Determining the unsaturated zone percolation rate, or flux, is an extremely important site characterization issue for the proposed Yucca Mountain nuclear waste repository. A new technique that measures the {sup 36}Cl content of tuff from the Exploratory Shaft will be used to calculate flux through the unsaturated zone over longer times than could be measured by the more conventional {sup 14}C method. Measurements of the {sup 36}Cl "bomb pulse" in soil samples from Yucca Mountain have been used to confirm that infiltration is not an important recharge mechanism. 5 refs., 3 figs
The water movement tracer test is designed to produce information derived from isotopic measurements...
The unsaturated zone at Yucca Mountain, Nevada, is being investigated as a potential location for a ...
The amount, spatial distribution, and velocity of water percolating through the unsaturated zone (UZ...
The rates of water movements in the tuffs at Yucca Mountain are important for assessing the performa...
Defining the spatial distribution and timing of subsurface fluid percolation is one of the most impo...
Measurements of chloride and {sup 36}Cl in soils from two locations near Yucca Mountain, Nevada, hav...
Development and testing of conceptual flow and transport models for hydrologic systems are strengthe...
Chlorine-36, including the natural cosmogenic component and the component produced during atmospheri...
The Nevada Nuclear Waste Storage Investigations Project of the US Department of Energy provides that...
Previous studies by scientists at Los Alamos National Laboratory (LANL) found elevated ratios of chl...
Measurements of {sup 36}Cl in cuttings from a borehole that was drilled 387 m into unsaturated tuffs...
Previous studies Los Alamos National Laboratory (LANL) found elevated ratios of chlorine-36 to total...
This document is an end-of-contract report, prepared by Hydro Geo Chem for Los Alamos National Labor...
A surface-based borehole investigation currently (1989) is being done to characterize liquid-water p...
Unsaturated tuff beneath Yucca Mountain, Nevada, is being evaluated by the US Department of Energy a...
The water movement tracer test is designed to produce information derived from isotopic measurements...
The unsaturated zone at Yucca Mountain, Nevada, is being investigated as a potential location for a ...
The amount, spatial distribution, and velocity of water percolating through the unsaturated zone (UZ...
The rates of water movements in the tuffs at Yucca Mountain are important for assessing the performa...
Defining the spatial distribution and timing of subsurface fluid percolation is one of the most impo...
Measurements of chloride and {sup 36}Cl in soils from two locations near Yucca Mountain, Nevada, hav...
Development and testing of conceptual flow and transport models for hydrologic systems are strengthe...
Chlorine-36, including the natural cosmogenic component and the component produced during atmospheri...
The Nevada Nuclear Waste Storage Investigations Project of the US Department of Energy provides that...
Previous studies by scientists at Los Alamos National Laboratory (LANL) found elevated ratios of chl...
Measurements of {sup 36}Cl in cuttings from a borehole that was drilled 387 m into unsaturated tuffs...
Previous studies Los Alamos National Laboratory (LANL) found elevated ratios of chlorine-36 to total...
This document is an end-of-contract report, prepared by Hydro Geo Chem for Los Alamos National Labor...
A surface-based borehole investigation currently (1989) is being done to characterize liquid-water p...
Unsaturated tuff beneath Yucca Mountain, Nevada, is being evaluated by the US Department of Energy a...
The water movement tracer test is designed to produce information derived from isotopic measurements...
The unsaturated zone at Yucca Mountain, Nevada, is being investigated as a potential location for a ...
The amount, spatial distribution, and velocity of water percolating through the unsaturated zone (UZ...