Essential Questions:
- What do you know about evaporation?
- What do you know about condensation?
Educational Objective:
The learner will
- List three factors that affect the rate of evaporation of water from an object.
- Demonstrate that evaporation cools an object, while condensation warms it.
- Demonstrate that an object need not be ice cold for water vapor to condense on it; it need only be cooler than the surrounding air.
- Demonstrate that evaporation leaves dissolved substances behind.
Evaporation Experiments #1-#4
Materials:
| # of Students per Item | Item | #of Students per Item | Item |
| Whole Class | 2 identical wet objects such as a towel or a glove | 2 | Shoelace cut into 6 cm strips |
| 6 | Balance scale | 6 | Crumpled wet paper towel and flat wet paper towel |
| 6 | Medicine droppers | 6 | Slides |
| 6 | ¼ cup of salt water | 6 | Magnifying glass |
Condensation Experiments
Materials:
| # of Students per Item | Item | #of Students per Item | Item |
| 6 | Shiny metal can | 6 | Crushed ice mixture |
| 6 | Mayonnaise jar with lid | 6 | 2 thermometers |
| 6 | 2 paper towels | 2 | Medicine dropper |
| 2 | Microscope slide | 2 | Magnifying glass |
Teacher Background:
Evaporation
The temperature of the moisture in a damp object represents a measurement of the average energy contained in the water molecules of that object. Emphasize the words average energy. This means that some molecules have much more energy than the average and some much less. Now, it is the much more energetic molecules that can and do escape into the atmosphere. They evaporate, taking their energy with them. Thus, the water left behind now contains a higher percentage of low-temperature, low-energy molecules. When this happens, heat energy flows from the object into the water and the object is cooled. Of course, the energy from the object speeds up some of the low-temperature water molecules. These can then evaporate, starting the whole cycle again.
Evaporation of water and transpiration by plants depend on the sun's energy. Transpiration is the process by which water escapes from the leaves of plants back into the atmosphere. A single tree may transpire almost 7,000 liters of water into the air during a six-month growing season.
After you have completed all of the experiments with your students, review the following with them. Can they think of a reason why it is said that water absorbs energy when it evaporates? Hint: Which object (towel, mitt) dried faster in the first activity? (The one in the warm place.) Warmth (higher temperature) means more energy is present.
What did the students see that tells them that objects cool when water evaporates from them? (The thermometer with the wet shoelace showed a lower temperature than the one left dry.) To reinforce this learning, have the students put a wet paper towel or some alcohol on their hands and blow on them. The cooling effects of evaporation will be felt easily.
How do we know that a larger surface area causes more (or faster) evaporation? (The paper towel left uncrumpled dried out faster.)
Some Things to Remember About Evaporation
- Water needs energy to evaporate.
- Objects cool when water takes energy from them and evaporates.
- The larger the surface area, the more evaporation takes place.
- Evaporation leaves dissolved substances behind.
Condensation
Condensation occurs if the air is saturated and if dust or salt particles are present. During condensation, water vapor collects around the dust or salt particles called condensation nuclei, and forms tiny droplets of water. Condensation is a loss of energy.
Some Things to Remember About Condensation
- Energy must be removed from water vapor for it to condense.
- Objects on which water condenses gains energy.
- Condensed water is nearly pure water.
Advanced Preparation:
Some of the experiments take more than one day to see the results. Read through all of the experiments first. You will find that you can have a whole class doing a couple of the experiments while waiting for the results of other experiments.
- As with any demonstration or lesson, read the entire lesson first.
- Some of the materials may take a few days to get ready.
- Prepare all of the materials ahead of time.
- Try out all of the experiments before you do them with your students. Humidity will play a significant role in the results of these experiments so you should test them out first.
Science Vocabulary:
- Evaporation: is the change of state from a liquid to a gas.
- Condensation: is the change of state from a gas to a liquid.
Procedure:
Evaporation
Teacher Demonstration: Experiment #1
- Put a wet object (towel, glove, etc.) in a warm place. (A sunny window will do.)
- Put an identical object where it is cooler.
- Compare the two objects in an hour.
Class Experiment #2
- Take a shoelace and cut it into several short lengths. (About 6 cm.)
- Slip equal lengths of cut shoelaces around the bulbs of two similar thermometers. (Most shoelaces are hollow. Prewash the shoelaces because they sometimes have a stiffening agent (sizing) present.)
- Tie the shoelaces with a string, or just make sure they do not slip off of the bulbs. (Tying the shoelaces is hard for small fingers. If the students are careful, the shoelaces will not slip off.)
- Wet one shoelace with water at room temperature. Keep the other one dry.
- Hold both thermometers while a friend vigorously fans the bulbs.
- Stop the fanning and read the temperature every two minutes. (I sometimes have the students count to a given number such as 50 as they fan.)
- Now have the students write or answer these questions:
- Does fanning a dry bulb change its temperature?
- How about fanning the wet bulb?
