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首页> 外文期刊>Journal of African Earth Sciences >Hydraulic parameters estimation by using an approach based on vertical electrical soundings (VES) in the semi-arid Khanasser valley region, Syria
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Hydraulic parameters estimation by using an approach based on vertical electrical soundings (VES) in the semi-arid Khanasser valley region, Syria

机译:使用基于垂直电测深(VES)的方法在叙利亚半干旱Khanasser山谷地区进行水力参数估算

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摘要

A new alternative approach based on using Vertical electrical sounding (VES) technique is proposed for computing the hydraulic conductivity IC of an aquifer. The approach takes only the salinity of the groundwater into consideration. VES measurements in the locations, where available water samples exist, are required in such an approach, in order to calibrate and establish empirical relationships between transverse resistance Dar-Zarrouck TR parameter and modified transverse resistance MTR, and between MTR and transmissivity T. Those relationships are thereafter used to extrapolate the transmissivity even in the VES points where no water samples exist This approach is tested and practiced in the Khanasser valley, Northern Syria, where the hydraulic conductivity of the Quaternary aquifer is computed. An acceptable agreement is found between the hydraulic conductivity values obtained by the proposed approach and those obtained by the pumping test which range between 0.864 and 8.64 m/day (10(-5) and 10(-4) m/s). The Quaternary aquifer transmissivity of the Khanasser Valley, has been characterized by using this approach and by adapting the MTR parameter. The transmissivity varies between a minimum of 79 m(2)/day and a maximum of 814 m(2)/day, with an average of 283 m(2)/day and a standard deviation of 145 m(2)/day. The easy and inexpensive approach proposed in this paper can be applied in other semi arid regions. (C) 2016 Elsevier Ltd. All rights reserved.
机译:提出了一种基于垂直电测深(VES)技术的替代方法,用于计算含水层的水力传导率IC。该方法仅考虑地下水的盐度。为了校准和建立横向电阻Dar-Zarrouck TR参数与修正的横向电阻MTR之间以及MTR与透射率T之间的经验关系,需要采用这种方法在存在可用水样的位置进行VES测量。此后,即使在不存在水样的VES点中,也可以使用这些方法外推透射率。该方法在叙利亚北部的Khanasser谷地进行了测试和实践,在那里计算了第四纪含水层的水力传导率。在通过提议的方法获得的水力传导率值与通过抽水试验获得的水力传导率值之间,在0.864至8.64 m / day(10(-5)至10(-4)m / s)之间找到了可以接受的协议。通过使用这种方法并通过调整MTR参数来表征Khanasser谷的第四纪含水层透射率。透射率在最小79 m(2)/天和最大814 m(2)/天之间变化,平均283 m(2)/天,标准偏差为145 m(2)/天。本文提出的简便且廉价的方法可以应用于其他半干旱地区。 (C)2016 Elsevier Ltd.保留所有权利。

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