VZJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Mansell, R. S.
Right arrow Articles by Bloom, S. A.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Mansell, R. S.
Right arrow Articles by Bloom, S. A.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Mansell, R. S.
Right arrow Articles by Bloom, S. A.
Related Collections
Right arrow Vadose Zone Processes and Chemical Transport
Right arrow Soil Models
Right arrow Soil Hydrology
Vadose Zone Journal 1:222-238 (2002)
© 2002 Soil Science Society of America

Reviews and Analyses

Adaptive Grid Refinement in Numerical Models for Water Flow and Chemical Transport in Soil

A Review

R. S. Mansell*,a, Liwang Mab, L. R. Ahujab and S. A. Blooma

a Soil and Water Science Department, University of Florida, 2169 McCarty Hall, Gainesville, FL 32611-0290
b USDA-ARS-NA-GPSR, 301 South Howes Street, Fort Collins, CO 80521

* Corresponding author (rsm{at}mail.ifas.ufl.edu)

Received 26 December 2001.

Insufficient spatial or temporal resolution is a common source of errors in numerical solutions for both water flow and solute transport in the variably unsaturated vadose zone. Evaporation near the surface, as well as infiltration into initially dry soil profiles, typically create mobile local regions with large gradients of the pressure head. Convection-dominant transport of solutes during water flow in soil also tends to create steep moving fronts of concentration with large localized concentration gradients. Groundwater flow and solute transport in highly heterogeneous aquifers similarly tend to be preferentially channeled through regions of high flow rates. Without due consideration of special resolution requirements for such critical cases of flow and transport, simulations using traditional finite difference (FDM) and finite element (FEM) numerical methods typically provide inaccurate solutions characterized by undesirable features such as oscillation and numerical dispersion. Incorporation of local adaptive grid refinement (LAGR) algorithms in numerical models for solving such cases is an effective approach that has been used to provide accurate numerical approximations by automated adjustment of local spatial resolution. Local error estimates are typically utilized to optimize spatial resolution. Definite advantages, as well as some limitations, exist for using LAGR algorithms in FDM and FEM numerical models for flow and transport in soils.

Abbreviations: CPU, central processing unit • CVFEM, control volume finite element numerical method • FCT, flux-corrected transport • FDM, finite difference method • FEM, finite element method • LAGR, local adaptive grid refinement • LEM, Lagrangian-Eulerian method • LUGR, local-uniform-grid refinement • MMOC, modified method of characteristics • MSRPT, modified single-step reverse particle tracking • PDE, partial differential equation • SRPT, single-step reverse particle tracking




This article has been cited by other articles:


Home page
Vadose Zone JHome page
B. Belfort and F. Lehmann
Comparison of Equivalent Conductivities for Numerical Simulation of One-Dimensional Unsaturated Flow
Vadose Zone J., November 11, 2005; 4(4): 1191 - 1200.
[Abstract] [Full Text] [PDF]


Home page
Vadose Zone JHome page
B. Brunone, B. Brunone, M. Ferrante, N. Romano, and A. Santini
Numerical Simulations of One-Dimensional Infiltration into Layered Soils with the Richards Equation Using Different Estimates of the Interlayer Conductivity
Vadose Zone J., May 1, 2003; 2(2): 193 - 200.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Soil Science Society of America Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2002 by the Soil Science Society of America.