun spends less time in the sky and is positioned much lower. This makes the winters colder. (Don’t forget that seasons are also affected by oceans and winds, though this is out of the scope of this particular activity.)


Exercises


  1. What is the main reason we have seasons on Earth?
  2. Why are there no sunsets on Uranus for decades?
  3. Are there seasons on Venus?

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Many wonders are visible when flying over the Earth at night, especially if you are an astronaut on the International Space Station (ISS)! Passing below are white clouds, orange city lights, lightning flashes in thunderstorms, and dark blue seas. On the horizon is the golden haze of Earth’s thin atmosphere, frequently decorated by dancing auroras as the video progresses. The green parts of auroras typically remain below the space station, but the station flies right through the red and purple auroral peaks. You’ll also see solar panels of the ISS around the frame edges. The wave of approaching brightness at the end of each sequence is just the dawn of the sunlit half of Earth, a dawn that occurs every 90 minutes, as the ISS travels at 5 miles per second to keep from crashing into the earth.


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Video Credit: Gateway to Astronaut Photography, NASA
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It just so happens that the Sun’s diameter is about 400 times larger than the Moon, but the Moon is 400 times closer than the Sun. This makes the Sun and Moon appear to be about the same size in the sky as viewed from Earth. This is also why the eclipse thing is such a big deal for our planet. You’re about to make your own eclipses as you learn about syzygy.


A total eclipse happens about once every year when the Moon blocks the Sun’s light. Lunar eclipses occur when the Sun, Moon, and Earth are lined up in a straight line with the Earth in the. Lunar eclipses last hours, whereas solar eclipses last only minutes.


Materials


  • 2 index cards
  • Flashlight or Sunlight
  • Tack or needle
  • Black paper
  • Scissors

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Download Student Worksheet & Exercises


  1. Trace the circle of your flashlight on the black paper and cut out the circle with paper. This is your Moon. If you are using the Sun instead, cut out a circle about the size of your fist.
  2. Make a tiny hole in one of the index cards by pushing a tack through the middle of the card.
  3. Hold the punched index card a couple inches above the plain one and shine your light through the hole so that a small disk appears on the lower card. Move the cards closer or further until it comes into focus. The disk of light is the Sun.
  4. Ask your lab partner to slowly move the black paper disk in front of your light as you watch what happens to the Sun on the bottom index card.
  5. Continue moving the black paper until you can see the Sun again.
  6. Where does your circle need to be in order to create an annular eclipse? A partial eclipse?
  7. How would you simulate Mercury transiting the Sun? What would you use?
  8. Fill out the table.

What’s Going On?

An eclipse is when one object completely blocks another. If you’re big on vocabulary words, then let the students know that eclipses are one type of syzygy (a straight line of three objects in a gravitational system, like the Earth, Moon, and Sun).


A lunar eclipse is when the Moon moves into the Earth’s shadow, making the Moon appear copper-red.



A solar eclipse is when the Moon’s shadow crawls over the Earth, blocking out the Sun partially or completely. There are three kinds of solar eclipses. A total eclipse blocks the entire Sun, whereas in a partial eclipse the Moon appears to block part, but not all of the Sun’s disk. An annular eclipse is when the Moon is too far from Earth to completely cover the Sun, so there’s a bright ring around the Moon when it moves in front of the Sun.


It just so happens that the Sun’s diameter is about 400 times larger than the Moon, but the Moon is 400 times closer than the Sun. This makes the Sun and Moon appear to be about the same size in the sky as viewed from Earth. This is also why the eclipse thing is such a big deal for our planet.


Transits are where the disk of a planet (like Venus) passes like a small shadow across the Sun. Io transits the surface of Jupiter. In rare cases, one planet will transit another. These are rare because all three objects must align in a straight line.



Astronomers use this method to detect large planets around distant bright stars. If a large planet passes in front of its star, the star will appear to dim slightly.


Note: A transit is not an occultation, which completely hides the smaller object behind a larger one.


Exercises


  1. What other planets can have eclipses?
  2. Which planets transit the Sun?
  3. How is a solar eclipse different from a lunar eclipse?
  4. What phase can a lunar eclipse occur?
  5.  Can a solar eclipse occur at night?

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You know you’re not supposed to look at the sun, so how can you study it safely?  I’m going to show you how to observe the sun safely using a very inexpensive filter.  I actually keep one of these in the glove box of my car so I can keep track of certain interesting sunspots during the week!


The visible surface of the sun is called the photosphere, and is made mostly of plasma (remember the grape experiment?) that bubbles up hot and cold regions of gas. When an area cools down, it becomes darker (called sunspots). Solar flares (massive explosions on the surface), sunspots, and loops are all related the sun’s magnetic field. While scientists are still trying to figure this stuff out, here’s the latest of what they do know…


The sun is a large ball of really hot gas – which means there are lots of naked charged particles zipping around. And the sun also rotates, but the poles and the equator move and different speeds (don’t forget – it’s not a solid ball but more like a cloud of gas). When charged particles move, they make magnetic fields (that’s one of the basic laws of physics). And the different rotation rates allow the magnetic fields to ‘wind up’ and cause massive magnetic loops to eject from the surface, growing stronger and stronger until they wind up flipping the north and south poles of the sun (called ‘solar maximum’). The poles flip every eleven years.


There have been several satellites specially created to observe the sun, including Ulysses (launched 1990, studied solar wind and magnetic fields at the poles), Yohkoh (1991-2001, studied x-rays and gamma radiation from solar flares), SOHO (launched 1995, studies interior and surface), and TRACE (launched 1998, studies the corona and magnetic field).


Ok – so back to observing the sun form your own house. Here’s what you need to do:


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Materials:


  • Baader filter film
  • set of eyeballs


Click here for an inexpensive Baader filter film. You can use these with your naked eye or over the OPEN END (not the eyepeice) of a telescope.  See image below:


Want to see a BIG solar flare?
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You might be curious about how to observe the sun safely without losing your eyeballs. There are many different ways to observe the sun without damaging your eyesight. In fact, the quickest and simplest way to do this is to build a super-easy pinhole camera that projects an image of the sun onto an index card for you to view.


CAUTION: DO NOT LOOK AT THE SUN THROUGH ANYTHING WITH LENSES!!


This simple activity requires only these materials:


  • tack
  • 2 index cards (any size)
  • sunlight

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Here’s what you do:



 
Download Student Worksheet & Exercises


With your tack, make a small hole in the center of one of the cards. Stack one card about 12″ above the over and go out into the sun. Adjust the spacing between the cards so a sharp image of the sun is projected onto the lower paper. The sun will be about the size of a pea.


You can experiment with the size of the hole you use to project your image. What happens if your hole is really big? Too small? What if you bend the lower card while viewing? What if you punch two holes? Or three?


Exercises


  1.  How many longitude degrees per day does the sunspot move?
  2.  Do all sunspots move at the same rate?
  3.  Did some of the sunspots change size or shape, appear or disappear?

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If you want to get from New York to Los Angeles by car, you’d pull out a map. If you want to find the nearest gas station, you’d pull out a smaller map. What if you wanted to find our nearest neighbor outside our solar system? A star chart is a map of the night sky, divided into smaller parts (grids) so you don’t get too overwhelmed. Astronomers use these star charts to locate stars, planets, moons, comets, asteroids, clusters, groups, binary stars, black holes, pulsars, galaxies, planetary nebulae, supernovae, quasars, and more wild things in the intergalactic zoo.


How to find two constellations in the sky tonight, and how to get those constellations down on paper with some degree of accuracy.


Materials


  • Dark, cloud-free night
  • Two friends
  • String
  • Rocks
  • Pencil

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Download Student Worksheet & Exercises


  1. Tape your string to the pencil.
  2. Loosely wrap the string around your finger several times so that the tip of the pencil is about an inch above the ground.
  3. Find a constellation. Point to a star in the constellation.
  4. Have a second person place a rock under the pencil tip.
  5. When they’ve placed the rock in position, point to another star.
  6. Have a second person place a rock under the pencil tip again.
  7. Repeat this process until all the stars have rocks under their positions.
  8. You should see a small version of the constellation on your paper.

What’s Going On?

People have been charting stars since long before paper was invented. In fact, we’ve found star charts on rocks, inside buildings, and even on ivory tusks. Celestial cartography is the science of mapping the stars, galaxies, and astronomical objects on a celestial sphere.


Celestial navigation (astronavigation) made it possible for sailors to cross oceans by sighting the Sun, moon, planets, or one of the 57 pre-selected navigational stars along with the visible horizon.


Watch the video that shows how the stars appear to move differently, depending on which part of the Earth you’re viewing from. What’s the difference between living on the equator or in Antarctica (explained in video)?


The first thing to star chart is the Big Dipper, or other easy-to-find constellation (alternates: Cassiopeia for northern hemisphere or the Southern Cross for the southern hemisphere). The Big Dipper is always visible in the northern hemisphere all year long, so this makes for a good target.


Use glow–in-the-dark stars instead of rocks, and charge them with a quick flash from a camera (or a flashlight). Keep your hand as still as you can while the second person lines the rock into position. You can also unroll a large sheet of (butcher or craft) paper and use markers to create a more permanent star chart.


Exercises:


  1. If you have constellations on your class ceiling, chart them on a separate page marking the positions of the rocks with X’s.
  2. Tonight, find two constellations that you will chart. Bring them with you tomorrow using the technique outlined above in Experiment.

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These are a set of videos made using planetarium software to help you see how the stars and planets move over the course of months and years. See what you think and tell us what you learned by writing your comments in the box below.


What’s odd about these star trails?

You can really feel the Earth rolling around under you as you watch these crazy star trails.
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Download Student Worksheet & Exercises


Do the planets follow the same arc across the night sky? You bet! All eight planets follow along the same arc that the sun follows, called the ecliptic. Here’s how the planets move across the sky:



Exercises:


  1. If you have constellations on your class ceiling, chart them on a separate page marking the positions of the rocks with X’s.
  2. Tonight, find two constellations that you will chart. Bring them with you tomorrow using the technique outlined above in Experiment.

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The Moon appears to change in the sky. One moment it’s a big white circle, and next week it’s shaped like a sideways bike helmet. There’s even a day where it disappears altogether. So what gives?


The Sun illuminates half of the Moon all the time. Imagine shining a flashlight on a beach ball. The half that faces the light is lit up. There’s no light on the far side, right? For the Moon, which half is lit up depends on the rotation of the Moon. And which part of the illuminated side we can see depends on where we are when looking at the Moon. Sound complicated? This lab will straighten everything out so it makes sense.


Materials


  • ball
  • flashlight

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This first video will show you how the moon changes it’s appearance over the course of its cycle:




This video will show you how to demonstrate why the moon changes it’s appearance over the course of its cycle:



 
Download Student Worksheet & Exercises


  1. This lab works best if your room is very dark. Button down those shades and make it as dark as you can.
  2. Assign one person to be the Sun and hand them the flashlight. Stay standing up about four feet away from the group. The Sun doesn’t move at all for this activity.
  3. Assign one person to be the Moon and hand them the ball. Stay standing up, as you’ll be circling the Earth.
  4. The rest of the people are the Earth, and they stand or sit right the middle (so they don’t get a flashlight in their eyes as the Moon orbits).
  5. Start with a new Moon. Shine the flashlight above the heads of the Earth. Move the Moon (ball) into position so that the ball blocks all the light from the flashlight. Ask the Earth kids how much light they can see on their side of the Moon (should be none). Which phase of the Moon is this?
  6. Now the Moon moves around to the opposite side of the Earth so that the Earth kids can see the entire half of the ball lit up by the flashlight. Ask the Earth kids how much light they can see on their side of the Moon (should be half the ball). Which phase of the Moon is this?
  7. Now find the positions for first quarter. Where does the Moon need to stand so that the Earth kids can see the first quarter Moon?
  8. Continue around in a complete circle and fill out the diagram. Color in the circles to indicate the dark half of the Moon. For example, the new Moon should be completely darkened.
  9. Now it’s time to investigate why Venus and Mercury have phases. Put the Sun in the center and assign a student to be Venus. Venus gets the ball.
  10. Venus should be walking slowly around the Sun. The Sun is going to have to rotate to always face Venus, since the Sun normally gives off light in every direction.
  11. The Earth kids need to move further out from the Sun than Venus, so they will be watching Venus orbit the Sun from a distance of a couple of feet.
  12. Earth kids: What do you notice about how the Sun lights up Venus from your point of view? Is there a time when you get to see Venus completely illuminated, and other times when it’s completely dark?
  13. Draw a diagram of what’s going on, labeling Venus’s full phase, new phase, half phases, crescent, and gibbous phases. Label the Sun, Earth, and all eight phases of Venus.

