[HTML][HTML] Delineation of vulnerable areas to water erosion in a mountain region using SDR-InVEST model: A case study of the Ourika watershed, Morocco
HA Ougougdal, MY Khebiza, M Messouli, L Bounoua - Scientific African, 2020 - Elsevier
HA Ougougdal, MY Khebiza, M Messouli, L Bounoua
Scientific African, 2020•ElsevierThe Ourika watershed is characterized by higher than average flood flows, a rugged
topography, a sparse vegetation cover and a friable substrate that makes it vulnerable to soil
erosion. Soil is an important non-renewable asset capital, providing several ecosystem
services that sustain life through physical and biological regulation processes. The loss, or
otherwise, redistribution of biota by soil erosion in the Ourika watershed has received little
attention and thus constitutes a key knowledge gap that needs to be addressed. This study …
topography, a sparse vegetation cover and a friable substrate that makes it vulnerable to soil
erosion. Soil is an important non-renewable asset capital, providing several ecosystem
services that sustain life through physical and biological regulation processes. The loss, or
otherwise, redistribution of biota by soil erosion in the Ourika watershed has received little
attention and thus constitutes a key knowledge gap that needs to be addressed. This study …
Abstract
The Ourika watershed is characterized by higher than average flood flows, a rugged topography, a sparse vegetation cover and a friable substrate that makes it vulnerable to soil erosion. Soil is an important non-renewable asset capital, providing several ecosystem services that sustain life through physical and biological regulation processes. The loss, or otherwise, redistribution of biota by soil erosion in the Ourika watershed has received little attention and thus constitutes a key knowledge gap that needs to be addressed. This study quantifies the level of erosion and maps its spatial distribution in the watershed using the Sediment Delivery Ratio (SDR) of the Integrated Valuation of Ecosystem Services and Trade-offs model (InVEST 3.6.0). The SDR maps the overland sediment generation and delivery to the stream at the watershed level using rainfall, soil properties, topography, cover management and cropping practices as predefined set of input variables. Recommended internal model calibration was used and results were compared to similar studies carried out in different parts of Morocco for validation. The results reveal that 93% of the watershed is subject to a strong rainfall aggressiveness greater than 50 MJ mm ha–1 h–1 yr–1 under an average rainfall intensity of 541 mm/year, rainfall capacity to initiate the detachment and transport of soil particles by runoff, and only 11.5 % of the watershed area is protected with vegetative cover. We find that overall, the Ourika watershed is losing its soil to erosion at an alarming average rate of 258.48 ton.ha–1.yr–1, a rate well above the tolerable threshold of 7 ton.ha–1.yr–1. The spatial distribution of this loss shows areas that need to be urgently remedied. The primary factors for soil erosion in the Ourika watershed appear to be related to the aggressive nature of local rainfall and the inherent susceptibility of soils, which can be costly to this cash-crop region. Because rainfall intensity, soil properties, and topography are intrinsic characteristics of the watershed, we suggest that seasonally adapted cropping rotations that maintains conservative practices with a high cover management may reduce soil erosion in the Ourika watershed.
Elsevier
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