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A Fragile Resource
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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.
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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. |
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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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