You are viewing an old version of this page. View the current version.
Compare with Current
View Page History
« Previous
Version 10
Next »
Motivation
Inputs | Outputs |
---|
| vertical распределение вертикальной проекции регионального теплового потока из недр Земли на заданной глубине
z (обычно
j_e = 25 \div 55 \ mW/m^2) |
|
|
Assumptions
Equations
Approximations
(1) |
T_g(x,y,z) = T_{ref}(x,y) + \int_{z_{ref}}^z G_T(x,y,z) dz |
|
(2) |
G_T(z) =\frac{d T_g}{d z}= \frac{j_z}{\lambda_e} |
|
|
|
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.