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首页> 外文期刊>Acta Geophysica >Quaternary aquifer transmissivity derived from vertical electrical sounding measurements in the semi-arid Khanasser Valley Region, Syria
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Quaternary aquifer transmissivity derived from vertical electrical sounding measurements in the semi-arid Khanasser Valley Region, Syria

机译:从叙利亚半干旱哈纳瑟河谷地区的垂直电测深获得的第四层含水层透射率

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摘要

Vertical electrical sounding technique (VES) is used as an alternative approach to pumping test for computing the Quaternary aquifer transmissivity in the Khanasser Valley, Northern Syria. The method is inexpensive, easy and gives faster results with higher special resolution than the traditional pumping technique. The hydraulic conductivity values obtained using VES agree with the pumping test results, which in the Khanasser Valley vary between the order of 0.864 and 8.64 m/day (10 ~(-5) and 10 ~(-4) m/s). The probable location of the Quaternary aquifer in the Khanasser Valley is obtained through the transmissivity map derived from VES. The knowledge of transmissivity is fundamental for modeling and management processes in the Khanasser Valley. Other similar semiarid regions can benefit from the approach successfully applied in the study area.
机译:垂直电测深技术(VES)被用作抽水试验的替代方法,用于计算叙利亚北部哈纳瑟山谷的第四纪含水层透射率。与传统的泵送技术相比,该方法便宜,容易,并且具有更高的特殊分辨率,可提供更快的结果。使用VES获得的水力传导率值与抽水测试结果一致,在哈纳瑟尔河谷,水的电导率值在0.864和8.64 m / day(10〜(-5)和10〜(-4)m / s)之间变化。通过从VES得出的透射率图获得在Khanasser谷中第四纪含水层的可能位置。透射率的知识是Khanasser谷地建模和管理过程的基础。其他类似的半干旱地区也可以从研究领域成功应用的方法中受益。

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