Modelling of variation moisture content in the aeration zone
1990
Szulczewski, W. (Akademia Rolnicza, Wroclaw (Poland). Katedra Matematyki)
In the paper a mathematical model for the soil moisture degree variation in the layer aeration zone is presented. The hydrological processes in every layer are described by Fokker-Planck's equation while it is assumed that water soil pressure head and flow are the same on the boundary layer. This solution is obtained by using linear and secret difference scheme. An example is also presented
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