Groundwater Artificial Recharge Potentiality in Al-Qilt Catchment Jericho – West Bank – Palestine

A. Masri, M. Ghanem
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Abstract

The main research objective is to highlight the potentiality of artificial groundwater recharge in Al-Qilt catchment- Jericho – Palestine regarding the water shortage in the groundwater-supplied areas. Artificial recharge can be a possible option in increasing the storability of the underground aquifer, which will add values to the Palestinian strategy to optimize the total accessibility of groundwater resources. The increase of water demands and the scarcity of water resources in the Jordan Rift areas are putting challenges for the water managers and planners to improve the water supplies in order to reach the best ways for the integrated water resources management. In Al-Qilt catchment, the surface water discharge flowing into the wadies in huge amounts had no noticeable significant benefits. A hydrological model was built for the Qilt basin using HEC-HMS software system and it was considered as an essential tool for better understanding of the basin hydrological situation and its hydrogeological characteristics. The surface runoff water speed was measured to be 3.2 m/s (27th of February, 2019) with a cross section width of 9.2 m and 0.75 m hight with water leading to a flow of 18.77 m3/s and the total flow of approximately 67565 m3/hr. The estimated model simulations reavealed of 18.5 m3/s and 66600 m3/hr for the speed flow and the total flow respectively and matched with the measured ones. The results were used for improving the aquifer-integrated management in Al-Qilt area and determining of the aquifer potentiality for artificial recharge. The built model results gave guiding to the hydrologists and the decision makers for selecting the appropriate techniques and sites for artificial recharge. The model indicated of good simulation tools to be used for other West Bank catchments.
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杰里科-西岸-巴勒斯坦Al-Qilt集水区地下水人工补给潜力
主要的研究目标是强调在Al-Qilt集水区-杰里科-巴勒斯坦人工补给地下水的潜力,以解决地下水供应地区的缺水问题。人工补给可以是增加地下蓄水层储存能力的一个可能选择,这将增加巴勒斯坦优化地下水资源总可得性的战略的价值。在约旦裂谷地区,水需求的增加和水资源的短缺对水的管理人员和规划人员提出了挑战,要求他们改善水的供应,以便找到综合水资源管理的最佳途径。在Al-Qilt集水区,大量地表水流入河道没有明显的显著效益。利用HEC-HMS软件系统建立了基尔特流域的水文模型,认为该模型是更好地了解流域水文状况及其水文地质特征的重要工具。2019年2月27日测得地表径流水流速度为3.2 m/s,断面宽度为9.2 m,断面高度为0.75 m,水流流量为18.77 m3/s,总流量约为67565 m3/hr。模型模拟的流速和总流量分别为18.5 m3/s和66600 m3/hr,与实测值基本吻合。研究结果可用于改进Al-Qilt地区含水层综合管理和确定含水层人工补给潜力。建立的模型结果为水文工作者和决策者选择合适的人工补给技术和地点提供了指导。该模型指出,良好的模拟工具可用于西岸其他集水区。
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