Page tree

You are viewing an old version of this page. View the current version.

Compare with Current View Page History

« Previous Version 3 Next »

@wikipedia


Motivation



Outputs

T_e(t, \, x, \, y, \, z)

along-hole geothermal temperature profile

Inputs

t

Astronomic time

\lambda(x, \, y, \, z)

Rock thermal conductivity 

j_z(x,y)

True vertical component of Regional Earth's heat flux (usually  j_z = 25 \div 55 \ mW/m^2)


Assumptions




Equations

Below Neutral Temperature LayerAbove Neutral Temperature Layer
(1) T_g(x,y,z) = T_n(x,y) + \int_{z_n}^z G_T(x,y,z) dz
(2) T(t, x, y,z) = T_s + \frac{j_z(x,y)}{\lambda_e} (z-z_s) + T_A \, \exp \left[ \, {(z_s-z}) \sqrt{\frac{\pi}{a_e \, \delta_T}} \, \right] \, \cos \left[ \, 2 \pi \frac{t - t_{min}}{\delta_T} + (z_s -z) \sqrt {\frac{\pi}{a_e \, \delta_T}} \, \right]
(3) G_T(x, y, z) =\frac{d T_g}{d z}= \frac{j_z(x,y,z)}{\lambda_e}

where

где

z_s

TVDss of the Earth's surface

T_{srf}

Annual average surface temperature based on weather reports

T_A

Annual average surface temperature variation based on weather reports

\delta_T

Temperature variation cycle (usually  \delta t = 1 \, {\rm year})

t_{min}

Temperature variation cycle shift (time moment of minimal temperature with respect to astronomic midnight 0:00)

a_e = \frac{\lambda_e}{\rho_e \, c_e}

Rock temperature conductivity

\rho_e

Rock density

c_e

Rock specific volumetric heat capacity at constant pressure

See Also


Geology / Geothermal Temperature Field

Geothermal Temperature Profile @model ]


References



Kasuda, T., and Archenbach, P.R. "Earth Temperature and Thermal Diffusivity at Selected Stations in the United States", ASHRAE Transactions, Vol. 71, Part 1, 1965.




  • No labels