ptfkit.zhao2016
ptfkit.zhao2016 ¶
Saturated hydraulic conductivity PTFs for the Loess Plateau of China.
Reference
Zhao, C., Shao, M., Jia, X., Nasir, M., & Zhang, C. (2016). Using pedotransfer functions to estimate soil hydraulic conductivity in the Loess Plateau of China. CATENA, 143, 1-6. https://doi.org/10.1016/j.catena.2016.03.037 DOI: 10.1016/j.catena.2016.03.037
- Territory
-
Typical Loess Plateau of China, covering approximately 430,000 square kilometers.
- Dataset
-
729 samples from 243 sites, sampled in 2012 at depths of 0-10, 10-20, and 20-40 cm. Each of 400 random calibration-validation splits used 583 development records and 146 validation records (Section 2.3.1).
| FUNCTION | DESCRIPTION |
|---|---|
calc_ptf_zhao2016_m2_1 | Estimate saturated hydraulic conductivity using reconstructed M2-1. |
calc_ptf_zhao2016_m2_2 | Estimate saturated hydraulic conductivity using reconstructed M2-2. |
calc_ptf_zhao2016_m2_3 | Estimate saturated hydraulic conductivity using reconstructed M2-3. |
calc_ptf_zhao2016_m2_4 | Estimate saturated hydraulic conductivity using reconstructed M2-4. |
calc_ptf_zhao2016_m2_5 | Estimate saturated hydraulic conductivity using reconstructed M2-5. |
calc_ptf_zhao2016_m2_6 | Estimate saturated hydraulic conductivity using reconstructed M2-6. |
calc_ptf_zhao2016_m2_1 ¶
calc_ptf_zhao2016_m2_1(*, bulk_density: float, silt: float, clay: float) -> floating
calc_ptf_zhao2016_m2_1(*, bulk_density: ArrayLike, silt: ArrayLike, clay: ArrayLike, out: NDArray[floating] | None = None) -> NDArray[floating]
Estimate saturated hydraulic conductivity using reconstructed M2-1.
| PARAMETER | DESCRIPTION |
|---|---|
bulk_density | Soil bulk density measured on undisturbed cores. (g/cm^3) TYPE: |
silt | Silt content measured by laser diffraction using USDA taxonomy (Section 2.2.2). (%) TYPE: |
clay | Clay content measured by laser diffraction using USDA taxonomy (Section 2.2.2). (%) TYPE: |
out | Optional output arrays for in-place calculation. TYPE: |
| RETURNS | DESCRIPTION |
|---|---|
ks | Saturated hydraulic conductivity, measured by the constant-head method. (mm/min) TYPE: |
Notes
Prediction target: Saturated hydraulic conductivity Highest-ranked fitted PTF, ranked by descending R-squared (Section 3.3). Uses Table 1 means and standard deviations for Jia et al. (2012) Equation 3 on both predictors and response, as a reviewed reconstruction.
Warning
The publication does not explicitly confirm Table 1 statistics as the fitted scaling constants or the application of response scaling. This reconstruction has not been verified against author software. Observed ranges describe the sampled soils; predictions are not clamped.
Source code in ptfkit/zhao2016.py
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calc_ptf_zhao2016_m2_2 ¶
calc_ptf_zhao2016_m2_2(*, bulk_density: float, silt: float, clay: float) -> floating
calc_ptf_zhao2016_m2_2(*, bulk_density: ArrayLike, silt: ArrayLike, clay: ArrayLike, out: NDArray[floating] | None = None) -> NDArray[floating]
Estimate saturated hydraulic conductivity using reconstructed M2-2.
| PARAMETER | DESCRIPTION |
|---|---|
bulk_density | Soil bulk density measured on undisturbed cores. (g/cm^3) TYPE: |
silt | Silt content measured by laser diffraction using USDA taxonomy (Section 2.2.2). (%) TYPE: |
clay | Clay content measured by laser diffraction using USDA taxonomy (Section 2.2.2). (%) TYPE: |
out | Optional output arrays for in-place calculation. TYPE: |
| RETURNS | DESCRIPTION |
|---|---|
ks | Saturated hydraulic conductivity, measured by the constant-head method. (mm/min) TYPE: |
Notes
Prediction target: Saturated hydraulic conductivity Mean coefficients of the top 25 percent, ranked by descending R-squared (Section 3.3). Uses Table 1 means and standard deviations for Jia et al. (2012) Equation 3 on both predictors and response, as a reviewed reconstruction.
Warning
The publication does not explicitly confirm Table 1 statistics as the fitted scaling constants or the application of response scaling. This reconstruction has not been verified against author software. Observed ranges describe the sampled soils; predictions are not clamped.
Source code in ptfkit/zhao2016.py
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calc_ptf_zhao2016_m2_3 ¶
calc_ptf_zhao2016_m2_3(*, bulk_density: float, silt: float, clay: float) -> floating
calc_ptf_zhao2016_m2_3(*, bulk_density: ArrayLike, silt: ArrayLike, clay: ArrayLike, out: NDArray[floating] | None = None) -> NDArray[floating]
Estimate saturated hydraulic conductivity using reconstructed M2-3.
| PARAMETER | DESCRIPTION |
|---|---|
bulk_density | Soil bulk density measured on undisturbed cores. (g/cm^3) TYPE: |
silt | Silt content measured by laser diffraction using USDA taxonomy (Section 2.2.2). (%) TYPE: |
clay | Clay content measured by laser diffraction using USDA taxonomy (Section 2.2.2). (%) TYPE: |
out | Optional output arrays for in-place calculation. TYPE: |
| RETURNS | DESCRIPTION |
|---|---|
ks | Saturated hydraulic conductivity, measured by the constant-head method. (mm/min) TYPE: |
Notes
Prediction target: Saturated hydraulic conductivity Mean coefficients of the top 50 percent, ranked by descending R-squared (Section 3.3). Uses Table 1 means and standard deviations for Jia et al. (2012) Equation 3 on both predictors and response, as a reviewed reconstruction.
