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Spatial Variability of Saturated Hydraulic Conductivity in Irrigated Agricultural Soils of Beni Moussa Sub-Perimeter, Tadla, Morocco Cover

Spatial Variability of Saturated Hydraulic Conductivity in Irrigated Agricultural Soils of Beni Moussa Sub-Perimeter, Tadla, Morocco

Open Access
|Sep 2025

Figures & Tables

Fig. 1.

Location map of the study area showing soil sampling points.
Location map of the study area showing soil sampling points.

Fig. 2.

PCA of the physicochemical soil parameters of Beni Moussa irrigated perimeter. PCA, principal component analysis.
PCA of the physicochemical soil parameters of Beni Moussa irrigated perimeter. PCA, principal component analysis.

Fig. 3.

Fitted semi-variogram for the selected soil property: A – CaCO3, B – electrical conductivity, C – organic carbon, D – bulk density, E – stability, F – clay, G – silt, H – sand, I – moisture using the exponential model, J – Saturated hydraulic conductivity, K – organic matter, L – pH water, M – pH_KCl, N – porosity, and O – total dissolved solids using the spherical model.
Fitted semi-variogram for the selected soil property: A – CaCO3, B – electrical conductivity, C – organic carbon, D – bulk density, E – stability, F – clay, G – silt, H – sand, I – moisture using the exponential model, J – Saturated hydraulic conductivity, K – organic matter, L – pH water, M – pH_KCl, N – porosity, and O – total dissolved solids using the spherical model.

Fig. 4.

Kriging maps produced for Beni Moussa irrigated perimeter: (a) – saturated hydraulic conductivity Ks(mm · h−1); (b) – porosity%; (c) – bulk density; (d) – moisture%, (e) – pH water; (f) – electrical-conductivity (μs · cm−1); (g) – clay (%); (h) – sand (%).
Kriging maps produced for Beni Moussa irrigated perimeter: (a) – saturated hydraulic conductivity Ks(mm · h−1); (b) – porosity%; (c) – bulk density; (d) – moisture%, (e) – pH water; (f) – electrical-conductivity (μs · cm−1); (g) – clay (%); (h) – sand (%).

Fig. 4.

Kriging maps produced for Beni Moussa irrigated perimeter: (i) – silt (%); (j) – carbonate de calcium CaCO3 (%); (k) – organic matter (%); (l) – organic carbon. (m) – total dissolved solids and (n) – pHKcl.
Kriging maps produced for Beni Moussa irrigated perimeter: (i) – silt (%); (j) – carbonate de calcium CaCO3 (%); (k) – organic matter (%); (l) – organic carbon. (m) – total dissolved solids and (n) – pHKcl.

Descriptive statistics for soil properties at 0–20 cm depth in the study area_

Soil parameterDescriptive statistics
UnitNMeanMaxMinSDVarianceSkewnessKurtosis
Saturated hydraulic conductivitymm · h−170380.68679.0632.60147.6121,791.2000.852–0.112
Bulk densityg · cm−1700.821.431.170.130.019–0.4370.219
Porosity(%)7045.0068.5354.605.2627.6990.4370.219
Water content(%)700.7449.3918.887.9663.3930.8442.695
Water–log[H+]707.068.647.840.410.171–0.123–0.926
Electrical conductivityμS · cm−17024.301414.00289.65293.7886,309.0401.8843.568
Total dissolved solidsmg · l−17011.87750.00171.75168.3428,339.9401.9083.826
Organic matter(%)702.5327.989.724.1217.0471.8695.996
CaCo3(%)701.5016.205.632.395.7361.8695.996
Clay(%)707.0061.3038.8914.09198.600–0.775–0.440
Silt(%)7013.0081.2641.4715.03226.1350.6620.266
Sand(%)702.2534.8517.256.1137.4060.6700.883

Pearson correlation analysis of soil variables in the study area_

Soil parameterCorrelations
ClaySiltSandOrganic carbonpH H2OWater contentPorosityBulk densitySaturated hydraulic conductivity
Clay1
Silt–0.906**1
Sand–0.022–0.355**1
Organic carbon0.168–0.064–0.1791
pH H2O–0.045–0.0180.087–0.429**1
Water content–0.1240.0400.249*–0.2250.314**1
Porosity–0.089–0.1180.455**0.015–0.0790.2241
Bulk density0.0890.118–0.455**–0.0150.079–0.224–1.000**1
Saturated hydraulic conductivity–0.295*0.264*0.068–0.0400.0690.333**–0.1170.1171

Best suited variogram models and Moran’s I_

Soil parameterSemi-variogram modelNugget C0Sill (C0 + C)N/S [%]Range [m]Moran’s I
pH (water)Spherical0.019698.6777.4723,943.080.097
Electrical conductivitySpherical0.001532.2520.2736,857.24–0.168
CaCO3Spherical0.0164125.9971.2838,431.470.188
Organic carbonSpherical0.0095138.8862.9520,929.04–0.184
SandSpherical0.001698.4452.485738.900.070
ClaySpherical0.018368.8086.0537,250.14–0.002
SiltSpherical0.003822.6048.895939.51–0.163
PorositySpherical0.0192168.9741.5610,851.700.231
Saturated hydraulic conductivitySpherical0.0042114.5128.705838.280.201
Organic matterSpherical0.0147121.4056.655215.99–0.162
pH (KCl)Spherical0.003192.5353.8420,617.100.219
Total dissolved solidsSpherical0.01725.3788.9211,538.66–0.140
Water contentExponential0.00100.8530.5923,207.25–0.220
Bulk densitySpherical0.0112151.3836.1339,548.550.296

Cross-validation metrics for 14 soil parameters_

Soil parameterMean errorRoot mean square error RMSERoot mean square standardised error RMSSEAverage standard error
pH (water)–8.98E–070.00860.80490.0107
Electrical conductivity–0.000264965.79960.78207.4201
CaCO3–0.0009380.01830.85700.0214
Organic carbon–0.0000060.03990.77820.0511
Sand–0.0000560.13730.80780.1702
Clay–0.0002010.43170.80360.5378
Silt0.0000490.36680.30261.2130
Porosity0.0000150.16930.62880.2693
Saturated hydraulic conductivity0.0001104.84410.80586.0197
Organic matter–0.0001030.06870.77820.0884
pH (KCl)–0.0007050.00860.80490.0107
Total dissolved solids0.0000010.13810.84090.1649
△θ–0.0000150.01410.76150.0186
Bulk density–1.68E–070.00320.83490.0039
DOI: https://doi.org/10.14746/quageo-2026-0001 | Journal eISSN: 2081-6383 | Journal ISSN: 2082-2103
Language: English
Submitted on: May 9, 2025
Published on: Sep 17, 2025
Published by: Adam Mickiewicz University
In partnership with: Paradigm Publishing Services
Publication frequency: 4 issues per year
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© 2025 Atika Mouaddine, Hicham Bouzekraoui, Ahmed Barakat, El Hamzaoui El Hassania, Soufiane Hajaj, Zakaria Bni, Maria El-Harram, published by Adam Mickiewicz University
This work is licensed under the Creative Commons Attribution 4.0 License.

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