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376 CHAPTER 18 Water Supply, Use, and Management<br />

North Platte R<br />

South<br />

WYOMING<br />

P<br />

NEW<br />

MEXICO<br />

i<br />

ver<br />

latte River<br />

Arkans<strong>as</strong> River<br />

COLORADO<br />

Canadian<br />

River<br />

0 50 100 kilometers<br />

Approximate scale E-W<br />

SOUTH DAKOTA<br />

NEBRASKA<br />

Platte River<br />

KANSAS<br />

OKLAHOMA<br />

TEXAS<br />

FIGURE 18.6 Groundwater-level changes <strong>as</strong> a result of<br />

pumping in the Tex<strong>as</strong>–Oklahoma–High Plains region. (Source: U.S.<br />

Geological Survey.)<br />

the Santa Fe Trail, dried up decades ago due to pumping<br />

groundwater. It w<strong>as</strong> a symptom of what w<strong>as</strong> coming. Both<br />

Ulysses and Lubbock are now facing water shortages and will<br />

need to spend millions of dollars to find alternative sources.<br />

Desalination <strong>as</strong> a Water Source<br />

IOWA<br />

Seawater is about 3.5% salt; that means each cubic<br />

meter of seawater contains about 40 kg (88 lb) of salt.<br />

Desalination, a technology for removing salt from water,<br />

is being used at several hundred plants around the world<br />

to produce water with reduced salt. To be used <strong>as</strong> a freshwater<br />

resource, the salt content must be reduced to about<br />

0.05%. Large desalination plants produce 20,000–<br />

30,000m 3 (about 5–8 million gal) of water per day. Today,<br />

about 15,000 desalination plants in over 100 countries are<br />

in operation, and improving technology is significantly<br />

lowering the cost of desalination.<br />

Even so, desalinated water costs several times <strong>as</strong> much<br />

<strong>as</strong> traditional water supplies in the United States. Desalinated<br />

water h<strong>as</strong> a place value, which means that the price rises<br />

quickly with the transport distance and the cost of moving<br />

water from the plant. Because the various processes that remove<br />

the salt require large amounts of energy, the cost of the<br />

water is also tied to ever-incre<strong>as</strong>ing energy costs. For these<br />

Missouri R<br />

iver<br />

Water level changes from<br />

predevelopment since 1940<br />

Declines of over 15 m<br />

(50 ft)<br />

Changes between –15 m<br />

& +3 m (–50 ft and +10 ft)<br />

Rises over 3 m (10 ft)<br />

re<strong>as</strong>ons, desalination will remain an expensive process, used<br />

only when alternative water sources are not available.<br />

Desalination also h<strong>as</strong> environmental impacts.<br />

Discharge of very salty water from a desalination plant<br />

into another body of water, such <strong>as</strong> a bay, may locally incre<strong>as</strong>e<br />

salinity and kill some plants and animals. The discharge<br />

from desalination plants may also cause wide fluctuations<br />

in the salt content of local environments, which<br />

may damage ecosystems.<br />

18.3 Water Use<br />

In discussing water use, it is important to distinguish<br />

between off-stream and in-stream uses. Off-stream use<br />

refers to water removed from its source (such <strong>as</strong> a river<br />

or reservoir) for use. Much of this water is returned to<br />

the source after use; for example, the water used to cool<br />

industrial processes may go to cooling ponds and then be<br />

discharged to a river, lake, or reservoir. Consumptive use<br />

is an off-stream use in which water is consumed by plants<br />

and animals or used in industrial processes. The water enters<br />

human tissue or products or evaporates during use<br />

and is not returned to its source. 4<br />

In-stream use includes the use of rivers for navigation,<br />

hydroelectric power generation, fish and wildlife<br />

habitats, and recreation. These multiple uses usually create<br />

controversy because each requires different conditions.<br />

For example, fish and wildlife require certain water levels<br />

and flow rates for maximum biological productivity.<br />

These levels and rates will differ from those needed for<br />

hydroelectric power generation, which requires large fluctuations<br />

in discharges to match power needs. Similarly, instream<br />

uses of water for fish and wildlife will likely conflict<br />

with requirements for shipping and boating. Figure 18.7<br />

demonstrates some of these conflicting demands on<br />

a graph that shows optimal discharge for various uses<br />

River flow (Discharge)<br />

Fish and wildlife<br />

Winter Spring Summer Fall<br />

Time of Year<br />

Hydroelectric<br />

Navigation<br />

Recreation<br />

FIGURE 18.7 In-stream water uses and optimal discharge<br />

(volume of water flowing per second) for each use. Discharge is the<br />

amount of water p<strong>as</strong>sing by a particular location and is me<strong>as</strong>ured in<br />

cubic meters per second. Obviously, all these needs cannot be met<br />

simultaneously.

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