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A modular three-dimensional finite-difference ground-water flow model

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TLDR
A computer program for simulating ground-water flow in three dimensions by using a block-centered finite-difference approach and has a modular structure, which permits the addition of new packages to the program without modifying existing packages.
Abstract
A computer program for simulating ground-water flow in three dimensions is presented. This report includes detailed explanations of physical and mathematical concepts on which the model is developed. Ground-water flow within the aquifer is simulated by using a block-centered finite-difference approach. The program is written in Fortran 77 and has a modular structure, which permits the addition of new packages to the program without modifying existing packages.

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Behavior of arsenic and geochemical modeling of arsenic enrichment in aqueous environments

TL;DR: In this paper, the effect of different adsorbent/As ratios, adsorption sites density, area available for adorption, pH changes and competition of As for adsorbing sites with other dissolved species such as phosphate.
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The application of satellite differential SAR interferometry-derived ground displacements in hydrogeology

TL;DR: The application of satellite differential synthetic aperture radar (SAR) interferometry, principally coherent (InSAR), and to a lesser extent, persistent-scatterer (PSI) techniques to hydrogeologic studies has improved capabilities to map, monitor, analyze, and simulate groundwater flow, aquifer-system compaction and land subsidence as discussed by the authors.
Journal ArticleDOI

Flow to a well of finite diameter in a homogeneous, anisotropic water table aquifer

TL;DR: In this article, a Laplace transform solution is presented for the problem of flow to a partially penetrating well of finite diameter in a slightly compressible water table aquifer, which allows for evaluation of both pumped well and observation piezometer data, accounts for effects of well bore storage and skin and allows for noninstantaneous release of water from the unsaturated zone.
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A computer program (MODFLOWP) for estimating parameters of a transient, three-dimensional ground-water flow model using nonlinear regression

Mary C. Hill
TL;DR: The U.S. Geological Survey MODFLOWP (pronounced MOD-FLOW*P) as discussed by the authors is a modular, three-dimensional, finite-difference, ground-water flow model (MODFLOW) which, with the new Parameter-Estimation Package (MEP) can be used to estimate parameters by nonlinear regression.
Journal ArticleDOI

Evaluation of Potential Impacts on Great Lakes Water Resources Based on Climate Scenarios of Two GCMs

TL;DR: The results of general circulation model predictions of the effects of climate change from the Canadian Centre for Climate Modeling and Analysis (model CGCM1) and the United Kingdom Meteorological Office's Hadley Centre (model HadCM2) have been used to derive potential impacts on the water resources of the Great Lakes basin this paper.
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