Development of a relation for steady-state pumping rate for Eagle Valley ground-water basin, Nevada

Freddy E. Arteaga; Timothy J. Durbin

doi:10.3133/ofr79261

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Development of a relation for steady-state pumping rate for Eagle Valley ground-water basin, Nevada

Freddy E. Arteaga·Timothy J. Durbin

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Abstract

Eagle Valley is a topographic and ground-water basin in the west-central area of Nevada. The demand for water in the valley is approaching the limits of the locally available resource, which is the water yield of 9,000 acre-feet per year from the adjacent mountain areas. The steady-state pumping rate from the ground-water basin is defined as the rate that just balances ground-water recharge and discharge. The recharge of water after agricultural or municipal use is a contribution toward overall ground-water recharge and, therefore, to the steady-state pumping rate. However, because the recharge factors are different for municipal and agricultural use, the total quantity of ground-water recharge from the beneficial use of water depends on the type of water use. Consequently, the steady-state pumping rate depends on the type of water use.

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Source-reported bounding extent: 39.07521443372525° to 39.308735760493846° latitude; -119.85682052039041° to -119.66639734275631° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Freddy E. Arteaga, Timothy J. Durbin. 1978. Development of a relation for steady-state pumping rate for Eagle Valley ground-water basin, Nevada. https://doi.org/10.3133/ofr79261

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