Reading


The Sun illuminates half of the Moon all the time. Imagine shining a flashlight on a beach ball. The half that faces the light is lit up. There’s no light on the far side, right? So for the Moon, which half is lit up depends on the rotation of the Moon. And which part of the illuminated side we can see depends on where we are when looking at the Moon. Sound complicated? This lab will straighten everything out so it makes sense.


One question you’ll hear is: Why don’t we have eclipses every month when there’s a new Moon? The next lesson is all about eclipses, but you can quickly answer their questions by reminding them that the Moon’s orbit around the Earth is not in the same plane as the Earth’s orbit around the Sun (called the ecliptic). It’s actually off by about 5o. In fact, only twice per month does the Moon pass through the ecliptic.


The lunar cycle is approximately 28 days. To be exact, it takes on average 29.53 days (29 days, 12 hours, 44 minutes) between two full moons.  The average calendar month is 1/12 of a year, which is 30.44 days. Since the Moon’s phases repeat every 29.53 days, they don’t quite match up. That’s why on Moon phase calendars, you’ll see a skipped day to account for the mismatch.


A second full Moon in the same month is called a blue Moon. It’s also a blue Moon if it’s the third full Moon out of four in a three-month season, which happens once every two or three years.


The Moon isn’t the only object that has phases. Mercury and Venus undergo phases because they are closer to the Sun than the Earth. If we lived on Mars, then the Earth would also have phases.


Exercises


  1. Does the sun always light up half the Moon?
  2. How many phases does the Moon have?
  3. What is it called when the Moon appears to grow?
  4. What is it called when you see more light than dark on the Moon?
  5. How long does it take for a complete lunar cycle?

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Using the position of the Sun, you can tell what time it us by making one of these sundials. The Sun will cast a shadow onto a surface marked with the hours, and the time-telling gnomon edge will align with the proper time.


In general, sundials are susceptible to different kinds of errors. If the sundial isn’t pointed north, it’s not going to work. If the sundial’s gnomon isn’t perpendicular, it’s going to give errors when you read the time. Latitude and longitude corrections may also need to be made. Some designs need to be aligned with the latitude they reside at (in effect, they need to be tipped toward the Sun at an angle). To correct for longitude, simply shift the sundial to read exactly noon when indicated on your clock. This is especially important for sundials that lie between longitudinal standardized time zones. If daylight savings time is in effect, then the sundial timeline must be shifted to accommodate for this. Most shifts are one hour.


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Download Student Worksheet & Exercises for ALL Sundials


Simple Sundial

  • Index card
  • Scissors
  • Tape


  1. This sundial takes only a couple minutes to make, and reads easily for beginner students.
  2. Cut the template.
  3. Cut your index card into two triangles by cutting from one corner to the opposite diagonal corner. Stack the two triangles and tape together. This is called your gnomon.
  4. Tape the triangle to your 12-hour line, putting tape on both sides of the gnomon as you stick it to the paper.
  5. Put the sundial in a sunny place where it won’t be disturbed (like inside of a sunny window or on a table outdoors).
  6. Point the sundial so that the gnomon is pointing north. This is most easily done if you orient your sundial at exactly noon in your location. Line up the sundial with the Sun so that the shadow the gnomon makes lines up exactly with the 12.
  7. Tape the sundial down so it won’t move or get blown away.
  8. The gnomon must be exactly perpendicular to the hour markers. Use a ruler or a book edge to help you line this up.

Intermediate Sundial

  • 2 yardsticks or metersticks
  • Protractor
  • Chalk
  • Clock


  1. Find a sunny spot that has concrete and grassy area right next to each other. You’re going to poke the yardstick into the grass and draw on the concrete with chalk, so be sure that the concrete goes in an approximately east-west direction.
  2. First thing in the morning, stick one of the yardsticks into the dirt, right at the edge of the concrete.
  3. At the top of the hour (like at 8 a.m. or 9 a.m.), go out to your yardstick to mark a position.
  4. Lay the second yardstick down along the shadow that the upright yardstick makes on the ground. Use chalk to draw the shadow, and use the yardstick to make your line straight.
  5. Label this line with the hour.
  6. Set your timer and run back out at the top of the next hour.
  7. Repeat steps 3-6 until you finish marking your sundial.
  8. When you’ve completed your sundial, fill out the table.

Advanced Sundial

  • Old CD (this can also be the transparent CD at the top of DVD/CD spindles)
  • Empty CD Case
  • Skewer
  • Sticky tape
  • Cardboard or small piece of clay
  • Protractor
  • Scissors
  • Tape
  • Hot glue


This sundial will work for all longitudes, but has a limited range of latitudes. If you live in the far north or far south, you’ll need to get creative about how to mount the CD so that the gnomon is pointed at the correct angle. For example, at the equator, the CD will lie flat (which is easy!), but near the north and south poles, the CD will be upside down.


  1. Cut out the timeline.
  2. Put a line of double-sided sticky tape along the back of the timeline. Extend the tape about ¼” (on the bottom edge) so it’s hanging off a paper a little.
  3. Flip the timeline over and roll the CD along this bottom edge, sticking the timeline to the edge of the CD. The timeline should be facing inward toward the center of the CD, perpendicular to the CD surface.
  4. Now it’s time to plug up the center hole. You can cut out circles from a CD and attach with tape, or use a small piece of clay.
  5. Push the skewer through the exact middle of the CD.
  6. Open up the CD case.
  7. Position the noon marker at the bottom and stick it using a piece of double-sided sticky tape or hot glue.
  8. The other side of the CD is glued to the CD case at the same angle as your latitude. For example, if I live at 43o north, I would use my protractor on the ground along the base of the CD case and lift the CD until the gnomon reads at 43o. Put a dab of hot glue to attach the CD to the lid of the case.
  9. Go outside and point the gnomon north (you may want to use a compass for this if it’s not noon.)
  10. The dial will have a shadow that falls on the timeline. You can read the time right off the timeline.
  11. For advanced students: Timeline correction: Do you remember how the Sun was fast or slow in the Stargazer’s Wall Chart from the lesson entitled: What’s in the Sky? That wavy line is called the Equation of Time, and you’ll need it to correct your sundial if you want to be completely accurate. This is a great demonstration for a Science Fair project, especially when you add a model of the Sun and Earth to help you explain what’s going on.

What’s Going On?

Sundials have been used for centuries to keep track of the Sun. There are different types of sundials. Some use a line of light to indicate what time it is, while others use a shadow.


Here are a couple of different models that, although they look a lot different from each other, actually all work to give the same results! Your sundial will work all days of the year when the Sun is out.


You’ll notice that north is the direction that your shadow’s length is the shortest. However, if you don’t know where east and west are, all you can do is know where north is. The equinox is a special time of year because the Sun rises in the exact east and sets in the exact west, making these two points exactly perpendicular with the north for your location (which they usually aren’t). At sunset, you can view your shadow (quickly before it disappears) and draw it with chalk on the ground, making a line that runs east-west. 90o CCW from the line is north.


In general, sundials are susceptible to different kinds of errors. If the sundial isn’t pointed north, it’s not going to work.  If the sundial’s gnomon isn’t perpendicular, it’s going to give errors when you read the time. Latitude and longitude corrections may also need to be made. Some designs need to be aligned with the latitude they reside at (in effect, they need to be tipped toward the Sun at an angle). To correct for longitude, simply shift the sundial to read exactly noon when indicated on your clock. This is especially important for sundials that lie between longitudinal standardized time zones. The Equation of Time from the advanced lesson entitled: What’s in the Sky? can be used to correct for the Sun running slow or fast. Remember, this effect is due to both the Earth’s orbit not being a perfect circle and the fact that the tilt axis is not perpendicular to the orbit path.  If daylight savings time is in effect, then the sundial timeline must be shifted to accommodate for this. Most shifts are one hour.


Exercises


  1. What kinds of corrections need to be made for your sundial?
  2. When wouldn’t your sundial work?
  3. How can you improve your sundial to be more accurate?

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This is a recording of a recent live teleclass I did with thousands of kids from all over the world. I’ve included it here so you can participate and learn, too


Our solar system includes rocky terrestrial planets (Mercury, Venus, Earth, and Mars), gas giants (Jupiter and Saturn), ice giants (Uranus and Neptune), and assorted chunks of ice and dust that make up various comets and asteroids.


Did you know you can take an intergalactic star tour without leaving your seat? To get you started on your astronomy adventure, I have a front-row seat for you in a planetarium-style star show. I usually give this presentation at sunset during my live workshops, so I inserted slides along with my talk so you could see the pictures better. This video below is long, so I highly recommend doing this with friends and a big bowl of popcorn. Ready?
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Materials:


  • Two balls, one larger than the other (like a soccer and a tennis ball, or bouncy ball and tennis ball)
  • Print out this worksheet to fill in as we go along!


Download the Black Hole Explorer Game. This was created by a team of scientists, you can use this set of instructions to build your own black hole board game. It plays two different ways: competitively and cooperatively. Black Hole Explorer was created for NASA by the Harvard-Smithsonian Center for Astrophysics.


This is a PDF download, so you’ll need Adobe Acrobat Reader to view the file. It’s fun, easy, and totally free for your family and students to enjoy!


Key Concepts

The solar system is the place that is affected by the gravity our sun. Our solar system includes rocky terrestrial planets (Mercury, Venus, Earth, and Mars), gas giants (Jupiter and Saturn), ice giants (Uranus and Neptune), and assorted chunks of ice and dust that make up various comets and asteroids. The eight planets follow a near-circular orbit around the sun, and many have moons.


Two planets (Ceres and Pluto) have been reclassified after astronomers found out more information about their neighbors. Ceres is now an asteroid in the Asteroid Belt between Mars and Jupiter. Beyond Neptune, the Kuiper Belt holds the chunks of ice and dust, like comets and asteroids as well as larger objects like dwarf planets Eris and Pluto.


Beyond the Kuiper belt is an area called the Oort Cloud, which holds an estimated 1 trillion comets. The Oort Cloud is so far away that it’s only loosely held in orbit by our sun, and constantly being pulled gravitationally by passing stars and the Milky Way itself. The Voyager Spacecraft are beyond the heliosphere (the region influenced gravitationally by our sun) but has not reached the Oort Cloud.


Our solar system belongs to the Milky Way galaxy. Galaxies are stars that are pulled and held together by gravity. Globular clusters are massive groups of stars held together by gravity, using housing between tens of thousands to millions of stars. Some galaxies are sparse while others are packed so dense you can’t see through them. Galaxies also like to hang out with other galaxies (called galaxy clusters ), but not all galaxies belong to clusters, and not all stars belong to a galaxy.


After a star uses up all its fuel, it can either fizzle or explode. Planetary nebulae are shells of gas and dust feathering away. Neutron stars are formed from stars that go supernova, but aren’t big and fat enough to turn into a black hole. Pulsars are spinning neutron stars with their poles aimed our way. Neutron stars with HUGE magnetic fields are known as magnetars. Black holes are the leftovers of a BIG star explosion. There is nothing to keep it from collapsing, so it continues to collapse forever. It becomes so small and dense that the gravitational pull is so great that light itself can’t escape.


The sun holds 99% of the mass of our solar system. The sun’s equator takes about 25 days to rotate around once, but the poles take 34 days. You may have heard that the sun is a huge ball of burning gas. But the sun is not on fire, like a candle. You can’t blow it out or reignite it. So, where does the energy come from?


The nuclear reactions deep in the core transforms 600 million tons per second of hydrogen into helium. This gives off huge amounts of energy which gradually works its way from the 15 million-degree Celsius temperature core to the 15,000 degree Celsius surface.


Active galaxies have very unusual behavior. There are several different types of active galaxies, including radio galaxies (edge-on view of galaxies emitting jets), quasars (3/4 view of the galaxy emitting jets), blazars (aligned so we’re looking straight down into the black hole jet), and others. Our own galaxy, the Milky Way, has a super-massive black hole at its center, which is currently quiet and dormant.


Dying stars blow off shells of heated gas that glow in beautiful patterns. William Hershel (1795) coined the term ‘planetary nebula’ because the ones he looked at through 18th century telescopes looked like planets. They actually have nothing to do with planets – they are shells of dust feathering away.


When a star uses up its fuel, the way it dies depends on how massive it was to begin with. Smaller stars simply fizzle out into white dwarfs, while larger stars can go supernova. A recent supernova explosion was SN 1987. The light from Supernova 1987A reached the Earth on February 23, 1987 and was close enough to see with a naked eye from the Southern Hemisphere.


