Geophysical Modelling Geography Math Problem
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In the most common case, the conductive heat transfer can be described analytically via the general conduction equation.Firstly, we may declare the thermal conductivity of the soil layers as constant value. Indeed, if heat transfer is plane and steady, and if is not large, one can make a reasonably accurate approximation using a constant average value of Then, we may declare the density and the specific heat of the soil layers as constants and. It is necessary to note that such assumption is somewhat groundless, especially for the cases of strictly inhomogeneous soils.