Upward vertical heat conduction from Earth's Centre towards Earth's surface leading to a static geothermal profile
See Also
Synonym: Geothermal Temperature Profile = Geotherma
Natural subsurface temperature profile along the True Vertical Direction:
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It is essentially a true vertical component of local Geothermal Temperature Field
. LaTeX Math Inline body T_G(x, \, y, \, z)
Many subsurface studies are focused on Sedimentary Cover below a specific surface area where lateral
variation of Geothermal Temperature Field LaTeX Math Inline body --uriencoded--\%7B x, \, y \%7D
maybe insignificant comparing to variation along the true vertical direction LaTeX Math Inline body T_G(x, \, y, \, z)
. LaTeX Math Inline body --uriencoded--\%7B z \%7D
This happens, for example, at the lateral scales of a typical Petroleum Field and allows modelling Geothermal Temperature Field with a laterally constant Geothermal Temperature Profile
. LaTeX Math Inline body T_G(z)
The high level overview of the Earth's Geothermal Temperature Profile is brought at Fig 1.
The zoomed picture of a typical Geothermal Temperature Profile in Sedimentary Cover of the Earth's Crust is brought at Fig 2.
Fig. 1. Schematic picture of Geothermal Temperature Profile of the Earth. | Fig. 2. A sample of Geothermal Temperature Gradient in Sedimentary Cover of the Earth's Crust. |
Impact from Surface Temperature Variations
The surface temperature variations penetrate the Sedimentary Cover all the way down to the Neutral Temperature Layer (NTL) (see Fig. 3) which varies from few meters to few dozens of meters.
Fig. 3.1. A sample of Geothermal Temperature Profile captured at a certain time moment when surface temperature was higher than annual average. | Fig. 3.2. A sample of Geothermal Temperature Profile with depth zoom around temperature variations above Neutral Temperature Layer captured at a certain time moment when surface temperature was higher than annual average but lower than monthly average. |
Fig. 3.3. A sample of Geothermal Temperature Profile captured at different time moments. | Fig. 3.4. A sample of Geothermal Temperature Profile captured at different time moments with zoom around temperature variations above Neutral Temperature Layer |
An imaginary subsurface temperature profile under assumption of the constant surface temperature
is called Unbiased Geothermal Temperature Profile LaTeX Math Inline body T_s(t) = \rm const
(see Fig. 4). LaTeX Math Inline body --uriencoded--T_%7BGN%7D(z)
Fig. 4. A typical example of Geothermal Temperature Profile (TG) and Unbiased Geothermal Temperature Profile (TGN) |
See Also
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Geology / Geothermal Temperature FieldGeology
[ Petroleum Geology ][ Geological Model (GM) ] [ Neutral Temperature Layer (NTL) ] [ Unbiased Geothermal Temperature Profile (TGN) ]
[ Geothermal Temperature Profile @model ]
Reference
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GeothermalTemperatureProfile.xlsx