Questions to Ask

  1. What’s your favorite part about Jupiter?
  2. Which planet is NOW your favorite (after listening to the slide show presentation)?
  3. What happened to the stars in the last slide of the show?
  4. How many moons around Jupiter or Saturn can you see with binoculars?
  5. What’s the difference between a galaxy and a black hole?
  6. How many Earths fit inside the sun?

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When I was in grad school, I needed to use an optical bench to see invisible things. I was trying to ‘see’ the exhaust from a  new kind of F15 engine, because the aircraft acting the way it shouldn’t – when the pilot turned the controls 20o left, the plane only went 10o. My team had traced the problem to an issue with the shock waves, and it was my job to figure out what the trouble was. (Anytime shock waves appear, there’s an energy loss.)


Since shock waves are invisible to the human eye, I had to find a way to make them visible so we could get a better look at what was going on. It was like trying to see the smoke generated by a candle – you know it’s there, but you just can’t see it. I wound up using a special type of photography called Schlieren.


An optical table gives you a solid surface to work on and nails down your parts so they don’t move. This is an image taken with Schlieren photography. This technique picks up the changes in air density (which is a measure of pressure and volume).


The air above a candle heats up and expands (increases volume), floating upwards as you see here. The Schlieren technique shines a super-bright xenon arc lamp beam of light through the candle area, bounces it off two parabolic mirrors and passes it through a razor-edge slit and a neutral density filter before reaching the camera lens. With so many parts, I needed space to bolt things down EXACTLY where I wanted them. The razor slit, for example, just couldn’t be anywhere along the beam – it had to be right at the exact point where the beam was focused down to a point.


I’m going to show you how to make a quick and easy optical lab bench to work with your lenses. Scientists use optical benches when they design microscopes, telescopes, and other optical equipment. You’ll need a bright light source like a flashlight or a sunny window, although this bench is so light and portable that you can move it to garage and use a car headlight if you really want to get creative. Once your bench is set up, you can easily switch out filters, lenses, and slits to find the best combination for your optical designs. Technically, our setup is called an optical rail, and the neat thing about it is that it comes with a handy measuring device so you can see where the focal points are for your lenses. Let’s get started:
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Materials:


  • lenses (glass or plastic), magnifying lenses work also
  • two razor blades (new)
  • index cards (about four)
  • razor
  • old piece of wood
  • single hair from your head
  • tape
  • aluminum foil
  • clothespins (2-4)
  • laser pointer
  • popsicle sticks (tongue-depressor size)
  • hot glue gun
  • scissors and a sharp razor
  • meter sticks (2)
  • bright light source (ideas for this are on the video)

Your lenses are curved pieces of glass or plastic designed to bend (refract) light. A simple lens is just one piece, and a compound lens is like the lens of a camera – there’s lots of them in there. The first lenses were developed by nature – dewdrops on plant leaves are natural lenses. The light changes speed and bends when it hits the surface of the drop, and things under the drop appear larger. (Read more about refraction here.) The earliest written records of lenses are found in the Greek archives and described as being glass globes filled with water.


Concave Lenses

Concave lenses are shaped like a ‘cave’ and curve inward like a spoon. Light that shines through a concave lens bends to a point (converging beam). Ever notice how when you peep through the hole in a door (especially in a hotel), you can see the entire person standing on the doorstep? There’s a concave lens in there making the person appear smaller.


You’ll also find these types of lenses in ‘shoplifting mirrors’. Store owners post these mirrors around help them see a larger area than a flat mirror shows, although the images tend to be a lot smaller.


If you have a pair of near-sighted glasses, chances are that the lenses are concave. Near-sighted folks need help seeing things that are far away, and the concave lenses increase the focal point to the right spot on their retina.


Concave lenses work to make things look smaller, so there not as widely used as convex lenses. You’ll find concave lenses inside camera lenses and binoculars to help clear weird optical problems that happen around the edges of a convex lens (called aberration).


Here’s a video on lenses, both convex and concave:



Convex lenses bulge outwards, bending the light out in a spray (diverging beam). A hand-held magnifying glass is a single concave lens with a handle. These lenses have been used as ‘burning glasses’ for hundreds of years – by placing a small piece of paper at its focal point and using the sun as a light source, you can focus the light energy so intensely that you reach the flash point of the paper (the paper auto-ignites around 450oF).


When you stack a large convex lens above a solar panel, the magnification effect makes it so you can get away with using a smaller photovoltaic cell to get the same amount of energy from the sun. You’ll find convex lenses in telescopes, microscopes, binoculars, eyeglasses, and more.


Mirrors

lenses-part1What if you coat one side of the lens with a reflecting silver coating? You get a mirror!


Stick wooden skewers into a piece of foam to simulate how the light rays reflect off the surface of the mirror. Note that when the mirror (foam) is straight, the light rays are straight (which is what you see when you look in the bathroom mirror). The light bounces off the straight mirror and zips right back at you, remaining parallel.


lenses-part2 copyNow arch the foam. Notice how the light ways (skewers) come to a point (focal point).


After the focal point, the rays invert, so the top skewer is now at the bottom and the bottom is now at the top.  This is your flipped (inverted) image. This is what you’d see when you look into a concave mirror, like the inside of a metal spoon. You can see your face, but it’s upside-down.


Slits

A slit allows light from only one source to enter. If you have light from other sources, your light beam is more scattered and your images and lines become blurry. Thin slits can be easily made by placing the edges of two razor blades very close together and securing into place. We’re going to use an anti-slit using a piece of hair, but you can substitute a thin needle.


Here’s a video on using filters and slits with your laser:



Filters

There are hundreds of different types of filters, used in photography, astronomy, and sunglasses. A filter can change the amount and type of light allowed through it. For example, if you put on red-tinted glasses, suddenly everything takes on a reddish hue. The red filter blocks the rest of the incoming wavelengths (colors) and only allows the red colors to get to your eyeball. There are color filters for every wavelength, even IR and UV.


UV filters reduce the haziness in our atmosphere, and are used on most high-end camera lenses, while IR filters are heat-absorbing filters used with hot light sources (like near incandescent bulbs or in overhead projectors).


A neutral density (ND) filter is a grayish-colored filter that reduces the intensity of all colors equally. Photographers use these filters to get motion blur effects with slow shutter speeds, like a softened waterfall.


Build an Optical Bench

It’s time to put all these pieces together and make cool optical stuff – are you ready?



Download Student Worksheet & Exercises


Click here for more experiments on building your own microscope and telescope.


Cat’s Eyes

Corner reflectors are U-turns for light beams. A corner mirror made from three mirrors will reflect the beam straight back where it came from, no matter what angle you hit it at.  Astronauts placed these types of mirrors on the moon so scientists could easily bounce laser beams off the moon and have them return to the same place on Earth. They used these reflected laser beams to measure the speed of light.


You’ll find corner mirrors in “cat’s eye” reflectors on the road. Car headlights illuminate the reflectors and send the beam straight back the same way – right at the driver.


Exercises


  1. Using only the shape, how can you tell the difference between a convex and a concave lens?
  2.  Which type of lens makes objects viewed through it appear smaller?
  3.  Which type of lens makes the objects viewed through it appear larger?
  4.  How do you get the f number?

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Hans Lippershey was the first to peek through his invention of the refractor telescope in 1608, followed closely by Galileo (although Galileo used his telescope for astronomy and Lippershey’s was used for military purposes).  Their telescopes used both convex and concave lenses.


A few years later, Kepler swung into the field and added his own ideas: he used two convex lenses (just like the ones in a hand-held magnifier), and his design the one we still use today. We’re going to make a simple microscope and telescope using two lenses, the same way Kepler did.  Only our lenses today are much better quality than the ones he had back then!


You can tell a convex from a concave lens by running your fingers gently over the surface – do you feel a “bump” in the middle of your hand magnifying lens?  You can also gently lay the edge of a business card (which is very straight and softer than a ruler) on the lens to see how it doesn’t lay flat against the lens.


Your magnifier has a convex lens – meaning the glass (or plastic) is thicker in the center than around the edges.  The image here shows how a convex lens can turn light to a new direction using refraction. You can read more about refraction here.


A microscope is very similar to the refractor telescope with one simple difference – where you place the focus point.  Instead of bombarding you with words, let’s make a microscope right now so you can see for yourself how it all works together. Are you ready?


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How to Make a Microscope

Materials:


  • 2 hand held magnifiers
  • dollar bill
  • penny


Here’s what you do: Hold one magnifying glass in each hand.  Focus one lens on a printed letter or small object.  Add the second lens above the first, so you can see through both.  Move the lens toward and away from you until you bring the letter into clear focus again.   You just made a microscope!  The lens closest to your eye is the EYEpiece.  The lens closest to the object is the OBJECTive. The image here is of the objective part of a compound microscope.  The different silver tubes have different sizes of lenses, each with a different magnification, so the same scope can go from 40X to 1,000X with the flip of a lens.


How do I determine magnification power for my microscope? Simply multiply the powers of your optics together to get the power of magnification. If you’re using one lens at 10X and the other at 4X, then the combined effect is 40X. You’ll usually find the power rating stamped in tiny writing along the magnifier.


So now you’ve made a microscope.  How about a telescope? Is it really a lot different?


The answer is no.  Simply hold your two lenses as you would for a microscope, but focus on a far-away object like a tree.  You just made a simple telescope… but the image is upside-down!


microscope1We don’t fully understand why, but every time we teach this class, kids inevitably start catching things on fire.  We think it’s because they want to see if they really can do it – and sure enough, they find out that they can!  Just do it in a safe spot (like a leaf on concrete) if that’s something you want to do. Click here for a detailed instructional video on how to do this safely.


How do I connect the flaming shrubbery back to the main optics lesson? Ask your child why the leaf catches on fire… and when the shrug, you can lead them around to a discussion about focus points of a lens.  It’s hard for kids to visualize the light lines through a lens, so you can shine a strong light through a fine-tooth comb as shown in the image above.  Use clear gelatin (or Jell-O) shapes as your “lenses” and shine your rays of light through it.  If your room is dark enough, you’ll get the image shown above.


The point where all the lines intersect is where things catch fire, as the energy is most concentrated at this point. Note how the lines flip after the focus point – this is why the telescope images are inverted.  The microscope image is not flipped because you’ve placed the image (and/or your eye) before the focus point.  Play around with it and find out where the focus point is.  Slide your lenses along a yardstick to easily measure distances.


How to Make a Telescope

Materials:


  • 2 hand held magnifiers
  • window


 
Want to experiment further? Then click for the Optical Bench experiment and also sneak a peek at the Advanced Telescope Building experiment where you will learn about lenses, refractor, and newtonian telescopes.


Ready to buy your own professional-quality instrument that will last you all the way through college? Click here for our recommendations on microscopes, telescopes, and binoculars.
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If you’ve never done this experiment, you have to give it a try! This activity will show you the REAL reason that you should never look at the sun through anything that has lenses in it.


Because this activity involves fire, make sure you do this on a flame-proof surface and not your dining room table! Good choices are your driveway, cement parking lot, the concrete sidewalk, or a large piece of ceramic tile.  Don’t do this experiment in your hand, or you’re in for a hot, nasty surprise.


As with all experiments involving fire, flames, and so forth, do this with adult help (you’ll probably find they want to do this with you!) and keep your fire extinguisher handy.


Materials:


  • sunlight
  • dead leaf
  • magnifying glass
  • fire extinguisher
  • adult help

Here’s what you need to do:


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Magnifying lenses, telescopes, and microscopes use this idea to make objects appear different sizes by bending the light. When light passes through a different medium (from air to glass, water, a lens…) it changes speed and usually the angle it’s traveling at.  A prism splits incoming light into a rainbow because the light bends as it moves through the prism. A pair of eyeglasses will bend the light to magnify the image.


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We’re going to bend light to make objects disappear. You’ll need two glass containers (one that fits inside the other), and the smaller one MUST be Pyrex. It’s okay if your Pyrex glass has markings on the side. Use cooking oil such as canola oil, olive oil, or others to see which makes yours truly disappear. You can also try mineral oil or Karo syrup, although these tend to be more sensitive to temperature and aren’t as evenly matched with the Pyrex as the first choices mentioned above.


Here’s what you need:


  • two glass containers, one of which MUST be Pyrex glass
  • vegetable oil (cheap canola brand is what we used in the video)
  • sink

Published value for light speed is 299,792,458 m/s = 186,282 miles/second = 670,616,629 mph
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When a beam of light hits a different substance (like glass), the speed of light changes. The color of the light (called the wavelength) can also change. In some cases, the change of wavelength turns into a change in the direction of the beam.


