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A finite-volume ELLAM for three-dimensional solute-transport modeling
Thomas F Russell1, Caroline I Heberton, Leonard F Konikow
1University of Colorado at Denver, Department of Mathematics, P.O. Box 173364, Campus Box 170, Denver, CO 80217-3364, USA. trussell@carbon.cudenver.edu
Ground Water
|March 27, 2003
Summary
A new three-dimensional finite-volume ELLAM (FVELLAM) method enhances ground water modeling. This method accurately simulates solute transport, even with large time steps, improving simulations in complex flow systems.
Area of Science:
- Environmental Science
- Hydrogeology
- Computational Science
Background:
- Ground water modeling is crucial for understanding solute transport.
- Existing methods may face limitations with advection-dominated systems.
- Accurate simulation of solute transport is essential for environmental management.
Purpose of the Study:
- To develop and implement a novel three-dimensional finite-volume ELLAM (FVELLAM) method.
- To integrate the FVELLAM as a solver option within the U.S. Geological Survey's (USGS) MODFLOW-2000.
- To evaluate the FVELLAM's performance in simulating ground water solute transport.
Main Methods:
- The FVELLAM method uses space-time finite volumes aligned with flow streamlines.
- It solves an integral form of the solute-transport equation, combining mass conservation with Eulerian-Lagrangian advantages.
- Implicit time discretization for dispersion and source/sink terms is coupled with Lagrangian advection tracking.
Main Results:
- The FVELLAM code successfully simulates advective transport, dispersion, mixing, retardation, and decay of solutes.
- It allows for large transport time increments (Courant numbers) and accurate results in advection-dominated systems (Peclet numbers).
- Testing against analytical solutions and other numerical codes shows excellent results, often with minimal time steps.
Conclusions:
- The FVELLAM method provides an effective and accurate approach for ground water solute transport simulation.
- Its implementation in MODFLOW-2000 expands the capabilities for ground water flow and transport modeling.
- The method's efficiency in handling advection-dominated systems makes it valuable for various hydrogeological applications.