Add to ORKGThe 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
Determining the unsaturated zone percolation rate, or flux, is an extremely important site character...
This paper presents a large-scale modeling study characterizing fluid flow and tracer transport in ...
In support of pacific Northwest Laboratory`s (PNL) preliminary total system performance assessment o...
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...
A comprehensive geochemical/geophysical model incorporates the current and relevant stratigraphic, p...
Defining the spatial distribution and timing of subsurface fluid percolation is one of the most impo...
A three-dimensional site-scale numerical model has been developed to simulate water and gas flow, he...
Characterizing percolation patterns in unsaturated zones has posed a greater challenge to numerical...
The rates of water movements in the tuffs at Yucca Mountain are important for assessing the performa...
To investigate the coupled processes involved in fluid and heat flow and chemical transport in the ...
Chlorine-36, including the natural cosmogenic component and the component produced during atmospheri...
This report, prepared by Hydro Geo Chem staff for Los Alamos National Laboratory, summarizes work co...
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...
Determining the unsaturated zone percolation rate, or flux, is an extremely important site character...
This paper presents a large-scale modeling study characterizing fluid flow and tracer transport in ...
In support of pacific Northwest Laboratory`s (PNL) preliminary total system performance assessment o...
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...
A comprehensive geochemical/geophysical model incorporates the current and relevant stratigraphic, p...
Defining the spatial distribution and timing of subsurface fluid percolation is one of the most impo...
A three-dimensional site-scale numerical model has been developed to simulate water and gas flow, he...
Characterizing percolation patterns in unsaturated zones has posed a greater challenge to numerical...
The rates of water movements in the tuffs at Yucca Mountain are important for assessing the performa...
To investigate the coupled processes involved in fluid and heat flow and chemical transport in the ...
Chlorine-36, including the natural cosmogenic component and the component produced during atmospheri...
This report, prepared by Hydro Geo Chem staff for Los Alamos National Laboratory, summarizes work co...
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...
Determining the unsaturated zone percolation rate, or flux, is an extremely important site character...
This paper presents a large-scale modeling study characterizing fluid flow and tracer transport in ...
In support of pacific Northwest Laboratory`s (PNL) preliminary total system performance assessment o...