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As an alternative, we also incorporated the hysteresis model of Lenhard et al. [1991] and Lenhard and Parker [1992], which eliminates pumping by keeping track of historical reversal points, into HYDRUS. HYDRUS also implements a scaling procedure to approximate hydraulic variability in a given soil profile by means of a set of linear scaling transformations that relate the individual soil hydraulic characteristics to those of a reference soil.
Examples of water flow simulations in simple and complex (Mallants et al., 1999) capillary barriers. Download now (3.4 MB)
Grignon Numerical analysis of water and solute transport in a cultivated silt loam soil (heterogeneity generated by farming practices) (Coquet et al., 2005).
Values in the Time-variable boundary conditions dialog were not updated correctly under
certain circumstances
Ae is printed into the new binary output
file AWIArea.out in 2D and 3D.
3. The PFAS computational modules can display the air-water interfacial area under Results.
4. Users can display solute concentrations on the air-water interfacial area in the HYDRUS GUI
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