Results
Fanning a dry bulb does not change its temperature. (The students may see a small temperature change, but it is due to vigorous fanning and is not a true change. It goes back when the student stops fanning.) Fanning a wet bulb causes its temperature to decrease. Vigorous fanning should be kept up for about two minutes.
When water evaporates from objects, it cools them; it takes heat energy away. (A good example would be putting on a wet bathing suit; it feels cold to the skin if it is still wet and you have had it off.) Each escaping water molecule carries some heat away with it. The experiment may not work well on a humid day. On such days, when you feel sticky and uncomfortable, the difference in wet and dry bulb readings may be small, only a few degrees or so. Repeat the exercise on the first pleasant day.
Class Experiment #3
- You will need a simple elementary balance scale.
- Wet two paper towels with the same amount of water.
- Crumple one into a ball.
- Place the crumpled one on one of the pans on the balance scale.
- Leave the other paper towel flat.
- Place it on the other pan of the balance.
- Use a medicine dropper to drop water on each paper towel until the two paper towels are completely balanced.
- At the end of a half hour, which towel has lost more water?
Results
At the end of half an hour, the flat towel will weigh less than the crumpled one. Since both towels weighed the same to begin with, the flat towel has lost more water.
This is because the flat towel has a larger surface exposed directly to the air. Escaping water vapor can be carried away more easily. Students should try different types of cloths. They can do this at home with their families.
Class Experiment #4
- Put some drops of salt water on a clean glass slide.
- Leave the slide in a warm place.
- The next morning, examine the slide.
- What do you see? What does it taste like? Do you think the water took any salt with it when it evaporated?
Results
The next morning, the slide will have a glazing of salt crystals where the drops were. They will taste like salt. The water took no salt when it evaporated.
Condensation
Class Experiment #1
- Fill a shiny metal can with ice cubes. Then watch what happens on the outside of the can.
- Carefully out a thermometer inside the can, but do not use it to stir the ice. The thermometer may break.
- Take a temperature reading from the thermometer every five minutes.
Questions
- How long does it take for water droplets to appear?
- What happened to water vapor in the air that caused condensation?
- Does the ice inside the can begin to melt?
- What causes this to happen?
Results
Almost any clean metal can will do. Shininess just makes the fine condensation droplets more visible. If the day is a very dry one and droplets do not appear on the outside of the can within a reasonable time, let students gently pant their breath onto the can.
Water vapor in the air cools, loses energy on contact with the can, and so condenses into liquid water. The ice inside the can begins to melt. The ice is gaining energy, partly from the air, partly from radiation (sunlight) within the room, and partly from the molecules of water vapor condensing into liquid outside the can.
Insert a thermometer into the crushed ice. Let the students monitor it from time to time. Does the temperature of the ice-water mixture rise while the ice is melting? (No!) Have them note when it finally begins to rise. (It will rise when all of the ice is melted.) If the ice is gaining energy, shouldn't its temperature rise? (Students may or may not recall from prior learning that it takes a certain amount of energy80 calories per gramjust to melt the ice with no temperature rise. Early elementary students may not know this but older students may have learned this.)
Class Experiment #2
- Wet a paper towel and crumple it.
- Put it and a thermometer inside a jar. (A large mayonnaise jar with a lid.)
- Put the lid on the jar.
- Then lay it on its side in the sunlight. Fix it so that it won't roll. Placea thermometer outside, but next to the jar.
- After a half hour, examine the jar.
Questions
- Has any condensation occurred?
- How much cooler is it outside the jar than inside?
- Must a container be ice cold for water to condense on it?
Results
A wet sponge may be substituted for the paper towel. Place the jar so that the thermometer inside is shaded from direct sun. Shade the outside thermometer with a piece of cardboard so that it does not absorb radiant energy from the sun. If left in the sun, it will read too high. It will show its own sun-heated temperature, not air temperature.)
After half an hour, condensation will be visible on the inside of the jar. Yet it will be slightly warmer inside the jar than outside. (Heat energy has been trapped in the jar, held both by air and water vapor.) Condensation occurs because the glass of the jar, being in contact with the cooler air outside the jar, is cool enough to cause the water vapor inside to condense on it.
The container doesn't have to be ice cold for water on condense on it as we see with this jar. Ask the students if they suppose it can get foggy inside a car even if it is not winter. (Yes.) Why do they suppose it happens?
In a closed car, passengers breathe water vapor into the air of the car. Some water also evaporates from their skin. The windshield and the windows are usually cooler than the inside the car, so water will condense onto the glass as droplets of "fog."
Class Experiment #3
- Collect a drop of condensed water on a microscope slide. (You can use a medicine dropper to collect the condensation by squeezing the bulb and placing the tip of the dropper next to a drop of condensed water. It will suck into the medicine dropper tube. Then drop the drop onto the slide. Repeat several times to get a large enough sample.)
- Leave the slide in a warm place overnight. Then examine the slide with a magnifier.
Questions
- Is anything left where the drop evaporated?
- From your observation, does condensed water have anything dissolved in it?
- Would you call it pure water?
Results
On a really clean slide, condensed water should leave no visible trace. Condensed water seems to have nothing dissolved in it.
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