Page tree

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

Compare with Current View Page History

« Previous Version 25 Next »


Motivation



Outputs

T_e(t, l)

along-hole geothermal temperature profile

Inputs

t

Astronomic time

z(l)

Pipeline trajectory TVDss

j_z

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(l) = T_n + \int_{z_n}^z G_T(z) dz
(2) T(t, z) = T_s + \frac{j_z}{\lambda_e} (z-z_s) + T_Y(t, z) + T_D(t, z)
(3) G_T(z) =\frac{d T_g}{d z}= \frac{j_z}{\lambda_e}
(4) T_A(t,z) = \delta T_A \, \exp \left[ \, {(z_s-z}) \sqrt{\frac{\pi}{a_e \, A_T}} \, \right] \, \cos \left[ \, 2 \pi \frac{t - \delta t_A}{A_T} + (z_s -z) \sqrt {\frac{\pi}{a_e \, A_T}} \, \right]

(5) T_D(t,z) = 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_{srf} -z) \sqrt {\frac{\pi}{a_e \, \delta_T}} \, \right]

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

A_T

Period of annual temperature variation cycle: A_T = 1 \, {\rm year})

\delta t_A

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 Profile

Geothermal Temperature Field @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