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Home > Society and Social Sciences > Politics and government > Assessing Potential Effects of Changes in Water Use with a Numerical Groundwater-Flow Model of Carson Valley, Douglas County, Nevada, and Alpine County, California: Usgs Scientific Investigations Report 2012-5262
Assessing Potential Effects of Changes in Water Use with a Numerical Groundwater-Flow Model of Carson Valley, Douglas County, Nevada, and Alpine County, California: Usgs Scientific Investigations Report 2012-5262

Assessing Potential Effects of Changes in Water Use with a Numerical Groundwater-Flow Model of Carson Valley, Douglas County, Nevada, and Alpine County, California: Usgs Scientific Investigations Report 2012-5262


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About the Book

Rapid growth and development within Carson Valley in Douglas County, Nevada, and Alpine County, California, has caused concern over the continued availability of groundwater, and whether the increased municipal demand could either impact the availability of water or result in decreased flow in the Carson River. Annual pumpage of groundwater has increased from less than 10,000 acre feet per year (acre-ft/yr) in the 1970s to about 31,000 acre-ft/yr in 2004, with most of the water used in agriculture. Municipal use of groundwater totaled about 10,000 acre-feet in 2000. In comparison, average streamflow entering the valley from 1940 to 2006 was 344,100 acre-ft/yr, while average flow exiting the valley was 297,400 acre-ft/yr. Carson Valley is underlain by semi-consolidated Tertiary sediments that are exposed on the eastern side and dip westward. Quaternary fluvial and alluvial deposits overlie the Tertiary sediments in the center and western side of the valley. The hydrology of Carson Valley is dominated by the Carson River, which supplies irrigation water for about 39,000 acres of farmland and maintains the water table less than 5 feet (ft) beneath much of the valley floor. Perennial and ephemeral watersheds drain the Carson Range and the Pine Nut Mountains, and mountain-front recharge to the groundwater system from these watersheds is estimated to average 36,000 acre-ft/yr. Groundwater in Carson Valley flows toward the Carson River and north toward the outlet of the Carson Valley. An upward hydraulic gradient exists over much of the valley, and artesian wells flow at land surface in some areas. Water levels declined as much as 15 ft since 1980 in some areas on the eastern side of the valley. Median estimated transmissivities of Quaternary alluvial-fan and fluvial sediments, and Tertiary sediments are 316; 3,120; and 110 feet squared per day (ft2/d), respectively, with larger transmissivity values in the central part of the valley and smaller values near the valley margins. A groundwater-flow model of Quaternary and Tertiary sediments in Carson Valley was developed using MODFLOW and calibrated to simulate historical conditions from water years 1971 through 2005.


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Product Details
  • ISBN-13: 9781288883868
  • Publisher: Bibliogov
  • Publisher Imprint: Bibliogov
  • Height: 246 mm
  • Sub Title: Usgs Scientific Investigations Report 2012-5262
  • Width: 189 mm
  • ISBN-10: 1288883862
  • Publisher Date: 01 Mar 2013
  • Binding: Paperback
  • Spine Width: 5 mm
  • Weight: 195 gr


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Assessing Potential Effects of Changes in Water Use with a Numerical Groundwater-Flow Model of Carson Valley, Douglas County, Nevada, and Alpine County, California: Usgs Scientific Investigations Report 2012-5262
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