Many sunny, arid regions are good for growing crops as long as water can be added. Some of the increase in productivity is due to farming in regions that are technically too dry. Groundwater can be used to make the desert bloom, but at what cost? And for how long? Eventually the wells will run dry.
Some aquifers are overused; people pump out more water than is replaced. As the water is pumped out, the water table slowly falls, requiring wells to be dug deeper, which takes more money and energy. Wells may go completely dry if they are not deep enough to reach into the lowered water table.
Intense drought has reduced groundwater levels in the southern U.S., particularly in Texas and New Mexico.
Other problems may stem from groundwater overuse. Subsidence and saltwater intrusion are two of them.
The Ogallala Aquifer supplies about one-third of the irrigation water in the United States. The Ogallala Aquifer is widely used by people for municipal and agricultural needs. (Figure below). The aquifer is found from 30 to 100 meters deep over an area of about 440,000 square kilometers!
The Ogallala Aquifer is found beneath eight states and is heavily used.
The water in the aquifer is mostly from the last ice age. About eight times more water is taken from the Ogallala Aquifer each year than is replenished. Much of the water is used for irrigation (Figure below).
Farms in Kansas use central pivot irrigation, which is more efficient since water falls directly on the crops instead of being shot in the air. These fields are between 800 and 1600 meters (0.5 and 1 mile) in diameter.
Lowering the water table may cause the ground surface to sink. Subsidence may occur beneath houses and other structures (Figure below).
The San Joaquin Valley of California is one of the world’s major agricultural areas. So much groundwater has been pumped that the land has subsided many tens of feet.
When coastal aquifers are overused, salt water from the ocean may enter the aquifer, contaminating the aquifer and making it less useful for drinking and irrigation. Salt water incursion is a problem in developed coastal regions, such as on Hawaii.
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| Credit: Courtesy of the US Geological Survey Source: http://commons.wikimedia.org/wiki/File:Gwsanjoaquin.jpg License: Public Domain | ||
| Credit: Courtesy of Chris Poulsen, National Drought Mitigation Center at the University of Nebraska-Lincoln, NASA Goddard Space Flight Center, and the GRACE science team Source: http://earthobservatory.nasa.gov/IOTD/view.php?id=76575 License: Public Domain | ||
| Credit: Courtesy of the US Geological Survey Source: http://ne.water.usgs.gov/ogw/hpwlms/physsett.html License: Public Domain | ||
| Credit: Courtesy of NASA/GSFC/METI/ERSDAC/JAROS and US/Japan ASTER Science Team Source: http://earthobservatory.nasa.gov/IOTD/view.php?id=5772 License: Public Domain | ||
| Credit: Courtesy of the US Geological Survey Source: http://commons.wikimedia.org/wiki/File:Gwsanjoaquin.jpg License: Public Domain |
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