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Home > Environment > Water: A Fragile Resource > PROPERTIES OF WATER

 

PROPERTIES OF WATER

 

Water (H2O) is a molecule, consisting of 2 atoms of hydrogen and 1 atom of oxygen that can exist in any of three forms: solid (ice), liquid, and vapor (water vapor or steam). Water is a polar molecule; that is, one end of the molecule has a positive electrical charge, and the other end has a negative chaise. The negative (oxygen) end of one water molecule is attracted to the positive (hydro­gen) end of another water molecule, forming a hy­drogen bond between the two mol­ecules. Hydrogen bonds are the basis for a number of water's physical properties including its high melting/freezing point (Q°C, 32"F) and high boiling point UOO°C, Z12°R Because most of the Earth has a temperature between 0°C and 100°C, most water exists as the liquid on which living organisms depend.

 

Water absorbs a great deal of solar heat without its temperature rising substantially. It is this high heat capacity that allows the oceans to have a mod­erating influence on climate, particularly of coastal areas. Another consequence of water's high heat capacity is that oceans do not experience the wide temperature fluctuations that are common on land.

    Water must absorb a lot of heat before it vapor­izes, or changes from liquid to vapor. When it does evaporate, it carries the heat (called its heat of va­porization) with it. Thus, evaporating water has a cooling effect. That is why your body is cooled when perspiration evaporates from your skin.

    Water is sometimes called the "universal sol­vent," and although this is an exaggeration, many materials do dissolve in water. In nature, water is never completely pure, because it contains dis­solved gases from the atmosphere and dissolved mineral salts from the Earth. Seawater, for exam­ple, contains a variety of dissolved salts including sodium chloride, magnesium chloride, magnesium sulfate, calcium sulfate, and potassium chloride. Water's dissolving ability has a major drawback, however: many of the substances that dissolve in water also pollute it.

 

 

    Water partially obeys the general physical rule that heat expands and cold contracts. As water cools, it contracts and becomes denser until it reaches 4°C (39°F), the temperature at which it is densest. When the temperature of water falls below 4°C, however, it becomes less dense. This is why ice (at 0°C) floats on denser, slightly warmer liquid water. Because water freezes from the top down rather than from the bottom up, aquatic organism can survive beneath a frozen surface.

 

The Hydrologic Cycle

Water continuously circulates through the physical environment, from the oceans to the atmosphere to the land and back to the oceans, in a complex cycle known as the hydrologic cycle, the result is a balance among water in the oceans, water on the land, and water in the atmosphere. The cycle thus continually renews the supply of purified water on land, which is essential to terres­trial organisms.

 

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