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首页> 外文期刊>Journal of Applied Geophysics >Integrated resistivity surveys for delineation of fractures for ground water exploration in hard rock areas
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Integrated resistivity surveys for delineation of fractures for ground water exploration in hard rock areas

机译:综合电阻率调查,用于确定硬岩地区地下水勘探中的裂缝

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Acute shortage of ground water in hard rock areas is well known. Ground water occurs in limited areal extent in secondary porosity generally developed due to weathering, fracturing, jointing, faulting etc. within the hard rock formations. These structural changes (fractures etc.) are sparsely distributed in the hard rock areas. Gradient profiling followed by geoelectrical sounding has been successfully utilized to delineate fractures saturated with water in hard rock areas of Gurudev Nagar, Mirzapur District, India. To begin with, the Gradient profiling (GP) survey was conducted along nine profiles with fixed current electrodes separation of 600 m and different potential electrodes separations for all the points lying between central region of the profile (about 33% of the total spread) at a station interval of 5 m. Eventually a comparative study of Wenner profiling and Gradient profiling along a specific profile line exhibits superiority of later over former. Based on the analyses of the response of GP survey, eleven prominent 'low' resistive points were selected. Geoelectrical sounding (GS) survey was then carried out at these locations. The interpreted sounding results show presence of fractured to highly-fractured sandstone. A test bore hole drilled at one of the locations yields a continuous discharge of ground water over 20,000 1/h. Present study clearly demonstrates that the GP survey is a powerful initial technique to identify the presence of fractures in hard rock areas and subsequent application of geoelectrical sounding at selected locations is very helpful for quantitative investigations. (C) 2007 Elsevier B.V. All rights reserved.
机译:硬岩地区的地下水严重短缺是众所周知的。由于硬岩层内的风化,压裂,节理,断层等原因,地下水在有限的区域范围内发生,通常在次生孔隙中发育。这些结构变化(裂缝等)稀疏分布在硬岩区域。在印度米尔扎普尔地区古鲁杰夫·纳加尔的硬岩地区,梯度剖面法和地电测深法已成功地用于描述含水饱和的裂缝。首先,沿着9个剖面进行了梯度剖面(GP)调查,其中固定电流电极的间距为600 m,位于剖面中心区域之间的所有点(总展宽的33%)的所有点的电位电极间距都不同。站点间隔为5 m。最终,沿着特定轮廓线对Wenner轮廓和Gradient轮廓进行的比较研究显示出后者优于前者的优势。在对GP调查的答复进行分析的基础上,选择了11个突出的“低”电阻点。然后在这些位置进行了地电探测(GS)调查。解释的测深结果表明存在破裂至高度破裂的砂岩。在其中一个位置上钻一个测试孔可以连续排放超过20,000 1 / h的地下水。当前的研究清楚地表明,GP勘测是一种确定硬岩区域是否存在裂缝的强大的初始技术,随后在选定位置应用地电测深对定量研究非常有帮助。 (C)2007 Elsevier B.V.保留所有权利。

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