Modelisation Du Risque D’érosion Hydrique Par L’équation Universelle Des Pertes En Terre Dans Le Rif Occidental: Cas Du Bassin Versant De Moulay Bouchta (Maroc)

  • Anis Zouagui Unité de Recherche: Gestion conservatoire des eaux et des sols (IAV-Hassan II) et CNESTEN, Rabat, Maroc
  • Mohamed Sabir École Nationale Forestière d’Ingénieurs (ENFI), Salé, Maroc
  • Mustapha Naimi Institut Agronomique et Vétérinaire Hassan II (IAV), Rabat, Maroc
  • Mohamed Chikhaoui Institut Agronomique et Vétérinaire Hassan II (IAV), Rabat, Maroc
  • Moncef Benmansour Centre National de l’Énergie, des Sciences et des Techniques Nucléaires (CNESTEN), Rabat, Maroc

Abstract

Soil erosion causes many environmental and socio-economic problems: loss of biodiversity, decrease in the productivity of agricultural land, siltation of dams and increased risk of flooding. It is therefore essential to establish a detailed evaluation of this process before any spatial planning. To evaluate the effects of soil erosion spatially and quantitatively in order to face this phenomenon, and propose the best conservation and land development strategies, the Universal Soil Loss Equation (USLE) coupled with a geographic information system (GIS) is applied. This model is a multiplication of the five erosion factors: the erosivity of the rain, the erodibility of the soil, the inclination and the slope length, the vegetation cover and the anti-erosion practices. The study area is the Moulay Bouchta watershed (7 889 ha), which is located in the western part of the Rif Mountains, is characterized by a complex and contrasting landscape. The resulting soil loss map shows an average erosion rate of 39.5 (t/ha/yr), 87% of the basin has an erosion rate above the tolerance threshold for soil loss (7 (t/ha/yr)). Soil losses per subbasin range from 16.2 to 81.4 (t/ha/yr). The amount of eroded soil is estimated at 311,591 (t/yr), corresponding to a specific degradation of 12.1 (t/ha/yr). In the absence of any erosion control, 25% of the soil losses would reach the new dam located a little upstream of the basin outlet, reducing its water mobilization capacity to 59,625 (m3/yr). The application of Principal Component Analysis (PCA) to soil erosion factors shows a significant influence of topographic factor (LS) on soil erosion process, followed by the effect of support practices (P), then by soil erodibility (K).

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Published
2018-01-31
How to Cite
Zouagui, A., Sabir, M., Naimi, M., Chikhaoui, M., & Benmansour, M. (2018). Modelisation Du Risque D’érosion Hydrique Par L’équation Universelle Des Pertes En Terre Dans Le Rif Occidental: Cas Du Bassin Versant De Moulay Bouchta (Maroc). European Scientific Journal, ESJ, 14(3), 524. https://doi.org/10.19044/esj.2018.v14n3p524