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Ground Water Atlas of the United States - Segment 1 California Nevada


Fresh Ground-Water use and management

During the early years of ground-water development in the coastal basins, from the 1850's to early 1900's, the principal use of water was for irrigated agriculture. Although agricultural ground-water use remains substantial, urbanization has gradually replaced most agricultural land in the larger basins and the greatest collective ground-water demand is now for public supply. The largest water users are cities and suburbs from San Francisco southward, but because of the unequal distribution of rainfall, most of the freshwater is in northern California. Accordingly, it has become necessary to regulate streamflow and import water into many coastal basins from the Sierra Nevada, the Colorado River, the Owens Valley, and northern California through an extensive system of aqueducts.

For many years, rapidly growing populations in several basins resulted in ground-water withdrawals that exceeded natural recharge on a long-term basis; this led to marked water-level declines. The consequences of these excessive withdrawals ranged from mild, such as increased pumping costs, to severe, such as land subsidence and seawater intrusion. Today (1995), ground water in the coastal basins of California is carefully managed. The current supply of water from all sources, including imported water, approximately balances demand. However, because the natural recharge to many basins, especially southward from the San Francisco Bay area, is far less than the volume of ground water currently (1995) withdrawn, increases in population will require either additional imports, more conservation, an increase in the amount of water now reclaimed, or a combination of all three. More than any other environmental factor, water availability will likely determine the size of the population these basins can support.


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