thermal_cable_model.ground — Ground Temperature Models
Seasonal ground and ambient temperature models.
The Kasuda equation models the undisturbed ground temperature as a function of depth and day-of-year, accounting for seasonal thermal wave penetration.
- class GroundTemperatureModel[source]
Bases:
ABCBase class for ground / ambient temperature models.
- class ConstantGroundTemperature[source]
Bases:
GroundTemperatureModelSpatially and temporally uniform ground temperature.
- class KasudaModel[source]
Bases:
GroundTemperatureModelKasuda & Archenbach (1965) undisturbed ground temperature.
\[T(z,t) = T_\text{mean} - T_\text{amp} \exp\!\Bigl( -z \sqrt{\frac{\pi}{P\,\alpha}}\Bigr) \cos\!\Bigl(\frac{2\pi}{P}\bigl(t - t_0 - \tfrac{z}{2}\sqrt{\frac{P}{\pi\,\alpha}}\bigr)\Bigr)\]- Parameters:
mean_surface_temp (float) – Annual mean surface temperature [°C].
annual_amplitude (float) – Half the peak-to-peak annual surface temperature swing [°C].
day_of_min_surface_temp (float) – Day of year at which the surface temperature is at its minimum (e.g. ~35 for central Europe ≈ early February).
soil_diffusivity (float) – Thermal diffusivity α of the soil [m²/s]. Typical range 0.3–0.8 × 10⁻⁶.
- SECONDS_PER_DAY = 86400.0
- DAYS_PER_YEAR = 365.25
- __init__(mean_surface_temp=12.0, annual_amplitude=10.0, day_of_min_surface_temp=35.0, soil_diffusivity=5e-07)[source]