STUDY OF THE CLOGGING PROCESS IN A SEMI-ARID REGION: WADI EL HIMMER, MOROCCO

M. Zaidi, N. Ahfir, A. Alem, B. Mansouri, Huaqing Wang
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Abstract

In semi-arid regions, managed aquifer recharge (MAR) is seen as an efficient solution among others for protecting groundwater resources. Clogging is one of the major issues that can reduce the durability of recharge facilities. As a consequence of clogging of soils by suspended matter, permeability, and porosity, and therefore exchange between surface water and groundwater are reduced. To our knowledge, few researchers have studied the mechanism of clogging of the MAR in a semi-arid region according to hydrologic conditions of the field. The main objective of the present work is to study the clogging process of recharge sites in a semi-arid region (Wadi El Himmer, Morocco). These recharge sites consist of a “Percolation Tank” and “Recharge Releases”, which retard and distribute the flow to facilitate infiltration into a saturated zone. Field measurements are conducted to quantify the thickness of the surface deposits (cake) according to precipitation at different recharge sites. To realize these measurements, wooden pickets were implanted at different locations of the recharge sites. After 12 weeks of exposure to hydro-meteorological conditions, the thickness of the deposited (suspended matter) layer was measured on each picket. In order to facilitate the interpretation of results, the kriging method was used to interpolate obtained measurements. A significant variation in cake thickness was observed at each recharge site following the flow direction. The layer deposited is mainly dominated by red clays and silts. These results prompted us to investigate the impact of these deposits on the deep clogging.
半干旱地区堵塞过程的研究:摩洛哥瓦迪埃尔希默
在半干旱地区,管理含水层补给(MAR)被视为保护地下水资源的有效解决方案之一。堵塞是降低充电设施耐久性的主要问题之一。由于土壤被悬浮物堵塞,渗透性和孔隙度降低,因此地表水和地下水之间的交换减少。据我们所知,很少有研究人员从野外水文条件出发,研究半干旱区旱地湿地的堵塞机理。本工作的主要目的是研究半干旱区(Wadi El Himmer,摩洛哥)补给点的堵塞过程。这些补给点由“渗滤池”和“补给放放点”组成,它们延缓和分配水流,以促进渗透到饱和区。根据不同补给点的降水,进行了现场测量,以量化地表沉积物(饼)的厚度。为了实现这些测量,在补给点的不同位置植入了木制纠察桩。在水文气象条件下暴露12周后,测量每个桩上沉积(悬浮物)层的厚度。为了便于结果的解释,采用克里格法对得到的测量值进行插值。沿流动方向,各补给点的滤饼厚度变化显著。沉积层以红粘土和粉砂为主。这些结果促使我们研究这些沉积物对深层堵塞的影响。
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