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Groundwater<br />

Ocean storage<br />

18.1 Water 371<br />

Soil<br />

Rain clouds<br />

Precipitation<br />

Infiltration<br />

Groundwater to soil<br />

Precipitation<br />

Evaporation from vegetation<br />

Evaporation from lakes<br />

Surface<br />

runoff<br />

Evaporation<br />

Transpiration from trees<br />

Evaporation from streams<br />

Cloud formation<br />

Evaporation from soil<br />

Transpiration from crops<br />

Evaporation from ocean<br />

Groundwater to vegetation<br />

Groundwater to streams<br />

Groundwater to ocean<br />

Percolation<br />

Rock<br />

FIGURE 18.2 The hydrologic cycle, showing important processes and transfer of water.<br />

(Source: Modified from Council on Environment Quality and Department of State, The Global 2000<br />

Report to the President, vol. 2 [W<strong>as</strong>hington, DC].)<br />

Water can be found in either liquid, solid, or g<strong>as</strong>eous<br />

form at a number of locations at or near <strong>Earth</strong>’s surface.<br />

Depending on the specific location, the water’s residence<br />

time may vary from a few days to many thousands of years<br />

(see Table 18.1). However, <strong>as</strong> mentioned, more than 99%<br />

of <strong>Earth</strong>’s water in its natural state is unavailable or unsuitable<br />

for beneficial human use. Thus, the amount of water<br />

for which all the people, plants, and animals on <strong>Earth</strong><br />

compete is much less than 1% of the total.<br />

As the world’s population and industrial production<br />

of goods incre<strong>as</strong>e, the use of water will also accelerate. The<br />

global per capita use of water in 1975 w<strong>as</strong> about 700 m 3 /year,<br />

or 2,000 gallons/day (185,000 gal/yr), and the total human<br />

use of water w<strong>as</strong> about 3,850 km 3 /year (about 10 15<br />

gal/yr). Today, world use of water is about 6,000 km 3 /yr<br />

(about 1.58 10 15 gal/yr), which is a significant fraction<br />

of the naturally available freshwater.<br />

Compared with other resources, water is used in very<br />

large quantities. In recent years, the total m<strong>as</strong>s (or weight)<br />

of water used on <strong>Earth</strong> per year h<strong>as</strong> been approximately<br />

1,000 times the world’s total production of minerals,<br />

including petroleum, coal, metal ores, and nonmetals.<br />

Where it is abundant and readily available, water is generally<br />

a very inexpensive resource. In places where it is not<br />

abundant, such <strong>as</strong> the southwestern United States, the<br />

cost of water h<strong>as</strong> been kept artificially low by government<br />

subsidies and programs.<br />

Because the quantity and quality of water available<br />

at any particular time are highly variable, water shortages<br />

have occurred, and they will probably occur with<br />

incre<strong>as</strong>ing frequency, sometimes causing serious economic<br />

disruption and human suffering. 4 In the Middle<br />

E<strong>as</strong>t and northern Africa, scarce water h<strong>as</strong> led to harsh<br />

exchanges and threats between countries and could even<br />

lead to war. The U.S. Water Resources Council estimates<br />

that water use in the United States by the year 2020 may<br />

exceed surface-water resources by 13%. 4 Therefore, an<br />

important question is, How can we best manage our water<br />

resources, use, and treatment to maintain adequate<br />

supplies?

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