Some effects of linearizing the unsaturated soil moisture transfer diffusivity model
Author:
Publisher
American Geophysical Union (AGU)
Subject
Water Science and Technology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1029/WR016i004p00643/fullpdf
Reference11 articles.
1. Solution of vertical unsaturated flow of soil water;Bruch;Soil Sci.,1974
2. Galerkin methods for parabolic equations;Douglas;SIAM J. Numer. Anal.,1970
3. A coupled heat and moisture transport model for Arctic soils;Guymon;Water Resour. Res.,1974
4. Study of relative efficiency of finite difference Galerkin techniques for modeling soil water transfer;Hayhoe;Water Resour. Res.,1978
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2. Lumped versus distributed mass matrices in the finite element solution of subsurface flow;Water Resources Research;1990-05
3. Mass lumping models of the linear diffusion equation;Advances in Water Resources;1983-06
4. Unsaturated soil water flow;Reviews of Geophysics;1983
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