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The resulting equations are solved in an iterative fashion, by linearization and subsequent Gaussian elimination for banded matrices, a conjugate gradient method for symmetric matrices, or the ORTHOMIN method for asymmetric matrices.
Added support for 4K monitors (high-dpi resolution)
Improved graphical tools “Slicer” and “Clipper”
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 demonstrating new system-dependent boundary conditions in HYDRUS, such as a specified gradient , a subsurface drip with the characteristic function, and a surface drip with dynamic evaluation of a wetting area.
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