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首页> 外文期刊>Journal of earth system science >Groundwater exploration in limestonea??shalea??quartzite terrain through 2D electrical resistivity tomography in Tadipatri, Anantapur district, Andhra Pradesh
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Groundwater exploration in limestonea??shalea??quartzite terrain through 2D electrical resistivity tomography in Tadipatri, Anantapur district, Andhra Pradesh

机译:LimeStonea的地下水探索?Shalea ??石英岩地形通过Tadipatri,Anantapur区,安德拉邦塔的Tadipatri

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Two-Dimensional (2D) Electrical Resistivity Tomography (ERT) survey was carried out at 11 sites within an area of $10 m{km}^{2}$ to delineate deeper potential groundwater zones in a complex geological terrain underlain by quartzite, shale and limestone formations with varied resistivity characteristics. The area is in medium rainfall zone in Tadipatri mandal of Anantapur district, Andhra Pradesh state, India. The investigation was carried out to meet the growing demands of water supply. Interpretation of the highdensity 2D resistivity dataset results revealed potential zones at only three sites in Tummalapenta, Ayyavaripalle and Guruvanipalle villages within the depth zone of 24a??124 m. A major fault zone orientedin EW direction is mapped at Tummalapenta site. Based on high resolution geophysical data interpretation and significant anomalies, four boreholes were drilled in complex, viz., limestone, shale and quartzite formations up to a maximum depth of 192 m in the area with the yield ranging from $300$ to $sim 5000$ liter per hour (lph). These four anomalous drilled borehole sites corroborates with the aquifer zone delineated through ERT technique. The aquifer parameters estimated from pumping tests show that the transmissivity varies between $sim 0.3$ and $m{179.5 m^{2}/day}$ while the storage coefficient ranges from 0.137 to 0.5 indicating large variation in aquifer characteristics of the system in a smaller area. Suitable water conservation measures were suggested for improving the groundwater condition and yield of the pumping wells.
机译:二维(2D)电阻率断层扫描(ERT)调查在11个地点的11个地点进行了10秒的地点,以便通过石英岩,页岩在复杂地质地形中描绘更深的地质地形中的更深层次的潜在地下水区。具有不同电阻率特性的石灰石形成。该地区位于印度安德拉邦州南塔帕尔区的塔迪帕特里曼达尔的中等降雨区。进行了调查,以满足供水需求不断增长。对高密度2D电阻率数据集结果的解释显示了在深度44A的深度区内的百铂坦,Ayyavaripalle和Guruvanipalle村庄仅有三个地点显示潜在区域。在Tummalapenta网站映射了一个主要的断裂区EW方向。基于高分辨率的地球物理数据解释和显着的异常,在复杂的,viz中钻出四个钻孔,在该地区的最大深度为192米的最大深度,从300美元到$ sim 5000每小时$升(洛克)。这四个异常钻孔的钻孔部位用通过ERT技术描绘的含水层区域进行了管制。从泵送测试估计的含水层参数表明,透射率在$ SIM 0.3 $和$ RM {179.5 m ^ {2} /天} $之间变化,而存储系数范围为0.137至0.5表示含水层特征的大变化系统在较小的区域。建议采取合适的水资源保护措施来改善泵送井的地下水条件和产量。

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