Quantification of Bed Load Transport in the Northern Part of the Central Plateau of Morocco: Case of Wadi Skhirate

H. Achiban, Hamid Achiban, A. Taous, Rachid Addou, Ismail Mansourie
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Abstract

Rivers play a vital role in our ecosystems, providing fresh water, supporting rich biodiversity, and contributing to human well-being. However, in the face of climate change and intensive human activities, the sediment load in rivers can reach critical levels, presenting a complex set of challenges that require immediate action. The increased sediment load can alter aquatic habitats, clog channels, reduce reservoir storage capacity, and increase the risk of flooding. These direct threats entail high costs in terms of material and ecological damage, loss of life, and expenditure on rebuilding damaged infrastructure. The quantification of bedload in watercourses is therefore crucial for maintaining water and soil resources, safeguarding riparian communities, and preserving ecological balance. The study reports the findings of a three-year monitoring of the bed load of Skhirate Wadi, a river that drains a part of the western Moroccan Meseta. The study used the colorimetric monitoring method, which quantifies the volumes of coarse sediment that were transported by monitoring topographic variations in the riverbed and measuring the distances covered by the sediment. The study showed the sediment was found to move around seven times annually on average. However, the frequency and magnitude of floods and the size of particles affect the variation in this displacement. It also showed sediments travel an average distance ranging from 649 to 883 meters per year, and that the average specific bedload at the watershed scale is 30 m3/ Km2/ year. Relationships between flood peaks mobilized sediment volumes, and average particle distances are established and discussed. These results are fundamental to understanding of coarse sediment transfer processes in the small rivers of the central plateau. They are also essential for assessing the impact on the aquatic ecosystem, on downstream dams, and on the various existing road and hydro-agricultural infrastructures. This assessment will enable the implementation of appropriate management strategies to anticipate changes and plan the planning of the river and its watershed.
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摩洛哥中部高原北部的床面负荷迁移量化:Wadi Skhirate 案例
河流在我们的生态系统中发挥着至关重要的作用,它提供淡水,支持丰富的生物多样性,并为人类福祉做出贡献。然而,面对气候变化和密集的人类活动,河流中的泥沙量可能达到临界水平,带来一系列复杂的挑战,需要立即采取行动。泥沙量的增加会改变水生生境、堵塞河道、降低水库蓄水能力并增加洪水风险。这些直接威胁会造成物质和生态破坏、生命损失以及重建受损基础设施的高昂成本。因此,河道床面负荷的量化对于维护水土资源、保护河岸社区和保持生态平衡至关重要。这项研究报告了对 Skhirate Wadi 河床负荷进行的为期三年的监测结果。该研究采用了比色监测方法,通过监测河床的地形变化和测量沉积物覆盖的距离来量化粗沉积物的迁移量。研究显示,沉积物平均每年移动七次。然而,洪水的频率和规模以及颗粒的大小都会影响这种位移的变化。研究还显示,沉积物每年平均移动 649 米至 883 米不等,流域范围内的平均特定床面负荷为 30 立方米/平方公里/年。洪峰移动沉积物量与平均颗粒距离之间的关系得到了确定和讨论。这些结果对于了解中部高原小河流的粗泥沙转移过程至关重要。它们对于评估对水生生态系统、下游水坝以及各种现有道路和水利农业基础设施的影响也至关重要。这种评估将有助于实施适当的管理战略,以预测变化和规划河流及其流域的规划。
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