Integrated electromagnetic survey for groundwater exploration: case study at El-Minya, western desert of Egypt

G. El-Qady, H. Shaaban, M. Abdel Zaher, M. Atya
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Abstract

ABSTRACT The determination of groundwater potentiality is one of the most significant challenges in hydro-geophysical research, especially in arid areas with limited water resources. A geophysical survey was carried out in the northwest of El-Minya Governorate to investigate the groundwater aquifer. A total of 20 controlled source audio-magnetotelluric (CSAMT) and 20 time domain electromagnetic soundings (TEM) were surveyed along two parallel profiles with station spacing varying between 500 and 2000 m. The CSAMT data was acquired using a hybrid source of low frequency band (0.1 Hz – 1 KHz) and standard high frequency band (10 Hz- 100 KHz). For the TEM survey, a coincident loop of side length of 50 m was used. The results of the integrated interpretation of both data sets (TEM and CSAMT) show a good consistency in the conductivity distribution. However, inspection of the results of the cross section indicates that two to three geoelectrical layers can be recognised in the subsurface medium. The area’s water potentiality is divided into two levels: the first begins immediately beneath the rock cap at depths of over 50 m and reaches nearly 200 m in some spots. The second level begins at a depth of 250 m and continues to a depth of 500 m.
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地下水勘探综合电磁测量:以埃及西部沙漠El-Minya为例
地下水潜力的确定是水文地球物理研究中最重要的挑战之一,特别是在水资源有限的干旱地区。在明亚省西北部进行了一项地球物理调查,以调查地下水含水层。在500 ~ 2000 m的平行剖面上,共测量了20个可控源音频大地电磁测深(CSAMT)和20个时域电磁测深(TEM)。CSAMT数据采用低频(0.1 Hz- 1 KHz)和标准高频(10 Hz- 100 KHz)混合源获取。瞬变电磁法测量采用边长为50 m的重合环路。两组数据(TEM和CSAMT)的综合解释结果显示电导率分布具有良好的一致性。然而,对断面结果的检查表明,在地下介质中可以识别出两到三个地电层。该地区的水势分为两个层次:第一级始于岩石帽下,深度超过50米,在某些地方达到近200米。第二层从250米深开始,一直持续到500米深。
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