Warning
The publication does not explicitly confirm Table 1 statistics as the fitted scaling constants or the application of response scaling. This reconstruction has not been verified against author software. Observed ranges describe the sampled soils; predictions are not clamped.
Source code in ptfkit/zhao2016.py
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calc_ptf_zhao2016_m2_4 ¶
calc_ptf_zhao2016_m2_4(*, bulk_density: float, silt: float, clay: float) -> floating
calc_ptf_zhao2016_m2_4(*, bulk_density: ArrayLike, silt: ArrayLike, clay: ArrayLike, out: NDArray[floating] | None = None) -> NDArray[floating]
Estimate saturated hydraulic conductivity using reconstructed M2-4.
| PARAMETER | DESCRIPTION |
|---|---|
bulk_density | Soil bulk density measured on undisturbed cores. (g/cm^3) TYPE: |
silt | Silt content measured by laser diffraction using USDA taxonomy (Section 2.2.2). (%) TYPE: |
clay | Clay content measured by laser diffraction using USDA taxonomy (Section 2.2.2). (%) TYPE: |
out | Optional output arrays for in-place calculation. TYPE: |
| RETURNS | DESCRIPTION |
|---|---|
ks | Saturated hydraulic conductivity, measured by the constant-head method. (mm/min) TYPE: |
Notes
Prediction target: Saturated hydraulic conductivity Mean coefficients of the top 75 percent, ranked by descending R-squared (Section 3.3). Uses Table 1 means and standard deviations for Jia et al. (2012) Equation 3 on both predictors and response, as a reviewed reconstruction.
Warning
The publication does not explicitly confirm Table 1 statistics as the fitted scaling constants or the application of response scaling. This reconstruction has not been verified against author software. Observed ranges describe the sampled soils; predictions are not clamped.
Source code in ptfkit/zhao2016.py
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calc_ptf_zhao2016_m2_5 ¶
calc_ptf_zhao2016_m2_5(*, bulk_density: float, silt: float, clay: float) -> floating
calc_ptf_zhao2016_m2_5(*, bulk_density: ArrayLike, silt: ArrayLike, clay: ArrayLike, out: NDArray[floating] | None = None) -> NDArray[floating]
Estimate saturated hydraulic conductivity using reconstructed M2-5.
| PARAMETER | DESCRIPTION |
|---|---|
bulk_density | Soil bulk density measured on undisturbed cores. (g/cm^3) TYPE: |
silt | Silt content measured by laser diffraction using USDA taxonomy (Section 2.2.2). (%) TYPE: |
clay | Clay content measured by laser diffraction using USDA taxonomy (Section 2.2.2). (%) TYPE: |
out | Optional output arrays for in-place calculation. TYPE: |
| RETURNS | DESCRIPTION |
|---|---|
ks | Saturated hydraulic conductivity, measured by the constant-head method. (mm/min) TYPE: |
Notes
Prediction target: Saturated hydraulic conductivity Mean coefficients of all 400 PTFs, ranked by descending R-squared (Section 3.3). Uses Table 1 means and standard deviations for Jia et al. (2012) Equation 3 on both predictors and response, as a reviewed reconstruction.
Warning
The publication does not explicitly confirm Table 1 statistics as the fitted scaling constants or the application of response scaling. This reconstruction has not been verified against author software. Observed ranges describe the sampled soils; predictions are not clamped.
Source code in ptfkit/zhao2016.py
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calc_ptf_zhao2016_m2_6 ¶
calc_ptf_zhao2016_m2_6(*, bulk_density: float, silt: float, clay: float) -> floating
calc_ptf_zhao2016_m2_6(*, bulk_density: ArrayLike, silt: ArrayLike, clay: ArrayLike, out: NDArray[floating] | None = None) -> NDArray[floating]
Estimate saturated hydraulic conductivity using reconstructed M2-6.
| PARAMETER | DESCRIPTION |
|---|---|
bulk_density | Soil bulk density measured on undisturbed cores. (g/cm^3) TYPE: |
silt | Silt content measured by laser diffraction using USDA taxonomy (Section 2.2.2). (%) TYPE: |
clay | Clay content measured by laser diffraction using USDA taxonomy (Section 2.2.2). (%) TYPE: |
out | Optional output arrays for in-place calculation. TYPE: |
| RETURNS | DESCRIPTION |
|---|---|
ks | Saturated hydraulic conductivity, measured by the constant-head method. (mm/min) TYPE: |
Notes
Prediction target: Saturated hydraulic conductivity Lowest-ranked fitted PTF, ranked by descending R-squared (Section 3.3). Uses Table 1 means and standard deviations for Jia et al. (2012) Equation 3 on both predictors and response, as a reviewed reconstruction.
Warning
The publication does not explicitly confirm Table 1 statistics as the fitted scaling constants or the application of response scaling. This reconstruction has not been verified against author software. Observed ranges describe the sampled soils; predictions are not clamped.
Source code in ptfkit/zhao2016.py
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