通过地理空间分析和磁感应强度评估土壤侵蚀风险:摩洛哥中部里夫省 Oued Ghiss 大坝流域研究

IF 2.7 Q2 MULTIDISCIPLINARY SCIENCES Scientific African Pub Date : 2024-09-19 DOI:10.1016/j.sciaf.2024.e02401
Soukaina Ed-Dakiri, Issam Etebaai, Said El Moussaoui, Abdelhamid Tawfik, Mustapha Lamgharbaj, Hajar El Talibi, Hinde Cherkaoui Dekkaki, Morad Taher
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引用次数: 0

摘要

在摩洛哥北部,由于极端的气候条件、多变的地形、岩性的脆弱性以及人为压力,水土流失对土壤退化和大坝沉积构成了严重威胁。本研究对摩洛哥里夫中部 Oued Ghiss 大坝集水区的土壤侵蚀易发性进行了定量和空间评估。该研究利用与地理信息系统 (GIS) 相结合的修订通用土壤流失方程 (RUSLE),并通过磁感应强度指标进行校准,对侵蚀因素进行了详细分析。该模型利用地理信息系统对降雨量、土壤类型、地形、土地覆盖和管理方法等数据进行空间分析,并通过磁感应强度测量确定稳定区和易受侵蚀区,对模型进行校准。由此绘制的土壤流失图显示,平均侵蚀率为 24 吨/公顷/年。具体而言,37.28%的流域面积的侵蚀率低于 5 吨/公顷/年,40.16%介于 5 至 10 吨/公顷/年之间,22.77%介于 10 至 20 吨/公顷/年之间,0.86%超过 20 吨/公顷/年。不同土壤剖面的磁感应强度测量结果表明,稳定的土壤向地表方向的磁感应强度增加,而侵蚀的土壤磁感应强度降低,磁感应强度变化与最终风险图之间存在显著的相关性。这种通过磁感应强度对 RUSLE 模型进行校准的创新方法改进了侵蚀脆弱性评估,并生成了更详细的土壤流失图。这些发现为政策制定者提供了重要信息,帮助他们为水土流失易发地区制定有针对性的管理计划,特别是吉斯大坝流域,这些发现将有助于防止大坝淤积和加强水资源管理。这证实了磁感应强度在评估土壤侵蚀脆弱性和改进数值模型方面的可靠性。
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Assessing soil erosion risk through geospatial analysis and magnetic susceptibility: A study in the Oued Ghiss dam watershed, Central Rif, Morocco
In northern Morocco, water erosion presents a critical risk for soil degradation and dam sedimentation, attributable to extreme climatic conditions, variegated topography, lithological vulnerabilities, and anthropogenic pressures. This study quantitatively and spatially evaluates soil erosion susceptibility within the catchment area of the Oued Ghiss dam in Central Rif, Morocco. Utilizing the Revised Universal Soil Loss Equation (RUSLE) integrated with Geographic Information Systems (GIS) and calibrated through magnetic susceptibility metrics, the study provides a detailed analysis of erosion factors. The model was applied using GIS to spatially analyze data on rainfall, soil type, topography, land cover, and management practices, with magnetic susceptibility measurements used to calibrate the model by identifying stable and erosion-prone areas. The resultant soil loss map reveals a mean erosion rate of 24 t/ha/year. Specifically, 37.28 % of the catchment area exhibits an erosion rate under 5 t/ha/year, 40.16 % between 5 and 10 t/ha/year, 22.77 % between 10 and 20 t/ha/year, and 0.86 % surpasses 20 t/ha/year. Magnetic susceptibility measurements across various soil profiles indicated that stable soils showed increased susceptibility towards the surface, while eroded soils displayed decreased susceptibility, with significant correlations found between magnetic susceptibility variations and the final risk map. This innovative calibration of the RUSLE model through magnetic susceptibility improves erosion vulnerability assessments and results in a more detailed soil loss map. The findings provide critical information for policymakers to develop targeted management plans for erosion-prone areas, particularly benefiting the Ghiss dam watershed, where these insights will aid in preventing dam siltation and enhancing water resource management. This confirms magnetic susceptibility's reliability in assessing soil erosion vulnerability and improving numerical models.
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来源期刊
Scientific African
Scientific African Multidisciplinary-Multidisciplinary
CiteScore
5.60
自引率
3.40%
发文量
332
审稿时长
10 weeks
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