Saturated-Unsaturated 3D Groundwater Model. I: Development
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VIEW THE REPLYPublication: Journal of Hydrologic Engineering
Volume 10, Issue 6
Abstract
A new saturated-unsaturated three-dimensional (3D) groundwater flow model (SU3D) has been developed that calculates the pressure distribution over the entire groundwater flow domain in response to rainfall and evapotranspiration. Recent advances in solving the saturated-unsaturated groundwater flow equation are incorporated into SU3D, which solves the nonlinear, 3D, modified mixed form of the Richards equation continuously throughout the groundwater flow domain. The block-centered, finite-difference method with a variably sized grid is employed to solve the governing partial differential equation. The non-linear terms of the governing equation are linearized using a modified Picard iteration scheme, and the preconditioned conjugate gradient method is used to solve the linearized system of equations. SU3D can simulate the effects of pumping from an aquifer, and it has an option to calculate potential evapotranspiration (PET) from meteorological data. The PET is partitioned into potential evaporation and potential transpiration as a function of the leaf area index, and then the actual evaporation and transpiration are calculated. Overland flow and seepage face calculations are not included in SU3D.
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Acknowledgments
Financial support for this investigation was provided in part by Suleyman Demirel University and the U. S. Geological Survey State Water Research Institute Program. This paper represents the opinions and conclusions of the writers and does not necessarily represent the official position of Suleyman Demirel University or the U.S. Geological Survey.
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© 2005 ASCE.
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Received: Sep 30, 2002
Accepted: Jul 5, 2004
Published online: Nov 1, 2005
Published in print: Nov 2005
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