The isotopic ratios of {sup 36}Cl/Cl are used in conjunction with geologic interpretation and numerical modeling to evaluate flow and transport pathways, processes, and model parameters in the unsaturated zone at Yucca Mountain. By synthesizing geochemical and geologic data, the numerical model results provide insight into the validity of alternative hydrologic parameter sets, flow and transport processes in and away from fault zones, and the applicability of {sup 36}Cl/Cl ratios for evaluating alternative conceptual models
The purpose of this Analysis/Model Report (AMR) is to document natural and anthropogenic (human-indu...
This paper presents a large-scale modeling study characterizing fluid flow and tracer transport in ...
A three-dimensional site-scale numerical model has been developed to simulate water and gas flow, he...
The isotopic ratios of {sup 36}Cl/Cl are used in conjunction with geologic interpretation and numeri...
Development and testing of conceptual flow and transport models for hydrologic systems are strengthe...
Defining the spatial distribution and timing of subsurface fluid percolation is one of the most impo...
A comprehensive geochemical/geophysical model incorporates the current and relevant stratigraphic, p...
The rates of water movements in the tuffs at Yucca Mountain are important for assessing the performa...
Characterizing percolation patterns in unsaturated zones has posed a greater challenge to numerical...
A three-dimensional site-scale numerical model has been developed to simulate water and gas flow, he...
To investigate the coupled processes involved in fluid and heat flow and chemical transport in the ...
This report, prepared by Hydro Geo Chem staff for Los Alamos National Laboratory, summarizes work co...
Chlorine-36, including the natural cosmogenic component and the component produced during atmospheri...
Determining the unsaturated zone percolation rate, or flux, is an extremely important site character...
Even with the significant progress made in modeling flow and transport in fractured rock in the last...
The purpose of this Analysis/Model Report (AMR) is to document natural and anthropogenic (human-indu...
This paper presents a large-scale modeling study characterizing fluid flow and tracer transport in ...
A three-dimensional site-scale numerical model has been developed to simulate water and gas flow, he...
The isotopic ratios of {sup 36}Cl/Cl are used in conjunction with geologic interpretation and numeri...
Development and testing of conceptual flow and transport models for hydrologic systems are strengthe...
Defining the spatial distribution and timing of subsurface fluid percolation is one of the most impo...
A comprehensive geochemical/geophysical model incorporates the current and relevant stratigraphic, p...
The rates of water movements in the tuffs at Yucca Mountain are important for assessing the performa...
Characterizing percolation patterns in unsaturated zones has posed a greater challenge to numerical...
A three-dimensional site-scale numerical model has been developed to simulate water and gas flow, he...
To investigate the coupled processes involved in fluid and heat flow and chemical transport in the ...
This report, prepared by Hydro Geo Chem staff for Los Alamos National Laboratory, summarizes work co...
Chlorine-36, including the natural cosmogenic component and the component produced during atmospheri...
Determining the unsaturated zone percolation rate, or flux, is an extremely important site character...
Even with the significant progress made in modeling flow and transport in fractured rock in the last...
The purpose of this Analysis/Model Report (AMR) is to document natural and anthropogenic (human-indu...
This paper presents a large-scale modeling study characterizing fluid flow and tracer transport in ...
A three-dimensional site-scale numerical model has been developed to simulate water and gas flow, he...