For example, if you stick a pencil is a glass of water and look through the side of the glass, you’ll notice that the pencil appears shifted. The speed of light is slower in the water (140,000 miles per second) than in the air (186,000 miles per second), called optical density, and the result is bent light beams and broken pencils.


You’ll notice that the pencil doesn’t always appear broken. Depending on where your eyeballs are, you can see an intact or broken pencil.


This is a very fine point about refraction: when light enters a new substance (like going from air to water) perpendicular to the surface (looking straight on), refractions do not occur.


However, if you look at the glass at an angle, then depending on your sight angle, you’ll see a different amount of shift in the pencil. Where do you need to look to see the greatest shift in the two halves of the pencil? (Hint: move the pencil back and forth slowly.)


Depending on if the light is going from a lighter to an optically denser material (or vice versa), it will bend different amounts. Glass is optically denser than water, which is denser than air.


Here’s a chart:


Vacuum 1.0000
Air 1.0003
Ice 1.3100
Water 1.3333
Pyrex 1.4740
Cooking Oil 1.4740
Diamond 2.4170


This means if you place a Pyrex container inside a beaker of vegetable oil, it will disappear. This also works for some mineral oils and Karo syrup. Note however that the optical densities of liquids vary with temperature and concentration, and manufacturers are not perfectly consistent when they whip up a batch of this stuff, so some adjustments are needed.


Not only can you change the shape of objects by bending light (broken or whole), but you can also change the size. Magnifying lenses, telescopes, and microscopes use this idea to make objects appear different sizes.


Questions to Ask


  • Does the temperature of the oil matter?
  • What other kinds of oil work? Blends of oils?
  • Does it work with mineral oil or Karo syrup?
  • Is there a viewing angle that makes the inside container visible?
  • Which type of lighting makes the container more invisible?
  • Can we see light waves?

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Here’s a trick question – can you make the color “yellow” with only red, green, and blue as your color palette?  If you’re a scientist, it’s not a problem.  But if you’re an artist, you’re in trouble already.


The key is that we would be mixing light, not paint.  Mixing the three primary colors of light gives white light.  If you took three light bulbs (red, green, and blue) and shined them on the ceiling, you’d see white.  And if you could magically un-mix the white colors, you’d get the rainbow (which is exactly what prisms do.)


If you’re thinking yellow should be a primary color – it is a primary color, but only in the artist’s world.  Yellow paint is a primary color for painters, but yellow light is actually made from red and green light.  (Easy way to remember this: think of Christmas colors – red and green merge to make the yellow star on top of the tree.)


As a painter, you know that when you mix three cups of red, green, and blue paint, you get a muddy brown. But as a scientist, when you mix together three cups of cold light, you get white.  If you pass a beam white light through a glass filled with water that’s been dyed red, you’ve now got red light coming out the other side.  The glass of red water is your filter.  But what happens when you try to mix the different colors together?


The cold light is giving off its own light through a chemical reaction called chemiluminescence, whereas the cups of paint are only reflecting nearby light. It’s like the difference between the sun (which gives off its own light) and the moon (which you see only when sunlight bounces off it to your eyeballs). You can read more about light in our Unit 9: Lesson 1 section.


Here’s what you need:


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Download Student Worksheet & Exercises


You can demonstrate the primary colors of light using glow sticks! When red, green, and blue cold light are mixed, you get white light.


Simply activate the light stick (bend it until you hear a *crack* – that’s the little glass capsule inside breaking) and while wearing gloves, carefully slice off one end of the tube with strong cutters, being careful not to splash (do this over a sink).


Cut off the ends for all three light sticks. Pass the contents of the light sticks through a coffee filter (or paper towel) into a disposable cup – this will capture the glass bits. Now your cup should be glowing white.


Sometimes the chemical light sticks contain a glowing green liquid encapsulated within a red or blue plastic tube, so when you slice it open to combine it with the other colors, it isn’t a true red. Be sure that your chemical light sticks contain a glowing RED LIQUID and BLUE LIQUID in a clear, colorless plastic tube, or this experiment won’t work. Order true color glow sticks here.


Exercises


  1.     What color do you get when you mix blue and green liquid lights?
  2.     What happens when you start to add the red light?
  3.     What is your final color result when mixing red, blue, and green lights?
  4.      How would your result differ if you instead mixed red, blue and green paints?

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There are three primary colors of light are red, green, and blue.  The three primary colors of paint are red, yellow, and blue (I know it’s actually cyan, yellow, and magenta, which we’ll get to in more detail later, but for now just stick with me and think of the primary colors of paint as red-yellow-blue and I promise it will all make sense in the end).


Most kids understand how yellow paint and blue paint make green paint, but are totally stumped when red light and green light mix to make yellow light. The difference is that we’re mixing light, not paint.


Lots of science textbooks still have this experiment listed under how to mix light: “Stir together one of red water and one glass of green water (dyed with food coloring) to get a glass of yellow water.” Hmmm… the result I get is a yucky greenish-brown color. What happened?


The reason  you can’t mix green and red water to get yellow is that you’re essentially still mixing paint, not light. But don’t take our word for it – test it out for yourself with this super-fast light experiment on mixing colors.


Materials:


  • pair of scissors
  • crayons
  • sharp wood pencil or wood skewer
  • index cards
  • drill (optional)

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Download Student Worksheet & Exercises


Here’s what you do: use a cup to outline circles on a sheet of stiff white paper (or manila folders). Stack several blank pages together and cut out multiple circles. Color the circles, push a sharp wooden pencil through a hole in the center, and spin! What color does yellow and blue make? Pink and purple? You can also make a button-spinner to really whirl it around by looping a length of string through two holes in the center of the disk circle.


Troubleshooting: These disks needs to spin rapidly in order to trick your eye into blending the colors. If you have a motor, batteries, and wires lying around, you can use them to spin the disks for you. Simply punch the motor’s shaft through the paper (colored-side up).


Turn the motor on by connecting the power and watch the colors mix! Other alternatives include using a drill, hand-held mixer/beaters (not a Kitchen Aid standard mixer!), electric screwdriver, etc.


Alternate Spinning Method: Want to do this project, but you don’t have enough speed or a motor?  You can make a ‘button spinner’ to whirl these things around super-fast.  (Did you know this is how the first circular saws were made?)


Attach your disk to a piece of stiff cardboard (index cards are too flimsy), punch out two holes near the center and thread a loop of string through and tie the ends together to make the old-fashioned “spinning disk”. Using a circling motion with your hands, you can twist up the string with the card in the middle and then pull horizontally outwards to untwist it and watch the cardboard whirl and whip around!!


Click here for the Mixing Cold Light experiment!


Exercises


  1.  What happens when blue and red are mixed on the spinner?
  2.  What happens when red and green are mixed on the spinner?
  3. What colors would you mix to get orange?
  4. What are the primary colors of light, and how do they differ from the primary colors we learn in art class?

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Ever play with a prism? When sunlight strikes the prism, it gets split into a rainbow of colors. Prisms un-mix the light into its different wavelengths (which you see as different colors). Diffraction gratings are tiny prisms stacked together.


When light passes through a diffraction grating, it splits (diffracts) the light into several beams traveling at different directions. If you’ve ever seen the ‘iridescence’ of a soap bubble, an insect shell, or on a pearl, you’ve seen nature’s diffraction gratings.


Scientist use these things to split incoming light so they can figure out what fuels a distant star is burning. When hydrogen burns, it gives off light, but not in all the colors of the rainbow, only very specific colors in red and blue. It’s like hydrogen’s own personal fingerprint, or light signature.


Astronomers can split incoming light from a star using a spectrometer (you can build your own here) to figure out what the star is burning by matching up the different light signatures.


Materials:


  • feather
  • old CD or DVD

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Here’s what you do: Take a feather and put it over an eye. Stare at a light bulb or a lit candle. You should see two or three flames and a rainbow X. Shine a flashlight on a CD and watch for rainbows. (Hint – the tiny “hairs” on the feather are acting like tiny prisms… take your homemade microscope to look at more of the feather in greater detail and see the tiny prisms for yourself!


What happens when you aim a laser through a diffraction grating? Here’s what you do:


Materials:



Download Student Worksheet & Excercises


Exercises


  1. Which light source gave the most interesting results?
  2. What happens when you aim a laser beam through the diffraction grating?
  3. How is a CD different and the same as a diffraction grating?
  4. Why does the feather work?

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This is the simplest form of camera – no film, no batteries, and no moving parts that can break. The biggest problem with this camera is that the inlet hole is so tiny that it lets in such a small amount of light and makes a faint image. If you make the hole larger, you get a brighter image, but it’s much less focused. The more light rays coming through, the more they spread out the image out more and create a fuzzier picture. You’ll need to play with the size of the hole to get the best image.


While you can go crazy and take actual photos with this camera by sticking on a piece of undeveloped black and white film (use a moderately fast ASA rating), I recommend using tracing paper and a set of eyeballs to view your images. Here’s what you need to do:


Materials:


  • box
  • tracing paper
  • razor or scissors
  • tape
  • tack

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Download Student Worksheet & Exercises


Here’s the quick set of instructions:


1. Use a cardboard box that is light-proof (no leaks of light anywhere).
2. Seal light leaks with tape if you have to. Cut off one side of the box (Note – there’s no need to do this if you’re using a shoebox).
3. Tape a piece of tracing paper over the cutout side, keeping it taut and smooth.
4. Make a pinhole in the box side opposite of the tracing paper.
5. Point the pinhole at a window and move toward or away from the window until you see its image in clear focus on the tracing paper.


OPTIONAL: You can hold up a magnifying glass in front of the pinhole to sharpen the image.


Exercises


  1.  How do the images appear when they’re projected onto the paper inside your camera?
  2. Why do you think it’s important to make the box as light-proof as possible?
  3. Is there a part of your body that works similarly to the pinhole?
  4.  Sketch a picture of something you saw through your pinhole camera.

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In this lab, we are going to make an eyeball model using a balloon. This experiment should give you a better idea of how your eyes work. The way your brain actually sees things is still a mystery, but using the balloon we can get a good working model of how light gets to your brain.


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Here’s what you need


    • 1 biconvex plastic lens
    • 1 round balloon, white, 9 inches
    • 1 assistant
    • 1 votive candle
    • 1 black marker
    • 1 book of matches
    • 1 metric ruler
    • Adult Supervision!


Download Student Worksheet & Exercises


Here’s what you do


  1. Blow up the balloon until it is about the size of a grapefruit. If it’s difficult to inflate, stretch the material a few times or ask an adult to help you.
  2. You will need an extra set of hands for this portion. Ask your partner to hold the neck of the balloon closed to keep the air in while you insert the lens into the opening. The lens will need to be inserted perpendicularly to the balloon’s neck. It will prevent any air from escaping once it’s in place. Like your eye, light will enter through the lens and travel toward the back of the balloon.
  3. Hold the balloon so that the lens is pointing toward you. Take the lens between your thumb and index finger. Look into the lens into the balloon. You should have a clear view of the inside. Start to twist the balloon a little and notice that the neck gets smaller like your pupils do when exposed to light. Practice opening and closing the balloon’s “pupil.”
  4. Have an adult help you put the candle on the table and light it. Turn out the lights.
  5. Put the balloon about 20 to 30 centimeters away from the candle with the lens pointed toward it. The balloon should be between you and the candle. You should see a projection of the candle’s flame on the back of the balloon’s surface. Move the balloon back and forth in order to better focus the image on the back of the balloon and then proceed with data collection.
  6.  Describe the image you see on the back of the balloon. How is it different from the flame you see with your eyes? Draw a picture of how the flame looks.
  7. The focal length is the distance from the flame to the image on the balloon. Measure this distance and record it.
  8. What happens if you lightly push down on the top of the balloon? Does this affect the image? You are experimenting with the affect caused by near-sightedness.
  9. To approximate a farsighted eye, gently push in the front and back of the balloon to make it taller. How does this change what you see?

What’s going on?


Okay, let’s discuss the part of the balloon that relate to parts of your eye. The white portion of the balloon represents your sclera, which you may have already guessed is also the white part of your eye. It is actually a coating made of protein that covers the various muscle in your eye and holds everything together.


Of course, the lens you inserted represents the actual lens in your eye. The muscles surrounding the lens are called ciliary muscles and they are represented by the rubber neck of your balloon. The ciliary muscles help to control the amount of light entering your eyes.


The retina is in the back of your eye, which is represented by the inside back of your balloon. The retina supports your rods and cones. They collect information about light and color and send it to your brain.


