Hydrochemical and 14C constraints on groundwater recharge and interbasin flow in an arid watershed: Tule Desert, Nevada

Author:

Hagedorn Benjamin

Funder

Vidler Water Company

California State University

Publisher

Elsevier BV

Subject

Water Science and Technology

Reference75 articles.

1. Groundwater residence time and paleorecharge conditions in the deep confined aquifers of the coastal watershed, South East Tanzania;Bakari;J. Hydrol.,2012

2. Bateman, R.L., 1976. Inventory and Chemical Quality of Groundwater in White River – Muddy River – Meadow Valley Wash Area, Southeastern Nevada. Desert Research Institute Project Report No. 40, 44 pp.

3. Belcher, W.R., Elliot, P.E., Geldon, A.L., 2001. Hydraulic-Property Estimates for Use With a Transient Ground Water Flow Model of the Death Valley Regional Ground-Water Flow System, Nevada and California. USGS Water-Resources Investigations Report 01-4120, 28 pp.

4. Stable isotopes in precipitation and groundwater in the Yucca Mt. region, Southern Nevada;Benson,1989

5. Berger, D.L., 1992. Lithologic Properties of Carbonate-Rock Aquifers at Five Test Wells in the Coyote Spring Valley area, Southern Nevada, as Determined from Geophysical Logs. U.S. Geological Survey Water-Resources Investigations Report 91-4167, 27 pp.

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