Matter is anything that takes up space, and is what makes up everything that we see. Solids, liquids and gases are three states of matter. A solid has both a fixed volume and fixed shape. A liquidtakes the shape of whatever container that it is in, but has a fixed volume. Gases, however, do not have a fixed volume—they spread out to take up space, like in a balloon.
Students should recognize examples of transitions between states of matter and the role of heat energy in causing them. Adding heat energy can convert a solid to a liquid, or a liquid to a gas. Removing heat energy can turn a gas to a liquid, or a liquid to a solid. The condensation in the ice water demonstration provides a visual example, as the cold glass condenses water vapor (gas) from the air to form liquid water on the outside of the glass.
Air is a fascinating gas. Every breath we take (~1 liter) has 1022molecules of air! That is about as many stars as exist in the universe. Interestingly, if you could make a box with sides the width of a human hair, it could still have trillions of air molecules inside. However, these air molecules are so small that air appears “invisible” to the naked eye. Air molecules do scatter light, especially at blue wavelengths, which gives the sky its color. Particles suspended in the air can both scatter and absorb light, creating a hazy appearance when the air is polluted (Figure 1).
Credit: http://www.jpl.nasa.gov/news/features.cfm?feature=423
The air around the Earth is called the atmosphere. Viewed from space (Figure 2), we see that the atmosphere is very thin compared to the Earth overall. However, the atmosphere is vitally important to life on Earth. It contains the air that animals breathe and that plants use for photosynthesis; absorbs UV radiation; regulates the planet’s temperature; blocks meteors from crashing onto our surface; and is where weather occurs.
The mass of the atmosphere (about 1.1×1019 pounds, or 5.1×1018 kilograms) can best be understood by considering atmospheric pressure, which is the pressure exerted by the weight of the atmosphere above a given point. Atmospheric pressure averages 14.7 psi (pounds per square inch) at sea level. This means that if you drew a square one inch wide and one inch long on the Earth’s surface, the column of air rising above that square into space would weigh 14.7 pounds! The higher you travel in the atmosphere, the lower the density of air, but there is no definite boundary where the atmosphere ends and outer space begins.
Credit: http://www.adventures.com.sg/