Exercises


  1.      How does your eye work like a camera?
  2.      How can you tell if a lens is double convex?
  3.      What is the difference between convex and concave?
  4.      Can you give an example of an everyday object that has both a convex and a concave side?
  5.      How can you change the balloon to make it like a near-sighted eye?
  6.      How can you change the balloon to make it like a far-sighted eye?

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benham1Charles Benhamho (1895) created a toy top painted with the pattern (images on next page). When you spin the disk, arcs of color (called “pattern induced flicker colors”) show up around the disk. And different people see different colors!


We can’t really say why this happens, but there are a few interesting theories. Your eyeball has two different ways of seeing light: cones and rods. Cones are used for color vision and for seeing bright light, and there are three types of cones (red, green, and blue). Rods are important for seeing in low light.


One possibility is… [am4show have=’p8;p9;p11;p38;p92;p19;p46;p66;’ guest_error=’Guest error message’ user_error=’User error message’ ]


…how the human eye is tuned for different colors. Your eyeballs respond at different rates to red, green, and blue colors. The spinning disk triggers different parts of the retina. This alternating response may cause some type of interaction within the nervous system that generates colors.


Another theory is that certain cones take longer react, and thus stay active, for longer amounts of time (though we’re still talking milliseconds, here). To put another way, the white color activates all three cones, but then the black deactivates them in a certain sequence, causing your brain to get mixed and unbalanced signals. Your brain does the best it can to figure it out the information it’s getting, and “creates” the colors you see in order to make sense of it all.


Neither of these theories explains the colors of Benham’s disk completely and the reason behind the illusion remains unsolved. Can you help out these baffled scientists?


Materials:




 
Download Student Worksheets & Exercises


All you need to do is download this PDF file and cutout a copy of a disc on the page. Then find a way to spin it at high speeds – you can stick a pencil through the center and spin it like a top, thread string through it and pull to rotate (just like the Mixing Colors Experiment), attach to a drill or mixer or electric screwdriver, or slap it on a motor shaft and engage the power. Which works best?


Exercises


  1. What colors were you able to see when the disks were spinning?
  2. How did the different patterns look when they were spun?
  3.  How did speed and direction affect what you saw?

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Ever notice how BRIGHT your white t-shirt looks in direct sun? That’s because mom washed with fluorescent laundry soap (no kidding!). The soap manufacturers put in dyes that glow white under a UV light, which make your clothes appear whiter than they really are.


Since light is a form of energy, in order for things to glow in the dark, you have to add energy first. So where does the energy come from? There are are few different ways to do this:


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Materials:


  • UV black fluorescent light (check shopping list to find out where to get one)
  • dark evening inside your house

Light bulbs use incandescence, meaning that the tungsten wire inside a light bulb gets so hot that it gives of light. Unfortunately, bulbs also give off a lot of heat, too. Incandescence happens when your electric stove glows cherry red-hot. Our sun gives off energy through incandescence also – a lot of it.


On the other end of things, cold light refers to the light from a glow stick, called luminescence. A chemical reaction (chemiluminescence) starts between two liquids, and the energy is released in the form of light. On the atomic scale, the energy from the reaction bumps the electron to a higher shell, and when it relaxes back down it emits a photon of light.


Phosphorescence light is the ‘glow-in-the-dark’ kind you have to ‘charge up’ with a light source. This delayed afterglow happens because the electron gets stuck in a higher energy state. Lots of toys and stick-on stars are coated with phosphorescent paints.


Triboluminescence is the spark you see when you smack two quartz crystals together in the dark. Other minerals spark when struck together, but you don’t have to be a rock hound to see this one in action – just take a Wint-O-Green lifesaver in a dark closet with a mirror and you’ll get your own spark show. The spark is basically light from friction.


Fluorescence is what you see on those dark amusement-park rides that have UV lights all around to make objects glow. The object (like a rock) will absorb the UV light and remit a completely different color. The light strikes the electron and bumps it up a level, and when the electron relaxed back down, emits a photon.



 
Download Student Worksheet & Exercises


Whew! There’s a lot to know about glow in the dark stuff, isn’t there? Let’s pull all this together and go on a Treasure Hunt. This hunt is best done just before bed, when it’s already dark outside. All you need is 20 minutes and a UV black light. Ready?


Here’s what you do: Shut off all the lights in the house and go around armed with your UV light, finding things that glow both inside and outside the house. I’ve found some surprises, including a batch of screaming yellow masking tape, eye-popping orange near the microwave (someone’s spillover from lunch?), and garishly green rocks just outside. Our teeth, laundry soap, and sneakers were way fun, too! What fluoresces in your house? Have fun!


What kind of stuff glows under a black light?

Loads of stuff! There are a bunch of everyday things that fluoresce (glow) when under a black light. Note – black lights emit UV light, some of which you can’t see (just like you can’t see infrared – the beam emitted from the remote control to the TV). By the way, that’s why “black lights” were named as such. The reason stuff glows is that fluorescent objects absorb the UV light and then spit it back almost instantaneously. Some of that energy gets lost during that process, and that changes the wavelength of the light, which makes this light visible and causes the material to appear to ‘glow’.


Here are some things that glow: white paper (although paper made pre-1950 doesn’t, which is how investigators tell the difference between originals and fakes), club soda or tonic water (it’s the quinine that glows blue), body fluids (yes, blood, urine, and more are all fluorescent), Vitamins (Vitamin A, B, B-12 (crush and dissolve in vinegar first), thiamine, niacin, and riboflavin are strongly fluorescent), chlorophyll (grind spinach in a small amount of alcohol (vodka) and pour it through a coffee filter to get the extract (keep the solids in the filter, not the liquid)), antifreeze, laundry detergents, tooth whiteners, postage stamps, driver’s license, jellyfish, and certain rocks (fluorite, calcite, gypsum, ruby, talc, opal, agate, quartz, amber) and the Hope Diamond (which is blue in regular light, but glows red).


When you purchase your UV fluorescent “black lights”, be sure to get the LONG WAVE version (short wave UV is the kind that causes permanent damage to living things – that’s how they kill the bacteria in water), and it appears that UV fluorescent lamps work better than the UV LEDs currently on the market, usually sold as “UV Flashlights”. We tried both, and the stuff shone brighter with the fluorescent lamps.


Exercises


  1.  Why are incandescent lights less energy-efficient than fluorescent lights?
  2.  What are the two types of fluorescent lights?
  3. What kinds of things did you find that glow on your treasure hunt? Give at least five examples.

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When light rays strikes a surface, part of the beam passes through the surface and the rest reflects back, like a ball bouncing on the ground. Where it bounces depends on how you throw the ball.


Have you ever looked into a pool of clear, still water and seen your own face? The surface of the water acts like a mirror and you can see your reflection. (In fact, before mirrors were invented, this was the only way people had to look at themselves.) If you were swimming below the surface, you’d still see your own face – the mirror effect works both ways.


Have you ever broken a pencil by sticking it into a glass of water?  The pencil isn’t really broken, but it sure looks like it!  What’s going on?


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Tall glass of water, with a red pensil inside.When a beam of light hits a different substance (like the water), the wavelength changes because the speed of the light changes. If you’re thinking that the speed of light is always constant, you’re right… in a vacuum like outer space between two reference frames.


But here on Earth, we can change the speed of light just by shining a light beam through different materials, like water, ice, blue sunglasses, smoke, fog, even our own atmosphere. How much the light speed slows down depends on what the material is made of.  Mineral oil and window glass will slow light down more than water, but not as much as diamonds do.


How broken the pencil appears also depends on where you look.  In some cases, you’ll see a perfectly intact pencil.  Other times, you’ll guess neither piece is touching.  This is why not everyone can see a rainbow after it rains.  The sun must be at a low angle in the sky, and also behind you for a rainbow to appear.  Most times, you aren’t at the right spot to see the entire arc touch the ground at both ends, either.


Lenses work to bend light the way you want them to. The simplest lenses are actually prisms.  Prisms unmix light into its different wavelengths. When light hits the prism, most of it passes through (a bit does reflect back) and changes speed.  Since the sunlight is made up of many different wavelengths (colors), each color gets bent by different amounts, and you see a rainbow out the other side.


Double Your Money

Here are a few neat activities that experiment with bending light, doubling your money, and breaking objects. Here’s what you do:


Materials:


  • glass jar (or water glass)
  • penny
  • eyeballs


Download Student Worksheet & Exercises


Here’s what you do:


1. Toss one coin into a water glass (pickle jars work great) and fill with an inch of water. Hold the glass up and find where you need to look to see TWO coins. Are the coins both the same size? Which one is the original coin? (Answer at the bottom of this page.)


2. Look through the top of the glass – how many coins are there now? What about when you look from the side?


3. Toss in a second coin – now how many are there?


4. Remove the coins turn out the lights. Shine a flashlight beam through the glass onto a nearby wall. (Hint – if this doesn’t work, try using a square clear container.) Stick a piece of paper on the wall where your light beam is and outline the beam with a pencil.


5. Shine the light at an angle up through the water so that it bounces off the surface of the water from underneath. Trace your new outline and compare… are they both the same shape?


6. Add a teaspoon of milk and stir gently. (No milk? Try sprinkling in a bit of white flour.) Now shine your flashlight through the container as you did in steps 4 and 5 and notice how the beam looks.


7. Use a round container instead of square… what’s the difference?


Answers:
1. The smaller coin is the reflection.
2. One coin when glanced from above, two from the side.
3. Four.
4. Beam is a circle.
5. Beam is an oval.
6. I can see the beam through the water!!
7. The round container distorts the beam, and the square container keeps the light beam straight. Both are fun!


The coin water trick is a neat way for kids to see how refraction works. In optics, refraction happens when light  waves travel from one medium with a certain refractive index (air, for example) to another medium which has a different refractive index (like water).  At the boundary between the two (where air meets water), the wave changes direction.


The wavelength increases or decreases but the frequency remains constant. When you sine light through a prism, the wavelength changes and you see a rainbow as the prism un-mixes white light into its different colors.The light wave changed direction when it traveled from air to glass, and then back to air again as it leaves the backside of the prism.


Did you try the pencil experiment? Did you notice how if you look at the pencil (placed at a slant) partially in the water, it appears to bend at the water’s surface? The light waves bend as they travel from water to air. To further complicate things, the way the eye received information about the position of the pencil actually makes the pencil to appear higher and the water shallower than they really are! Can you imagine how important this is for trying to spear a fish? The fish might appear to be in a different place, so you need to account for this when you take aim!


Click here for the Disappearing Beaker experiment!


Exercises


  1. When one coin is in the water, you can actually see two:  Are the coins both the same size? Which one is the original coin?
  2. In step 2 of the experiment: How many coins are there when viewed from the top of the glass? What about when you look from the side?
  3. What happened when you tossed in a second coin?
  4. How did your outlines compare?

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Have you ever wondered why the sky is blue? Or why the sunset is red? Or what color our sunset would be if we had a blue giant instead of a white star? This lab will answer those questions by showing how light is scattered by the atmosphere.


Particles in the atmosphere determine the color of the planet and the colors we see on its surface. The color of the star also affects the color of the sunset and of the planet.


Materials


  • Glass jar
  • Flashlight
  • Fingernail polish (red, yellow, green, blue)
  • Clear tape
  • Water
  • Dark room
  • Few drops of milk

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Download Student Worksheet & Exercises


  1. Make your room as dark as possible for this experiment to work.
  2. Make sure your label is removed from the glass jar or you won’t be able to see what’s going on.
  3. Fill the clear glass jar with water.
  4. Add a teaspoon or two of milk (or cornstarch) and swirl.
  5. Shine the flashlight down from the top and look from the side – the water should have a bluish hue. The small milk droplets scatter the light the same way our atmosphere’s dust particles scatter sunlight.
  6. Try shining the light up from the base – where do you need to look in order to see a faint red/pink tint? If not, it’s because you are looking for hues that match our real atmosphere, and the jar just isn’t that big, nor is your flashlight strong enough! Instead, look for a very slight color shift. If you do this experiment after being in the dark for about 10 minutes (letting your eyes adjust to the lack of light), it is easier to see the subtle color changes. Just be careful that you don’t let the brilliant flashlight ruin your newly acquired night-vision, or you’ll have to start the 10 minutes all over again.
  7. If you are still having trouble seeing the color changes, shine your light through the jar and onto an index card on the other side. You should see slight color changes on the white card.
  8. Cover the flashlight lens with clear tape.
  9. Paint on the tape (not the lens) the fingernail polish you need to complete the table.
  10. Repeat steps 7-9 and record your data.

What’s Going On?

