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SVHeat
1D allows vertical or horizontal heat flow models to be solved quickly and efficiently. 1D models can be created based on slices through 2D models which makes model creation quick and simple.
Boundary conditions may be
specified as constant or free-form equations of temperature or
gradients. Detailed climatic boundary conditions may also be specified.
The
finite element solution makes use of fully automatic mesh generation
and mesh refinement to solve the problem quickly as well as indicating
zones of critical gradient.
Read an independent review of our software by the Journal of Ground Water here! (PDF 75KB)
Reprinted from Ground Water with permission of the National Ground Water Association Press. Copyright 2004.
Frozen
or unfrozen analysis in saturated or unsaturated soils
Volumetric
heat capacity represented by a constant or the Newman
equation
Temperature
or flux boundary conditions may be represented as
constants or free-form equations of time or position. Climatic boundary conditions also supported