Estimation of Groundwater Recharge in a Volcanic Aquifer System Using Soil Moisture Balance and Baseflow Separation Methods: The Case of Gilgel Gibe Catchment, Ethiopia

F. Tufa, Fekadu Fufa Feyissa, Adisu Befekadu Kebede, Beekan Gurmessa Gudeta, Wagari Mosisa Kitessa, Seifu Kebede Debela, Bekan Chelkeba Tumsa, Alemu Yenehun, M. Van Camp, K. Walraevens
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Abstract

Understanding the recharge–discharge system of a catchment is key to the efficient use and effective management of groundwater resources. The present study focused on the estimation of groundwater recharge using Soil Moisture Balance (SMB) and Baseflow Separation (BFS) methods in the Gilgel Gibe catchment where water demand for irrigation, domestic, and industrial purposes is dramatically increasing. The demand for groundwater and the existing ambitious plans to respond to this demand will put a strain on the groundwater resource in the catchment unless prompt intervention is undertaken to ensure its sustainability. Ground-based hydrometeorological 36-years data (1985 to 2020) from 17 stations and satellite products from CHIRPS and NASA/POWER were used for the SMB method. Six BFS methods were applied through the Web-based Hydrograph Analysis Tool (WHAT), SepHydro, BFLOW, and Automated Computer Programming (PART) to sub-catchments and the main catchment to estimate the groundwater recharge. The streamflow data (discharge) obtained from the Ministry of Water and Energy were the main input data for the BFS methods. The average annual recharge of groundwater was estimated to be 313 mm using SMB for the years 1985 to 2020 and 314 mm using BFS for the years 1986 to 2003. The results from the SMB method revealed geographical heterogeneity in annual groundwater recharge, varying from 209 to 442 mm. Significant spatial variation is also observed in the estimated annual groundwater recharge using the BFS methods, which varies from 181 to 411 mm for sub-catchments. Hydrogeological conditions of the catchment were observed, and the yielding capacity of existing wells was assessed to evaluate the validity of the results. The recharge values estimated using SMB and BFS methods are comparable and hydrologically reasonable. The findings remarkably provide insightful information for decision-makers to develop effective groundwater management strategies and to prioritize the sub-catchments for immediate intervention to ensure the sustainability of groundwater.
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利用土壤水分平衡和基流分离方法估算火山含水层系统的地下水补给量:埃塞俄比亚 Gilgel Gibe 集水区案例
了解集水区的补给-排泄系统是高效利用和有效管理地下水资源的关键。本研究的重点是利用土壤水分平衡法(SMB)和基流分离法(BFS)估算吉尔吉吉贝集水区的地下水补给量,该集水区的灌溉、生活和工业用水需求正在急剧增加。对地下水的需求以及为满足这一需求而制定的现有宏伟计划将对集水区的地下水资源造成压力,除非及时采取干预措施,确保地下水资源的可持续性。SMB 方法使用了来自 17 个站点的 36 年(1985 年至 2020 年)地面水文气象数据以及来自 CHIRPS 和 NASA/POWER 的卫星产品。通过基于网络的水文图分析工具 (WHAT)、SepHydro、BFLOW 和自动计算机编程 (PART),对子流域和主流域应用了六种 BFS 方法,以估算地下水补给量。从水利和能源部获得的溪流数据(排水量)是 BFS 方法的主要输入数据。1985 年至 2020 年,采用 SMB 方法估算的年均地下水补给量为 313 毫米;1986 年至 2003 年,采用 BFS 方法估算的年均地下水补给量为 314 毫米。SMB 方法的结果显示,地下水年补给量存在地域差异,从 209 毫米到 442 毫米不等。使用 BFS 方法估算的年地下水补给量也存在显著的空间差异,子流域的差异从 181 毫米到 411 毫米不等。对集水区的水文地质条件进行了观测,并对现有水井的出水能力进行了评估,以评价结果的有效性。使用 SMB 和 BFS 方法估算出的补给值具有可比性,在水文上也是合理的。研究结果为决策者制定有效的地下水管理策略和优先考虑需要立即干预的次级集水区以确保地下水的可持续性提供了极具洞察力的信息。
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