Why is the sunset red? The colors you see in the sky depends on how light bounces around. The red/orange colors of sunset and sunrise happen because of the low angle the Sun makes with the atmosphere, skipping the light off dust and dirt (not to mention solid aerosols, soot, and smog). Sunsets are usually more spectacular than sunrises, as more “stuff” floats around at the end of the day (there are less particles present in the mornings). Sometimes just after sunset, a green flash can be seen ejecting from the setting Sun.


The Earth appears blue to the astronauts in space because the shorter, faster wavelengths are reflected off the upper atmosphere. The sunsets appear red because the slower, longer wavelengths bounce off the clouds.Sunsets on other planets are different because they are farther (or closer) to the Sun, and also because they have a different atmosphere than planet Earth. The image shown here is a sunset on Mars. Uranus and Neptune appear blue because the methane in the upper atmosphere reflects the Sun’s light and the methane absorbs the red light, allowing blue to bounce back out.


sunset-mars


Exercises


  1. What colors does the sunset go through?
  2. Does the color of the light source matter?

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In this experiment, water is our prism. A prism un-mixes light back into its original colors of red, green, and blue. You can make prisms out of glass, plastic, water, oil, or anything else you can think of that allows light to zip through.


What’s a prism? Think  of a beam of light.  It zooms fast on a straight path, until it hits something (like a water drop).  As the light goes through the water drop, it changes speed (refraction). The speed change depends on the angle that the light hits the water, and what the drop is made of.  (If it was a drop of mineral oil, the light would slow down a bit more.) Okay, so when white light passes through a prism (or water drop), changes speed, and turns colors.  So why do we see a rainbow, not just one color coming out the other side?


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The secret is because the light is made up of different wavelengths, and each gets bent by different amounts when they hit a new material. So one wave changes speed to red, another to yellow, another to green, etc. when the beam hits the prism. And water drops are tiny prisms.


The light passing through a water drop gets refracted twice, not once.  The first time is when it enters the water drop, the second when it bounces off the other side of the drop and reflects back through the water drop and out again (some of the light does make it out the other side of the drop, but most of it bounces back).  When the light emerges from the water drop, it changes speed again, and presto! You have a rainbow.


Natural rainbows (the ones that you see after it rains) happen when water drops (tiny prisms) in the air are hit by sunlight from behind you at just the right angle (which is relatively a low angle, near the ground).  The best rainbows can be seen when half of the sky is darkened with rainclouds and you’re in a clear patch with sun behind you. And guess what?  You can even see a nighttime rainbow (called a moonbow), although they’re pretty rare, usually near full moon.


Here’s what you do:


Materials:


  • mirror
  • shallow baking dish
  • water
  • sunlight


 
Download Student Worksheet & Exercises


Set a clear tray of water in sunlight. Lean a mirror against an inside edge and adjust so that a rainbow appears on the wall. You can also use a light bulb shining through a slit in a flat cardboard piece as a light source.


Troubleshooting: This is one of the easiest experiments to do, and the most beautiful. The trouble is, you don’t know where the water shadow will show up, so make sure you point the mirror to the sky and play with the angle of the mirror until you find the wavering rainbow. Because the shadow is constantly moving, you can snap a few pictures when you’ve got it so you can look over the finer details later. If this project still eludes you, take a large sheet and use it instead of the tiny index card.


Exercises


  1.   What serves as the prism in this experiment?
  2.   What property can help make something a good prism material?
  3. What are some other items that could be used as prisms?

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In a simplest sense, a kaleidoscope is a tube lined with mirrors. Whether you leave the end opened or tape on a bag of beads is up to you, but the main idea is to provide enough of an optical illusion to wow your friends. Did you know that by changing the shape and size of the mirrors, you can make the illusion 3D?


If you use only two mirrors, you’ll get a solid background, but add a third mirror and tilt together into a triangle (as shown in the video) and you’ll get the entire field filled with the pattern. You can place transparent objects at the end (like marbles floating in water or mineral oil) or just leave it open and point at the night stars.


The first kaleidoscopes were constructed in 1816 by a scientist while studying polarization. They were quickly picked up as an amusement gadget by the public and have stayed with us ever since.


Materials:


  • three mirrors the same size
  • tape and scissors

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Download Student Worksheet & Exercises


Here’s what you do: Carefully tape together three identical mirrors, making a triangle-tube with the mirrors on the inside. (You can also use Mylar or silver wrapping paper taped to cardboard instead of mirrors.) Tape all rough edges well and peek through the opening as you walk around.


Variations: By changing the size and shape of the mirrors, you can change the dimensional effect you see. Just be sure to look at the mirror surface, not the opening. You can also make mirrors wider at the bottom and narrower at the top (easier with cardboard mirrors); use four or five mirrors instead of three; change the length of the mirrors; use curved mirrors instead of flat (find curved cardboard from an oatmeal box or carefully cut apart a soda can and tape Mylar or spray with chrome paint from the hardware store).


Exercises


  1. What is a light source?
  2. What is a light reflector?
  3. Sketch an image of something interesting that you were able to see as the light reflected from the multiple surfaces of the kaleidoscope to your eyes:

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ss-lwImagine you’re a painter.  What three colors do you need to make up any color in the universe?  (You should be thinking: red, yellow, and blue… and yes, you are right if you’re thinking that the real primary colors are cyan, magenta, and yellow, but some folks still prefer to think of the primary colors as red-yellow-blue… either way, it’s really not important to this experiment which primary set you choose.)


Here’s a trick question – can you make the color “yellow” with only red, green, and blue as your color palette?  If you’re a scientist, it’s not a problem.  But if you’re an artist, you’re in trouble already.


The key is that we would be mixing light, not paint.  Mixing the three primary colors of light gives white light.  If you took three light bulbs (red, green, and blue) and shined them on the ceiling, you’d see white.  And if you could magically un-mix the white colors, you’d get the rainbow (which is exactly what prisms do.)


If you’re thinking yellow should be a primary color – it is a primary color, but only in the artist’s world.  Yellow paint is a primary color for painters, but yellow light is actually made from red and green light.  (Easy way to remember this: think of Christmas colors – red and green merge to make the yellow star on top of the tree.) It’s because you are using projection of light, not the subtrative combination of colors to get this result.


Here’s a nifty experiment that will really bring these ideas to life (and light!):


Materials:


  • flashlight (three is best, but you can get by with two)
  • fingernail polish (red, green, and blue)
  • clear tape or cellophane (saran wrap works too)
  • white wall space

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Download Student Worksheet & Exercises


Here’s what you do: Find three flashlights. Cover each with colored cellophane (color filters) or paint the plastic lens cover with nail polish (red, green, and blue). Shine onto a white ceiling or wall, overlap the colors and make new colors. Leave the flashlights on, line them up on a table, turn off the lights, and dance – you will be making rainbow shadows on the wall! In addition, you can paint the lens of a fourth flashlight yellow to see what happens.


When you combine red and green light, you will get yellow light. Combine green and blue to get cyan (turquoise). Combine blue and red to get magenta (purple). Turn on the red and green lights and the wall will appear yellow. Wave your hand in front of the lights and you will see cyan and magenta shadows. Turn on the green and blue lights, and the wall turns cyan with yellow and magenta shadows. Turning on the blue and red give a magenta wall with yellow and cyan shadows. Turn on all colors and you will get a white wall with cyan, yellow, and magenta shadows – rainbow shadows!


Troubleshooting: This experiment has a few things to be aware of. If you’re not getting the colored shadows, check to be sure that the flashlight is bright enough to illuminate a wall in the dark. Be sure to shut the doors, shades, windows, and drapes. In the dark, when you shine your red flashlight on the wall, the wall should glow red. Beware of using off-color nail polish – make sure it’s really red, not hot pink.


If you still need help making this experiment work, you can visit your local hardware store and find three flood lamp holders (the cheap clamp-style ones made from aluminum work well – you’ll need three) and screw in colored “party lights” (make one red, one green, and one blue), which are colored incandescent bulbs. These will provide a lot more light! You can also add a fourth yellow light to further illustrate how yellow light isn’t a primary color. Try using only red, yellow, and blue… you’ll quickly find that you can’t obtain all the colors as you could with the original red-green-blue lights.


Exercises


  1.  What are the three primary colors of light?
  2.  What color do you get when mixing the primary colors of light?
  3. How do you mix the primary colors of light to get yellow?
  4. Use crayons or colored pencils to draw what you saw when all three lights were shining on the wall and you waved your hand in front of the light.

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Why do families share similar features like eye and hair color? Why aren’t they exact clones of each other? These questions and many more will be answered as well look into the fascinating world of genetics!


Genetics asks which features are passed on from generation to generation in living things. It also tries to explain how those features are passed on (or not passed on). Which features are stay and leave depend on the genes of the organism and the environment the organism lives in. Genes are the “inheritance factors “described in Mendel’s laws. The genes are passed on from generation to generation and instruct the cell how to make proteins. A genotype refers to the genetic make-up of a trait, while phenotype refers to the physical manifestation of the trait.


We’re going to create a family using genetics!


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Materials
• Paper or use this Genetics Table
• Two different coins
• Scissors
• Glue or Tape



Download Student Worksheet & Exercises


Step one: Creating the Parent Generation

  1. First you’re going to create the genetic make-up of the parents. Here’s how:
  2. Take out the Genetics Data Table, and flip the first coin to create the genetic profile for the mother.
  3. Flip the coin and in the Mother’s Hair trait column, write D for dominant if the coin reads heads, and R for recessive if tails in the table.
  4. Flip the coin again. In the Mother’s Hair trait column right after the first trait, write D for dominant if the coin reads heads, and R for recessive if tails in the table.
  5. If you flipped heads the first time and tails the second, you’d write “DR” in the Mother’s Hair box.
  6. Continue this process for all of Mother’s traits. You should have two letters in each box for the entire column.
  7. Repeat steps 3-6 for Father. When you’ve completely filled out Mother’s and Father’s columns, you’ve completed the paternal genetic profile. Now you’re ready for the next part:

Step two: The Child

  1. Will the child be a boy or a girl? To determine this, flip the second coin. Heads for a boy, tails for a girl. After this is decided, circle boy or girl under “child 1” on the Genetics Data Table.
  2. Now the first coin will represent the gene from the mother and the second coin will represent the gene from the father.
  3. Start with the Hair trait: Flip both coins. If the first coin is tails, take the first trait from the mother. If the first coin is heads, take the second trait.
    1. For example, if the first coin is tails, and the mother’s code is DR, then write “D” in the child one column for hair.
    2. Do the same thing for the father’s traits with the second coin. For example, if the second coin is heads, and the father’s code is DR, then write “R” in the Hair Trait column of child 1.
    3. By the end of this step, child 1 should have one letter from the mother, and one letter for the father in child 1’s hair trait column.
  4. Use the same steps used to find the genetic code for the hair trait to find the code for the rest of the traits. By the end all the traits should have one letter from the mother’s genetic code and one letter from the father’s genetic code.

Step 3: What the Child Looks Like

Grab a sheet of paper and start drawing the child. If the genetic code for a trait has a “D” in it, then the dominant trait is used.


For example, if the hair color is DD, DR, or RD then the hair color is dark. If the hair color code is RR, then the hair color is light. Draw the traits on your paper!


You can repeat this for as many children as you would like in your family.


Step 4: Make another family and compare!

Are all families alike? What if you try this process again for another family? Do you see any similarities or differences? Do similar features come from dominant genes? Do differences come from recessive genes? What other traits would you include? Write this in your science journal!


Conclusions:

In fact, most similarities should come from the dominant genes because they are expressed more often. The recessive genes are expressed less often, so the create the differences.


Extra credit:

What percent of the children expressed the dominant allele of each trait? Did you get Mendel’s results? Do the calculations and check it out!


Exercises


  1. What is the difference between a genotype and a phenotype?
  2. What is a dominant trait?
  3. What is a recessive trait?
  4. Assume B=Black hair and b=blond hair.  Make a Punnet square to cross Bb with bb. Tell what the possibilities are for offspring hair color.
  5. Why don’t traits simply average out in offspring.  For example, why does a tall plant crossed with a short plant not yield a bunch of average-sized plants?
  6. In your activity, what percent of the children expressed the dominant allele of each trait? Did you get Mendel’s results? Do the calculations and check it out!

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Plants need light, water, and soil to grow. If you provide those things, you can make your own greenhouse where you can easily observe plants growing. Here’s a simple experiment on how to use the stuff from your recycling bin to make your own garden greenhouse.


