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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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GWM-a ground-water management process for the U.S. Geological Survey modular ground-water model (MODFLOW-2000)

TL;DR: In this paper, the authors present a survey of the state-of-the-art tools and techniques used in the construction of a bridge in the city of New Orleans, Louisiana.
Journal ArticleDOI

Estimate of recharge from radiocarbon dating of groundwater and numerical flow and transport modeling

Chen Zhu
TL;DR: In this paper, the authors combine radiocarbon age and hydraulic data to estimate recharge to a regional groundwater aquifer using a linked numerical 14C transport and flow model while hydraulic conductivity values are proportionally adjusted to match observed heads.
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A method of converting no-flow cells to variable-head cells for the U. S. Geological Survey modular finite-difference ground-water flow model

TL;DR: The U.S. Geological Survey Modular Ground-Water Flow Model (MODFLOW) as mentioned in this paper simulates ground-water flow through porous media using the finite-difference method.
Journal ArticleDOI

A Wetland Simulation Module for the MODFLOW Ground Water Model

TL;DR: In this article, the authors developed a computer package for the widely used MOD-FLOW code that would simulate three-dimensional wetland flow hydroperiods and wetland interactions with aquifers and slough channels.
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