Applying of High-Resolution Geophysical Techniques for Drainage Investigations at El-Basateen Cemetery Area, Cairo, Egypt

E. Morsy, Md. Farhat Rahman Niaz, Md. Abdullah Aziz, M. Qayum, M. Hossain, S. Nihad, Md. Shahjahan Kabir
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引用次数: 1

Abstract

Due to the collapse of some cemetery in Basateen area, South of Cairo, this paper presents the application of geoelectrical resistivity sounding and imaging, as well as ground penetrating radar techniques for outlining the reasons and the presence of draining water and groundwater at the investigated area. A Vertical Electrical Sounding (VES) survey was performed at 3 points through the studied site to investigate the vertical extent of the subsurface sequence and the saturation levels. A total of 9 Dipole-Dipole imaging profiles were surveyed to determine the lateral distribution of saturation of drain water and infiltrated groundwater, and a total of 6 GPR profiles with 100- and 200- MHz antennae were surveyed to evaluate and determine the depth and the degree of saturation of the subsurface layer/s. The qualitative and quantitative interpretation of the acquired VES's and dipole-dipole imaging profiles showing easily the levels of saturations at the studied site. From the interpretation of GPR profiles, it was possible to locate and determine the saturated zones and the level of the groundwater through the area. The radar signals are penetrated enough and enabled the identification of the subsurface reflectors. The results of GPR, VES's and Resistivity imaging showed a good agreement. The integrated interpretations were verified by local geology and information from several bores. Also, the study was supported by a chemical analysis from the drain water and Ein El-Seera spring (close to studied site), to determine the main source of the drain and infiltrated water at the studied site.
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高分辨率地球物理技术在埃及开罗El-Basateen墓地地区排水调查中的应用
由于开罗南部Basateen地区的一些墓地倒塌,本文介绍了地电阻率测深和成像以及探地雷达技术的应用,以概述调查地区排水和地下水的原因和存在。垂直电测深(VES)测量在研究地点的3个点进行,以调查地下层序的垂直范围和饱和度水平。利用9条偶极子-偶极子成像剖面确定了排水和渗透地下水饱和度的横向分布;利用6条100和200 MHz天线探地雷达剖面评价和确定了地下层的深度和饱和度/s。对所获得的电磁脉冲和偶极子-偶极子成像剖面的定性和定量解释很容易显示研究地点的饱和度水平。通过探地雷达剖面的解释,可以定位和确定该地区的饱和区和地下水的水位。雷达信号被充分穿透,能够识别地下反射器。探地雷达、地震探测和电阻率成像结果吻合较好。综合解释得到了当地地质和几个钻孔资料的验证。此外,该研究还得到了排水和Ein El-Seera泉(靠近研究地点)的化学分析的支持,以确定研究地点排水和渗透水的主要来源。
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