We’ll first look at how to make a standard, ordinary greenhouse. Once your plants start to grow, use the second part of this experiment to track your plant growth. Once you’ve got the hang of how to make a bottle garden, then you can try growing a carnivorous greenhouse.
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Materials:


  • 2 liter bottle
  • scissors or razor
  • gravel or sand
  • spanish moss
  • dish or plate
  • seeds of your choice

Experiment:


  1. Using an exacto knife or scissors, cut the label from the soda bottle. Carefully cut the bottle in half so that the bottom (container) piece is deep enough to hold soil and plants. Poke a few holes into the bottom of the container for drainage.
  2. Fill the bottom of the bottle with a half cup of sand or gravel to provide drainage. Use playground sand, aquarium gravel or small stones picked up from a hike. If sand or gravel isn’t available, crush an old clay pot and use that. (Let an adult crush the pot.)
  3. Place a 1-inch layer of Spanish or Spaghnum moss in the mini greenhouse to keep the soil from mixing with the rock layer. Place a thick layer of potting soil on top of the moss, at least 4 inches deep or 1 inch from the top. Tamp down lightly with your finger
  4. Put the top half of the soda bottle back on, tucking inside the edges of the container. If necessary, you can cut small slits into the upper portion to make it fit. Leave the cap on.
  5. Place atop a waterproof plate in a sunny spot and water sparingly. The lid retains moisture and heat, so your seeds should sprout quickly. Because the plastic is clear, you’ll be able to see the roots beneath the surface of the soil. If the greenhouse gets too steamy, you can remove the lid once in a while. When your seedlings get big enough, transplant to the garden, and plant a new crop!

Tracking Plant Growth

You know that plants grow… but when a plant grows, is the entire stem getting longer, like rolling dough, or is only the tip growing, like squeezing the end of a toothpaste tube?


This simple experiment can give you the answer. Ready?


  1. Tie string around the edge of a plants stem, between the last leaf at the end, and the next leaf.
  2. Make observations as the plant grows.

What’s going on? If the entire stem grows, your string will always stay at the end. If just the tip grows, the string will become further and further from the edge. Which is it? Are you surprised?


Carnivorous Greenhouse

Was the last activity too tame for you? You’ll need to order carnivorous plant seeds. Carnivorous plants are heterotrophs. As you learned, this means they must get their energy from other organisms instead of the sun. Such plants are good at catching small animals, such as insects, to eat. Used the video below to learn how to plant the seeds that will produce these carnivores, and how to care for them once they have sprouted.



Download Student Worksheet & Exercises


Exercises


  1. What is a carnivorous plant?
  2.  What is another name for a carnivorous plant?
  3.  What does a carnivorous plant need to thrive?
  4.  Should we fertilize a carnivorous plant? Why or why not?

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The way animals and plants behave is so complicated because it not only depends on climate, water availability, competition for resources, nutrients available, and disease presence but also having the patience and ability to study them close-up.


We’re going to build an eco-system where you’ll farm prey stock for the predators so you’ll be able to view their behavior. You’ll also get a chance to watch both of them feed, hatch, molt, and more! You’ll observe closely the two different organisms and learn all about the way they live, eat, and are eaten.


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This experiment comes in two parts. The materials you need for both parts are:


  • four 2-liter soda bottles, empty and clean
  • 2 bottle caps
  • one plastic lid that fits inside the soda bottle
  • small piece of fruit to feed fruit flies
  • aluminum foil
  • plastic container with a snap-lid (like an M&M container or film can)
  • scissors and razor with adult help
  • tape
  • ruler
  • predators: spiders OR praying mantis OR carnivorous plants (if you’re using carnivorous plants, make sure you do this Carnivorous Greenhouse experiment first so you know how to grow them successfully)
  • soil, twigs, small plants

Fruit Fly Trap

In order to build this experiment, you first need prey. We’re going to make a fruit fly trap to start your prey farm, and once this is established, then you can build the predator column. Here’s what you need to do to build the prey farm:



Download Student Worksheet & Exercises


Did you know that fruit flies don’t really eat fruit? They actually eat the yeast that growing on the fruit. Fruit flies actually bring the yeast with them on the pads of their feet and spread the yeast to the fruit so that they can eat it. You can tell if a fruit fly has been on your fuit because yeast has begun to spread on the skin.


When you have enough fruit flies to transfer to the predator-prey column, put the entire fruit fly trap in the refrigerator for a half hour to slow the flies down so you can move them.


If you find you’ve got way too many fruit flies, you might want to trap them instead of breed them. Remove the foil buckets every 4-7 days or when you see larvae on the fruit, and replace with fresh ones and toss the fruit away. Don’t toss the larvae in the trash, or you’ll never get rid of them from your trash area! Put them down the drain with plenty of water.


Predator-Prey Column

You can use carnivorous plants, small spiders, or praying mantises. If you use plants, choose venus flytraps, sundews, or butterworts and make sure your soil is boggy and acidic. You can add a bit of activated charcoal to the soil if you need to change the pH. Since the plants like warm, humid environments, keep the soil moist enough for water to fog up the inside on a regular basis. You know you’ve got too much moisture inside if you find algae on the plants and dirt. (If this happens, poke a couple of air holes.) Don’t forget to only use distilled water for the carnivorous plants!


Keep the column out of direct sunlight so you don’t cook your plants and animals.



Exercises


  1. What shape is the head of the mantis?
  2.  How many eyes does a praying mantis have?
  3.  How else has the mantis head evolved to stalk their prey?
  4.  How does a praying mantis hold its food?
  5.  Do fruit flies eat fruit?
  6.  How do predators and prey change over time?

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What grows in the corner of your windowsill? In the cracks in the sidewalk? Under the front steps? In the gutter at the bottom of the driveway? Specifically, how  doe these animals build their homes and how much space do they need? What do they eat? Where do fish get their food? How do ants find their next meal?


These are hard questions to answer if you don’t have a chance to observe these animals up-close. By building an eco-system, you’ll get to observe and investigate the habits and behaviors of your favorite animals. This column will have an aquarium section, a decomposition chamber with fruit flies or worms, and a predator chamber, with water that flows through all sections. This is a great way to see how the water cycle, insects, plants, soil, and marine animals all work together and interact.


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Here’s what you need:


  • four (or more) 2-liter soda bottles, empty and clean and with caps
  • scissors
  • tape
  • razor with adult help
  • ruler
  • soil
  • water
  • plants or seeds
  • compost or organic/food scraps
  • spiders, snails, fruit flies, etc

Here’s what you do:



Download Student Worksheet & Exercises


You can easily incorporate the Water Cycle Column, the Terraqua Column, the Predator-Prey Column, Worm Column, and the Fruit Fly Trap into your Eco-Column. If you want to make your Eco-Column more permanent, seal it together with silicone sealant, making sure you have enough drainage holes and air holes in the right places first.


Exercises


  1. What are parts of the eco system?
  1. Give an example of each.
  1. What do decomposers do?
  1. How do fruit flies breed?
  1. How does the precipitation funnel function in this eco column?

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Some insects are just too small! Even if we try to carefully pick them up with forceps, they either escape or are crushed. What to do?


Answer: Make an insect aspirator! An insect aspirator is a simple tool scientists use to collect bugs and insects that are too small to be picked up manually. Basically it’s a mini bug vacuum!


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Download Student Worksheet & Exercises


Here’s what we’ll need:


  • A small vial or test tube with a (snug fitting) two-holed rubber stopper.
  • Two short pieces of stiff plastic tubing. We’ll call them tube A and tube B.
  • Fine wire mesh (very small holes because this is what will stop the bugs from going into your mouth!)
  • A cotton ball.
  • One to two feet of flexible rubber tubing.
  • Duct tape or a rubber band.

Here’s how we make it:


  • Insert the tube A and Tube B into the stopper such that the stopper is in the middle of both pieces.
  • Bend both A and B plastic tubing 90 degrees away from each other. Their ends should be pointing away from each other.
  • Cut a square of mesh large enough to the end of the plastic tubing. Tape (or rubber-band) the mesh over bottom of tube A only. Remember, if you cover both of the tubes the bugs won’t be able to enter the aspirator.
  • Insert a small amount of cotton ball into the other side of tube A (not enough to block airflow, just enough to help filter the dust and particles entering the vial.
  • Cut another piece of mesh and cover the other end of Tube A. Secure that mesh with another piece of tape/rubber band.
  •  Fit the rubber tubing over the top of tube B (the bent side).
  • Fit the stopper into the vial/test tube.

How it works: To use the aspirator, hold the end of the rubber tubing near the insects you want to collect, and suck through the top of tube A. The vacuum you create sucks the insects into the vial/test tub (make sure they can fit in the tube!).


Troubleshooting: The bugs aren’t being pulled into the vial! In that case the suction may not be strong enough. Remove the cotton ball and try again. If it still is not working check to make sure the aspirator is air-tight (is the stopper fitting snuggly into the vial? Are there cracks/holes around or in the plastic tubes?).


TIP: I kept eating bugs! Make sure your wire mesh is very fine (the holes are smaller than the bugs you’re trying to collect). Otherwise you may be ordering a lunch you don’t want!


Exercises


  1. Why don’t we use a large vacuum to suck up the bugs?
  2.  Why do we need a small mesh covering on the end of the straw that we suck on?
  3.  Why do we need to be careful about catching ants?
  4.  What insects did you catch that you rarely see?
  5.  What familiar insects did you catch? (answers may vary).

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Art and science meet in a plant press. Whether you want to include the interesting flora you find in your scientific journal, or make a beautiful handmade greeting card, a plant press is invaluable. They are very cheap and easy to make, too!


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Here’s what you need:


  • Newspaper
  • Cardboard
  • Belt buckle or large, strong rubber bands
  • Sheets of paper


 



Download Student Worksheet & Exercises


Here’s how you make it:


  1. Cut the cardboard into square pieces.
  2. Cut or fold the sheets of newspaper into squares the same size as the cardboard.
  3. Place 4 sheets of newspaper between each piece of cardboard. You can also use white copy paper.
  4. Place the plants you want to press in between the newspaper.
  5. If you want, you can sandwich the plant press with the wood planks for added pressure.
  6. Bind it tightly with the rubber bands or a belt buckle.
  7. Leave it in a dry place for two to four days.

How does it work? The pressure from the rubber band/string pushes the water from the plants. The water is then absorbed by the newspaper. Since the pressure is the key to the press, it’s important not to open the press for at least two days (more is better).


Troubleshooting: The press works by pushing the moisture out of the plants, so any way moisture can stay in (or get back in) to the plants will make the press less effective. First, storing the press in a dry place is essential. If the press is left in a moist area not only will in not work, but it will grow mold and ruin the press and the plants. Conversely, if the pressure is not great enough, the moisture will not be pressed out. Thus make sure that the plants fit in the press, are bound tightly, and that the press is stored in a dry area for at very least two days.


Exercises


  1. Draw and describe the functions of the following plant parts: root, stem.
  2. What two major processes happen at the leaf?
  3. Why are flowers necessary?
  4. Do all plants have roots, stems, leaves and flowers?

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If you’re thinking sunlight, you’re right. Natural light is best for plants for any part of the plant’s life cycle. But what can you offer indoor plants?


In Unit 9 we learned how light contains different colors (wavelengths), and it’s important to understand which wavelengths your indoor plant prefers.


Plants make their food through photosynthesis: the chlorophyll transforms carbon dioxide into food. Three things influence the growth of the plant: the intensity of the light, the time the plant is exposed to light, and the color of the light.


When plants grow in sunlight, they get full intensity and the full spectrum of all wavelengths. However, plants only really use the red and blue wavelengths. Blue light helps the leaves and stems grow (which means more area for photosynthesis) and seedlings start, so fluorescent lights are a good choice, since they are high in blue wavelengths.


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For my fourth grade science project, I placed a box over a plant and poked different colored lights into each upper corner to see which way the plant grew. It turned out that my plant grew toward the blue light the most.  When I turned off the red light, my little plant stopped flowering, but started flowering again when the red light turned on.


After doing my homework, I learned that chemicals in my plant respond to light and dark conditions, which means that my little plant could “tell time” by using chemistry. Not the 12-hour clock that we use to tell time with, but they know time over a longer period, like when to flower in a season and when to conserve energy for winter.


I know now that if I had indoor plants, I’d choose fluorescent bulbs high in the blue wavelengths, and I’d also add an incandescent bulb if my plant had flowers I wanted to blossom. Since incandescent also produces heat, I’d also try playing with red LED lights which weren’t available to me when I did my project, but would make an interesting study today!


Here’s a video on what happens if you use a black light with indoor plants:



The scientific method is used by scientists to answer questions and solve problems. Often, good scientific questions are best on things we already know. For example, we know plants need light to grow because the light allows them to make their own food, but what color of light is best? Use the scientific method in the lab below to figure it out.


