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Rate of Geothermal Temperature 

LaTeX Math Inline
body--uriencoded--T_G(%7B\bf r%7D)
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 vertical compnent of the Earth heat flux to the subsurface heat conbductivity:

LaTeX Math Block
anchorGT
alignmentleft
G_T({\bf r}) = \frac{j_z({\bf r})}{\lambda_e({\bf r})}

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[ Geothermal Temperature Gradient (GradT) ] [  Geothermal Temperature Profile (TG) ]