Earth System Science
Module: Hydrosphere
Introduction
Water blesses our planet and makes it appear beautifully blue from
space. The presence of liquid water clearly distinguishes Earth
from all the planets and moons of the solar system. In fact, water
covers almost three times as much of Earth's surface as land does.
(Sussman, p.26)
We do not just drink water; we are water. Water constitutes 50 to
90 percent of the weight of all living organisms. It is one of the
most abundant and important substances on the Earth. Water sustains
plant and animal life, plays a key role in the formation of weather,
helps to shape the surface of the planet through erosion and other
processes, and covers roughly 70% of the Earth's surface.
Water continually circulates between the Earth's surface and its
atmosphere in what is called the hydrologic cycle. The hydrologic
or water cycle, is one of the basic processes in nature. Responding
to heat from the sun and other influences, water from the oceans,
rivers, lakes, soils and vegetation evaporates into the air and
becomes water vapor. The water vapor rises into the atmosphere,
cools, and turns into liquid water or ice, forming clouds. When
the water droplets or ice crystals get large enough, they fall back
to the surface as rain or snow. Once on the ground, water does one
of three things; some of it filters into the soil and is either
absorbed by plants or percolates downward to groundwater reservoirs.
Some runs off into streams and rivers and eventually into the oceans.
Some evaporates.
The water in a lake, the snow on a mountain, the humid air or the
drop of morning dew are all part of the same system. The total annual
water loss from the surface of the planet equals the Earth's total
annual precipitation. Changing any part of the system, such as the
amount of vegetation in a region or land uses, affects the rest
of the system.
Despite its abundance, we cannot use most of Earth's water. If we
represent the Earth's water as 100 liters, 97 of them would be seawater.
Most of the remaining three would be ice. Only about 3 ml out of
the whole 100 liters would be water that we can consume; that water
is pumped from the ground or taken from fresh water, rivers and
lakes.
Water participates in many important chemical reactions, and most
substances are soluble in water. Due to its effectiveness as a solvent,
truly pure water rarely occurs in nature. Water carries many natural
and human-introduced impurities as it travels through the hydrologic
cycle. These impurities give each water its distinctive chemical
makeup, or quality. Rain and snow capture small dust particles or
aerosols from the air, and sunlight causes emissions from the burning
of gasoline and other fossil fuels to react with water to form sulfuric
and nitric acids. These pollutants return to Earth as acid rain
or snow. The acids in the water slowly dissolve rocks, placing dissolved
solids in water. Small but visible pieces of the rocks and soils
also enter the water, resulting in suspended solids and making some
waters turbid. When water percolates into the ground, it is in very
close contact with rocks and more minerals dissolve into the water.
These impurities dissolved or suspended in water determine its quality.
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