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Now showing items 1-10 of 14
Origin and distribution of soil nitrates on the Nevada Test Site
(University of Nevada, Reno, 1982)
Unusually high nitrate concentrations were found in soils of Yucca and Frenchman Flats. A maximum concentration of 11,100 mg/kg was found within the 2-6 inch soil depth on Frenchman playa. Maximum nitrate concentrations ...
A two-dimensional simulation of tritium transport in the vadose zone at the Nevada Test Site
(University of Nevada, Reno, 1990)
no abstract provided
Froth flotation of the Daisy Mine fluorite ores, Nye County, Nevada
(University of Nevada, Reno, 1965)
Batch flotation tests were conducted with samples taken from the Daisy fluorite mine to determine some of the problems facing a future flotation operation. The 8 samples selected for study were those containing fluorite ...
Tritium movement in the unsaturated zone, Nevada Test Site
(University of Nevada, Reno, 1978)
Tritum movement in three different geomorphic settings was investigated at the Nevada Test Site. Two hundred soil samples were collected from high fan, mid fan and playa sediments in Yucca and Frenchman Flats.
The hydrogeochemistry and aqueous uranium distribution of Petersen Mountain and Red Rock Valley, Washoe County, Nevada
(University of Nevada, Reno, 1983)
The chemical characteristics of water from Peterson Mountain and Red Rock Valley result from dissolution and reflect the composition of the Sierra Nevada type crystalline rocks. Background and anomalous uranium limits in ...
A new approach for simulating heat transfer and groundwater flow in the Leach Hot Springs hydrothermal system, Pershing County, Nevada
(University of Nevada, Reno, 1988)
The average spring discharge temperature at Leach Hot Springs in southern Grass Valley, Nevada is 76.8° C. Geothermal reservoir temperatures, estimated from silica and Na-K-Ca geothermometers, range from 155 ° to 176 ° C. ...
The geology of radioactive mineral occurrences near Marietta, Nevada
(University of Nevada, Reno, 1977)
Near Marietta, Nevada, uranium that originally formed in the area in connection with granitic plutonic intrusive rocks, has been exposed to the surface and is being released into the region's hydrologic cycle.
Stratigraphy, structure, geophysics, and water chemistry of the Jersey Valley area, Pershing and Lander Counties, Nevada
(University of Nevada, Reno, 1981)
The stratigraphy, structure, geophysics, and water chemistry of the Jersey Valley area have been studied. Photogeologic interpretation indicate faults forming grabens within Jersey Valley. Maximum subsurface temperature ...
Geology of the Desert Peak geothermal anomaly, Churchill County, Nevada
(University of Nevada, Reno, 1979)
Field mapping in the northern Hot Springs Mountains, Churchill County, Nevada, indicates that the intersection of Basin and Range faults with an earlier fault zone corresponds with the location of the Desert Peak Geothermal ...
Relation between surficial geology and near-surface ground-water quality, Las Vegas Valley, Nevada
(University of Nevada, Reno, 1977)
Chemical analyses of major dissolved constituents in near-surface groundwater, defined as groundwater within the upper 50 feet of alluvium, reflect general differences in surficial alluvial lithologies in Las Vegas Valley, Nevada.