Motivation
Subsurface Temperature Profile around Lateral Flow makes adjustments to Geothermal Temperature Profile T_G(z) to account for the lateral reservoir flow with a constant temperature (see Fig. 1 and Fig. 2).
Fig. 1. Sample Subsurface Temperature Profile around a h_f height lateral flow at depth z_f with temperature T_f | Fig. 2. Sample Subsurface Temperature Profile around two lateral flows with temperature T_{f1} and T_{f2} |
Outputs
T_e(t, z) | Subsurface temperature distribution |
Inputs
t | Time lapse after the temperature step from T_e(z=0) =0 up to T_e(z=0) =T_f |
z | Spatial coordinate along the transversal direction to constant temperature T_e(z)= T_f plane z=0 |
z_f | TVDss of the top of the lateral flow unit |
h_f | True vertical thickness of the the lateral flow unit |
T_f | Boundary temperature at z=0 |
a_e | Thermal diffusivity of the surroundings |
T_G(z) | Geothermal Temperature Profile |
Equations
Driving equation | Initial conditions | Boundary conditions | ||||||||
---|---|---|---|---|---|---|---|---|---|---|
|
|
|
Solution
| ||
| ||
|
where
\mbox{erf}(x) | Error function |
See Also
Geology / Geothermal Temperature Field / Geothermal Temperature Profile
Physics / Fluid Dynamics / Linear Fluid Flow
[ Temperature Flat Source Solution @model ] [ Geothermal Temperature Profile @model ]