Motivation
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
T_G(t, {\bf r}) | |
G_T({\bf r}) | Geothermal Temperature Gradient |
Inputs
t | Local Calendar Time |
{\bf r} | Position vector |
z(l) | |
{\bf j}(x,y, z = z_{ref}) | Earth's Heat Flux at some reference depth z = z_{ref} as function of (x, \, y) |
q({\bf r}) | Volumetric density of heat sources distributed throughout the subsurface rock volume |
T_s(t, x, y) | Surface temperature based on weather reports |
\lambda_e({\bf r}) | Subsurface Thermal Conductivity profile as function of position vector |
a_{e}({\bf r}) | Subsurface Thermal diffusivity profile as function of position vector |
where
l | Measured Depth of wellbore trajectory with reference to Earth's surface ( l=0) |
z_s = z(l=0) |
Assumptions
Equations
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See Also
Geology / Geothermal Temperature Field
[ Constant Areal Geothermal Temperature Profile @model ] [ Geothermal Temperature Gradient ]