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Rate of Geothermal Temperature
| LaTeX Math Inline |
|---|
| body | --uriencoded--T_G(%7B\bf r%7D) |
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|
change along
True Vertical Direction with no account of effects of the seasonal/daily temperature variations ( which are only noticeable above
Neutral Temperature Layer ):
Ratio of ture of true vertical compnent component of the Earth heat flux to the subsurface heat conbductivityregional Earth's Heat Flux
| LaTeX Math Inline |
|---|
| body | --uriencoded--j_z(%7B\bf r%7D) |
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|
to the subsurface Thermal Conductivity | LaTeX Math Inline |
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| body | --uriencoded--\lambda_e(%7B\bf r%7D) |
|---|
|
at a certain subsurface point | LaTeX Math Inline |
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| body | --uriencoded--%7B\bf r%7D |
|---|
|
:
| LaTeX Math Block |
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|
G_T({\bf r}) = \frac{j_z({\bf r})}{\lambda_e({\bf r})} |
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