Experiment:


  • Place four plants in an area that will get minimal natural lighting.
  • Do some colors of light help plants grow better than plain white light? Make a hypothesis about this question.
  • To test things out, grow one plant with plain white light. Grow the other plants with colored light, either by using colored bulbs or by covering white bulbs with tissue paper.
  • Make daily observations. Which plant grew best? Was your hypothesis correct?

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How does salt affect plant growth, like when we use salt to de-ice snowy winter roads? How does adding fertilizer to the soil help or hurt the plants? What type of soil best purifies the water? All these questions and more can be answered by building a terrarium-aquarium system to discover how these systems are connected together.


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Here’s what you need:


  • two 2-liter soda bottles, empty and clean
  • two bottle caps
  • scissors and razor with adult help
  • tape
  • water, soil, and plants

Here’s what you do:




Download Student Worksheet & Exercises


Water drips off the roof of your house, down your driveway, over your toothbrush and down the sink, through farm fields, and into rivers, lakes and oceans. While traveling, this water picks up litter, nutrients, salts, oil, and also gets purified by running through soil. All of this has an affect on fish and animals that live in the oceans. The question is, how does it affect the marine ecosystem? That’s what this experiment will help you discover.


Land and aquatic plants are excellent indicators of changes in your terraqua system. By using fast-germinating plats, you’ll see the changes in a relatively short about of time. You can also try grass seeds (lawn mixes are good, too), as well as radishes and beans. Pick seeds that have a life cycle of less than 45 days.


How to Care for your TAC (Terra-Aqua Column) EcoSystem:

  1. Keep the TAC out of direct sunlight.
  2. Keep your cotton ball very wet using only distilled water. Your plants and triops are very sensitive to the kind of water you use.
  3. Feed your triops once they hatch (see below for instructions)
  4. Keep an eye on plant and algae growth  (see below for tips)

About the plants and animals in your TAC:


  1. Carnivorous plans are easy to grow in your TAC, as they prefer warm, boggy conditions, so here are a few tips: keep the TAC out of direct sunlight but in a well-lit room. Water should condense on the sides of the column, but if lots of black algae start growing on the soil and leaves, poke more air holes! Water your soil with distilled water, or you will burn the roots of your carnivorous plants.  Trim your plants if they crowd your TAC.
  2. If you run out of fruit flies, place a few slices of banana or melon in an aluminum cup or milk jig lid at the bottom of a soda bottle (which has the top half cut off). Invert the top half and place it upside down into the bottom part so it looks like a funnel and seal with tape so the flies can’t escape.  Make a hole in the cap small enough so only one fly can get through. The speed of a fruit fly’s life cycle (10-14 days) depends on the temperature range (75-80 degrees). Transfer the flies to your TAC. If you have too many fruit flies, discard the fruit by putting it outside (away from your trash cans) or flush it down the toilet.
  3. You can’t feed a praying mantis too much, and they must have water at all times. You can place 2-3 baby mantises in a TAC at one time with the fruit flies breeding below. When a mantis molts, it can get eaten by live crickets, so don’t feed if you see it begin to molt. When you see wings develop, they are done fully mature. Adult mantises will need crickets, houseflies, and roaches in addition to fruit flies.
  4. Baby triops will hatch in your TAC aquarium. The first day they do not need food. Crush a green and brown pellet and mix together. Feed your triop half of this mixture on the 2nd and the other half on the 4th day (no food on day 3). After a week, feed one pellet per day, alternating between green and brown pellets. You can also feed them shredded carrot or brine shrimp to grow them larger. If you need to add water (or if the water is too muddy), you can replace half the water with fresh, room temperature distilled water. You can add glowing beads when your triop is 5 days old so you can see them swimming at night (poke these through the access hole).

Exercises


  1.  What three things do plants need to survive?
  2.  What two things do animals need to survive?
  3.  Does salt affect plants? How?

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Flowering plants can be divided into monocotyledons and dicotyledons (monocots and dicots). The name is based on how many leaves sprout from the seed, but there are other ways to tell them apart. For monocots, these will be in multiples of three (wheat is an example of a monocot). If you count the number of petals on the flower, it would have either three, six, nine, or a multiple of three. For dicots, the parts will be in multiples of four or five, so a dicot flower might have four petals, five petals, eight, ten, etc.

Let's start easy...grab a bunch of leaves and lets try to identify them. Here's what you need to know:

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Materials:

  • lettuce or celery
  • sharp knife with adult help
  • cutting board
  • microscope with slides
  • flowers of your choice

Download Transpiration Lab (for Monocots & Dicots)

Further Experiments:

  1. Source: Wiki

    Most monocots have veins that are parallel, running side by side. To see an example of this, look at a blade of grass. Most dicots have leaves with veins that form networks. Look at the leaf of lettuce, or a leaf from an oak or maple tree. This is not an absolute test, but it will usually put you on the right path.

  2. Another test involves cutting the plant's stem. Use a sharp knife to cut through the stem, and then examine it with a magnifying glass or microscope. You are looking for the vascular tissue that carries food and water through the plant. For dicots, the vascular tissue are arranged in rings or lines. For an easy example of that, chop some celery. The "strings" in the celery is the vascular tissue, and you will find them lined up in a nice row. That tells us that celery is a dicot. For monocots, the vascular bundles are spread through the entire stem. While you are chopping your celery, chop some hearts of palm or some bamboo shoots. Neither will have that distinctive row of vascular tubes, since palms and bamboo are both monocots.
  3. Head for your local grocery store. Look through the produce section, and you should find a wide variety of both monocots and dicots. Most groceries also have a section for live flowers, which will give you a great chance to count some petals.
  4. Look at your flowers. Which are monocots and which are dicots? Why?

 

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When birds and animals drink from lakes, rivers, and ponds, how pure it is? Are they really getting the water they need, or are they getting something else with the water?


This is a great experiment to see how water moves through natural systems. We’ll explore how water and the atmosphere are both polluted and purified, and we’ll investigate how plants and soil help with both of these. We’ll be taking advantage of capillary action by using a wick to move the water from the lower aquarium chamber into the upper soil chamber, where it will both evaporate and transpire (evaporate from the leaves of plants) and rise until it hits a cold front and condenses into rain, which falls into your collection bucket for further analysis.


Sound complicated? It really isn’t, and the best part is that it not only uses parts from your recycling bin but also takes ten minutes to make.


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Here’s what you need:


  • three 2-liter soda bottles, empty and clean
  • razor with adult help
  • scissors
  • tape
  • ruler
  • 60 cm heavy cotton string
  • soil
  • water
  • ice
  • plants
  • drill and drill bits
  • fast-growing plant seeds (radish, grass, turnips, Chinese cabbage, moss, etc.)

Here’s what you do:



Download Student Worksheet & Exercises


Make sure your wicks are thoroughly soaked before adding the soil and plants! You can either add ice cubes to the top chamber or fill it carefully with water and freeze the whole thing solid. If you’re growing plants from seeds, leave the top chamber off until they have sprouted.


You can add a strip of pH paper both inside and outside your soil chamber to test the difference in pH as you introduce different conditions. You can check out the Chemical Matrix Experiment and the Acid-Base Experiment also!) What happens if you light a match, blow it out, and then drop it in the soil chamber? (Hint – you’ve just made acid rain!)


Do you think salt travels with the water? What if you add salt to the aquarium chamber? Will it rain salty water? You can place a bit of moss in the collection bucket to indicate how pure the water is (don’t drink it – that’s never a good idea).


Exercises


  1. Do you think salt travels with the water?
  2. What if you add salt to the aquarium chamber? Will it rain salty water?
  3. What happens if you light a match, blow it out, and then drop it in the soil chamber? (Hint – you’ve just made acid rain!)

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After you've completed this experiment, you can try making your own sound-to-light transformer as shown below. Using the properties of sound waves, we'll be able to actually see sound waves when we aim a flashlight at a drum head and pick up the waves on a nearby wall.

Here's what you need:

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  • empty soup can
  • balloon
  • small mirror
  • tape
  • scissors
  • hot glue gun
  • laser or flashlight

You will be adjusting the length of string of a pendulum until you get a pendulum that has a frequency of .5 Hz, 1 Hz and 2 Hz. Remember, a Hz is one vibration (or in this case swing) per second. So .5 Hz would be half a swing per second (swing one way but not back to the start). 1 Hz would be one full swing per second. Lastly, 2 Hz would be two swings per second. A swing is the same as a vibration so the pendulum must move away from where you dropped it and then swing back to where it began for it to be one full swing/vibration.
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Advanced students: Download your Seeing Sound Waves using Light


This is one of my absolute favorites, because it’s so unexpected and unusual… the setup looks quite harmless, but it makes a sound worse than scratching your nails on a chalkboard. If you can’t find the weird ingredient, just use water and you’ll get nearly the same result (it just takes more practice to get it right). Ready?


NOTE: DO NOT place these anywhere near your ear… keep them straight out in front of you.


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Here’s what you need:


  • water or violin rosin
  • string
  • disposable plastic cup
  • pokey-thing to make a hole in the cup


Download Student Worksheet & Exercises


Exercises


  1. What does the rosin (or water) do in this experiment?
  2. What is vibrating in this experiment?
  3. What is the cup for?

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f18Sound can change according to the speed at which it travels. Another word for sound speed is pitch. When the sound speed slows, the pitch lowers. With clarinet reeds, it’s high. Guitar strings can do both, as they are adjustable. If you look carefully, you can actually see the low pitch strings vibrate back and forth, but the high pitch strings move so quickly it’s hard to see. But you can detect the effects of both with your ears.


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The range of your ears is about 20 – 20,000 Hz (cycles per second). Bats and dogs can hear a lot higher than we can. The image (right) is a real picture of an aircraft as it breaks the sound barrier – meaning that the aircraft is passing the speed that sounds travels at (about 700 mph). The white cloud you see in the photo is related to the shock waves that are forming around the craft as it moves into supersonic speeds. You can think of a shock wave as big pressure front, which creates clouds. In this photo, the pressure from the shock waves is condensing the water vapor in the air.


There are lots of things on earth that break the sound barrier – bullets and bullwhips, for example. The loud crack from a whip is the tip zipping faster than the speed of sound.


shockwaveSo why do we hear a boom at all? Sonic booms are created by air pressure (think of how the water collects at the bow of a boat as it travels through the water). The vehicle pushes air molecules aside in such a way they are compressed to the point where shock waves are formed. These shock waves form two cones, at the nose and tail of the plane. The shock waves move outward and rearward in all directions and usually extend to the ground.


As the shock cones spread across the landscape along the flightpath, they create a continuous sonic boom. The sharp release of pressure, after the buildup by the shock wave, is heard as the sonic boom.



How to Make an Air Horn

Let’s learn how to make loud sonic waves… by making an air horn. Your air horn is a loud example of how sound waves travel through the air. To make an air horn, poke a hole large enough to insert a straw into the bottom end of a black Kodak film canister. (We used the pointy tip of a wooden skewer, but a drill can work also.) Before you insert the straw, poke a second hole in the side of the canister, about halfway up the side.


Here’s what you need:


  • 7-9″ balloon
  • straw
  • film canister
  • drill and drill bits

Grab an un-inflated balloon and place it on your table. See how there are two layers of rubber (the top surface and the bottom surface)? Cut the neck off a balloon and slice it along one of the folded edges (still un-inflated!) so that it now lays in a flat, rubber sheet on your table.


Drape the balloon sheet over the open end of the film canister and snap the lid on top, making sure there’s a good seal (meaning that the balloon is stretched over the entire opening – no gaps). Insert the straw through the bottom end, and blow through the middle hole (in the side of the canister).


You’ll need to play with this a bit to get it right, but it’s worth it! The straw needs to *just* touch the balloon surface inside the canister and at the right angle, so take a deep breath and gently wiggle the straw around until you get a BIG sound. If you’re good enough, you should be able to get two or three harmonics!



 


Download Student Worksheet & Exercises


Troubleshooting: Instead of a rubber band vibrating to make sound, a rubber sheet (in the form of a cut-up balloon) vibrates, and the vibration (sound) shoots out the straw. This is one of the pickiest experiments – meaning that it will take practice for your child to make a sound using this device. The straw needs to barely touch the inside surface of the balloon at just the right angle in order for the balloon to vibrate. Make sure you’re blowing through the hole in the side, not through the straw (although you will be able to make sounds out of both attempts).


Here’s a quick video where you can hear the small sonic boom from a bull whip:



Since most of us don’t have bull whips, might I recommend a twisted wet towel? Just be sure to practice on a fence post, NOT a person!


Exercises 


  1. Why do we use a straw with this experiment?
  2. Does the length of the straw matter? What will affect the pitch of this instrument?

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