ptfkit.ahuja1984
ptfkit.ahuja1984 ¶
Ahuja et al. (1984), effective-porosity relations for saturated conductivity.
Reference
Ahuja, L. R., Naney, J. W., Green, R. E., & Nielsen, D. R. (1984). Macroporosity to characterize spatial variability of hydraulic conductivity and effects of land management. Soil Science Society of America Journal, 48, 699-702.
- Territory
-
Chickasha, Oklahoma, and the Wahiawa Plateau, Oahu, Hawaii, USA
- Dataset
-
Undisturbed cores from 15 sites in a 9.6-ha Renfro silt loam watershed and 54 cores from three related Hawaii Oxic soils; the Hawaii study also supplied 35 field measurements of saturated hydraulic conductivity.
| FUNCTION | DESCRIPTION |
|---|---|
calc_ptf_ahuja1984 | Calculate the pedotransfer function. |
calc_ptf_ahuja1984 ¶
calc_ptf_ahuja1984(*, total_porosity: float, theta_33: float, coefficient_b: float, exponent_n: float) -> floating
calc_ptf_ahuja1984(*, total_porosity: ArrayLike, theta_33: ArrayLike, coefficient_b: ArrayLike, exponent_n: ArrayLike, out: NDArray[floating] | None = None) -> NDArray[floating]
Calculate the pedotransfer function.
Estimate saturated hydraulic conductivity from total porosity and water content at -33 kPa using user-supplied empirical coefficients.
| PARAMETER | DESCRIPTION |
|---|---|
total_porosity | Total porosity; in the experiments it was taken as saturated volumetric water content. (cm^3/cm^3) TYPE: |
theta_33 | Volumetric soil water content at -33 kPa pressure head. (cm^3/cm^3) TYPE: |
coefficient_b | Soil-specific empirical coefficient in the generalized Kozeny-Carman relation. (cm/h) TYPE: |
exponent_n | Empirical exponent; the paper evaluates values of 4 and 5 for deriving conductivity scaling-factor distributions. (1) TYPE: |
out | Optional output arrays for in-place calculation. TYPE: |
| RETURNS | DESCRIPTION |
|---|---|
k_sat | Saturated hydraulic conductivity. (cm/h) TYPE: |
Territory
Chickasha, Oklahoma, and the Wahiawa Plateau, Oahu, Hawaii, USA
Models
\(k(h)\): Saturated hydraulic conductivity
Notes
Prediction target: Saturated hydraulic conductivity from effective porosity, defined as total porosity minus volumetric water content at -33 kPa. Effective porosity is total_porosity - theta_33; the paper notes that field capacity is not a precisely defined soil parameter. Soil-core fitted exponents were near 4, whereas the smaller Hawaii field dataset had a fitted slope of 1.59 over a narrower effective-porosity range.
Warning
The empirical coefficient B varies with soil type; callers must supply a coefficient calibrated for the soil being evaluated. Callers must supply the exponent. The paper evaluates both n = 4 and n = 5 and does not select one as a unique transferable value. total_porosity must be greater than or equal to theta_33.
Source code in ptfkit/ahuja1984.py
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