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Application of a spatially distributed water balance model for assessing surface and groundwater resources: a case study of Adigrat area, Northern Ethiopia

机译:空间分布水平衡模型评估地面和地下水资源的应用 - 以埃塞俄比亚北部阿德格特地区为例

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摘要

The study area is located in the northern part of Ethiopia and covers an area of 279km~2. The study area is one of the most water-stressed areas of Ethiopia, which is characterized by erratic nature with short period of rainy season that lasts from late June to early September. As a result surface water is limited, making groundwater the main source of water for domestic and irrigation purposes. Hence, the main objective of this research work is to assess the available water resource of the study area using a GIS-based distributed water balance model (WetSpass). This model depends on the spatial variations of land use, soil texture, topography, slope, groundwater level, and hydro-meteorological conditions. Input data for the WetSpass model were prepared in the form of grid maps and parameter attribute tables. The parameter attribute tables were adjusted using the professional knowledge and literature conducted nearby the study area. The main outputs of the WetSpass model are seasonal and annual evapotranspiration, surface runoff and groundwater recharge. Accordingly, the simulated model result shows that 77.6% of the annual precipitation is lost through evapotranspiration, 16% becomes surface runoff and about 6.4% of the annual precipitation recharges to the groundwater. The novelty of this research work is to show that the WetSpass model can be used to simulate water balance components in semi-arid and water-stressed environments provided that the model input parameters are close-fitting to the local condition. The output of this study can serve as reference for water resource experts and policymakers during planning and management of different water resource-related projects.
机译:研究区位于埃塞俄比亚的北部,占地面积279公里〜2。该研究区是埃塞俄比亚最省油的地区之一,其特点是短期的雨季短期,持续时间从6月下旬到9月初。结果表面用水有限,制造地下水是国内和灌溉目的的主要水源。因此,本研究工作的主要目的是使用基于GIS的分布式水平衡模型(WETSpass)来评估研究区域的可用水资源。该模型取决于土地使用,土壤纹理,地形,坡度,地下水位和水流气象条件的空间变化。以网格图和参数属性表的形式编写Wetspass模型的输入数据。参数属性表使用研究区域附近进行的专业知识和文献进行调整。 Wetspass模型的主要输出是季节性和年度蒸散,表面径流和地下水充电。因此,模拟模型结果表明,每年降水量的77.6%通过蒸散蒸腾而丧失,16%变为表面径流,占年降水量的约6.4%的地下水。本研究工作的新颖性是展示威特通模型可用于模拟半干旱和耐水环境中的水平衡分量,规划为模型输入参数对本地条件闭合。本研究的产出可作为不同水资源相关项目的规划和管理期间水资源专家和政策制定者的参考。

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