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Groundwater recharge estimation using HYDRUS 1D model in Alasehir sub-basin of Gediz Basin in Turkey

机译:使用HYDRUS 1D模型估算土耳其盖迪斯盆地Alasehir盆地的地下水补给量

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摘要

Gediz Basin, located in the western part of Turkey constituting 2% land of the country, has an important groundwater potential in the area. Alasehir sub-basin, located in the southeast of the Gediz Basin and subject to the extensive withdrawal for the irrigation, constitutes the study area. Natural recharge to the sub-basin due to precipitation is numerically investigated in this study. For this purpose, 25 research wells, whose depths range from 20 to 50 m, were drilled to observe the recharge and collect the necessary field data for the numerical model. Meteorological data were collected from 3 weather stations installed in the study area. The numerical model HYDRUS was calibrated using the field water content data. Soil characterization was done on the core samples; the aquifer characterization was performed, and the alluvial aquifer recharge due to precipitation was calculated. As a result, the computed recharge value ranges from 21.78 to 68.52 mm, with an average value of 43.09 mm. According to the numerical model, this amount of recharge corresponds to 10% of the amount of annual rainfall.
机译:Gediz盆地位于土耳其西部,占该国2%的土地,在该地区具有重要的地下水潜力。位于吉迪斯盆地东南部的阿拉塞希尔(Alasehir)次流域构成了研究区域,需要大量灌溉。在这项研究中,数值研究了由于降水导致的流域自然补给。为此,钻了25口深度为20至50 m的研究井,以观察补给并收集数值模型所需的现场数据。气象数据是从研究区域内安装的3个气象站收集的。数值模型HYDRUS使用现场含水量数据进行了校准。对核心样品进行了土壤表征;进行含水层表征,并计算出由于降水造成的冲积含水层补给量。结果,计算的补给值范围为21.78至68.52 mm,平均值为43.09 mm。根据数值模型,该补给量相当于年降雨量的10%。

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