This analysis is designed to use existing modeling and analysis results as the basis for estimated groundwater flow rates into the saturated zone (SZ) site-scale model domains, both as recharge (infiltration) at the upper boundary (water table), and as underflow at the lateral boundaries. Specifically, this work compiles information on the recharge boundary conditions supplied to the base-case and alternate SZ site-scale flow models taken from (1) distributed recharge from the 1997 (D'Agnese et al. 1997 [DIRS 100131]) or 2001 (D'Agnese et al. 2002 [DIRS 158876]) SZ regional-scale (Death Valley Regional Flow System [DVRFS]) model; (2) recharge below the area of the 1997 (Wu et al. 1997 [DIRS 156453]) or 2003 (BSC 2004 [DIRS 169861]) unsatura...
This manual documents two computer programs. The first is a finite difference ground-water flow mode...
Estimating the quantity of water that reaches the water table following an infiltration event is vit...
Better representations of groundwater processes need to be incorporated into large-scale hydrologica...
Groundwater recharge is the main forcing of regional groundwater flow. In traditional partial‐differ...
The purpose of the flow calibration analysis work is to provide Performance Assessment (PA) with the...
A calibrated groundwater flow model for a contaminated site can provide substantial information for ...
The purpose of this report is to document the 19-unit, hydrogeologic framework model (19-layer versi...
Abstract Recharge is a fundamental component of groundwater systems, and in groundwater-modeling exe...
This Analysis/Model Report (AMR) documents an updated analysis of water-level data performed to prov...
An analysis of recharge, i.e. the quantity of water that infiltrates from the land surface to the a...
The City of Tucson plans to construct a groundwater recharge and recovery facility in southern Avra ...
The quantification of groundwater recharge is an important but challenging task in groundwater flow ...
Groundwater recharge rates calculated with the GROWA model have been applied as the recharge boundar...
A conceptual model was established to study the patterns of flow in vadose and saturated zones syste...
The accurate estimation of groundwater recharge is the key and a necessity for sustainable use of gr...
This manual documents two computer programs. The first is a finite difference ground-water flow mode...
Estimating the quantity of water that reaches the water table following an infiltration event is vit...
Better representations of groundwater processes need to be incorporated into large-scale hydrologica...
Groundwater recharge is the main forcing of regional groundwater flow. In traditional partial‐differ...
The purpose of the flow calibration analysis work is to provide Performance Assessment (PA) with the...
A calibrated groundwater flow model for a contaminated site can provide substantial information for ...
The purpose of this report is to document the 19-unit, hydrogeologic framework model (19-layer versi...
Abstract Recharge is a fundamental component of groundwater systems, and in groundwater-modeling exe...
This Analysis/Model Report (AMR) documents an updated analysis of water-level data performed to prov...
An analysis of recharge, i.e. the quantity of water that infiltrates from the land surface to the a...
The City of Tucson plans to construct a groundwater recharge and recovery facility in southern Avra ...
The quantification of groundwater recharge is an important but challenging task in groundwater flow ...
Groundwater recharge rates calculated with the GROWA model have been applied as the recharge boundar...
A conceptual model was established to study the patterns of flow in vadose and saturated zones syste...
The accurate estimation of groundwater recharge is the key and a necessity for sustainable use of gr...
This manual documents two computer programs. The first is a finite difference ground-water flow mode...
Estimating the quantity of water that reaches the water table following an infiltration event is vit...
Better representations of groundwater processes need to be incorporated into large-scale hydrologica...