The finite element model developed in Part I is verified against field data and the results are compared with those obtained from a one-dimensional finite difference model. Two field examples are given: vertical flow in a clay soil with red cabbage, and two-dimensional flow in a complex layered and anisotropic situation. The results indicate that the finite element model is well suited for the treatment of complex and realistic field problems.
|Original language||English (US)|
|Title of host publication||Proc Soil Sci Soc Am|
|Number of pages||7|
|Publication status||Published - Mar 1975|
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