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利用 HYDRUS 1D 模型估算土耳其杰伊汉盆地阿拉谢希尔子流域的地下水补给量。

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

机构信息

Department of Civil Engineering, İzmir Institute of Technology, İzmir, Turkey.

Torbalı Vocational High School, Dokuz Eylül University, İzmir, Turkey.

出版信息

Environ Monit Assess. 2019 Sep 5;191(10):610. doi: 10.1007/s10661-019-7792-6.

Abstract

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.

摘要

杰地兹盆地位于土耳其西部,占该国土地的 2%,该地区具有重要的地下水潜力。位于杰地兹盆地东南部的阿拉谢希尔子流域因灌溉而大量抽取地下水,是本次研究的区域。本研究通过数值方法研究了该子流域因降水产生的自然补给。为此,钻了 25 口研究井,深度在 20 至 50 米之间,以观测补给并收集数值模型所需的实地数据。气象数据是从安装在研究区域的 3 个气象站收集的。使用实地含水量数据对 HYDRUS 数值模型进行了校准。对岩心样本进行了土壤特征描述;对含水层进行了特征描述,并计算了因降水而产生的冲积含水层补给量。结果表明,计算得出的补给量在 21.78 至 68.52 毫米之间,平均值为 43.09 毫米。根据数值模型,这一补给量相当于年降雨量的 10%。

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