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In some specific subsurface applications which require the knowledge of subsurface temperature distributions the assumption of the Constant Areal Geothermal Temperature Profile is not valid and the problem requires a proper 3D modelling solution.
Outputs
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| Geothermal Temperature Gradient |
Inputs
| Local Calendar Time | ||||||||||||||||||
| Positioning | ||||||||||||||||||
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| Earth's Heat Flux at some reference depth
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| volumetric density of heat sources | ||||||||||||||||||
| Surface temperature based on weather reports | ||||||||||||||||||
| Subsurface Thermal Conductivity profile as function of position vector | ||||||||||||||||||
| Subsurface Thermal diffusivity profile as function of position vector |
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