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首页> 外文期刊>Journal of earth system science >Groundwater prospecting by the inversion of cumulative data of Wennera??Schlumberger and dipolea??dipole arrays: A case study at Turamdih, Jharkhand, India
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Groundwater prospecting by the inversion of cumulative data of Wennera??Schlumberger and dipolea??dipole arrays: A case study at Turamdih, Jharkhand, India

机译:通过Wennera,Schlumberger和dipolea,偶极子阵列的累积数据反演进行地下水勘探:以印度贾坎德邦图拉姆迪为例

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The present study deals with groundwater prospecting in hardrock terrain. Initially, the Wennera??Schlumberger array and the dipolea??dipole array data have been acquired using Syscal Junior Switch-48. Furthermore, data acquired using both arrays have been merged using Prosys-II data handling software for the inversion of the cumulative data for possible mapping of water-bearing fracture rock masses with different structural distribution in a complex geological environment. The data have been analysed using RES2DINV software, based on the smoothness constrained least-square technique. Two numbers of 2D electrical resistivity tomography profiles (AA$^{prime}$ and BB$^{prime}$) have been selected over an official colony of the Turamdih uranium mine for groundwater prospecting, which is located at about 24 km west of Jaduguda, Jharkhand, India. High-resistivity features associated with a dyke-like structure have been delineated in both the profiles. Three low-resistivity features have been delineated as water saturated alluvium/aquifers in profile AA$^{prime}$. A low-resistivity feature associated with the water-saturated fracture zone has been identified in profile BB$^{prime}$, which is well correlated with the surficial location of an ephemeral channel at the bottom of the hill across the slope. It is observed that geoelectric sections generated by the inversion of cumulative data of both arrays provide superior results compared with the Wennera??Schlumberger and dipolea??dipole arrays, separately.
机译:本研究涉及硬岩地形中的地下水勘探。最初,使用Syscal Junior Switch-48获得了Wennera ?? Schlumberger阵列和偶极子??偶极子阵列数据。此外,使用Prosys-II数据处理软件合并了使用两个阵列获取的数据,以对累积数据进行反演,以便在复杂的地质环境中对具有不同结构分布的含水裂隙岩体进行可能的测绘。基于平滑度受约束的最小二乘法,使用RES2DINV软件对数据进行了分析。在Turamdih铀矿的官方殖民地上选择了两个数量较大的2D电阻断层扫描剖面图(AA $ ^ { prime} $和BB $ ^ { prime} $),用于探矿,该矿区位于约24 km印度贾坎德邦Jaduguda西部。在两个剖面中都描绘了与堤状结构相关的高电阻率特征。在剖面AA $ ^ { prime} $中,水饱和的冲积层/含水层被描述为三个低电阻率特征。在剖面BB $ ^ { prime} $中已确定了与水饱和裂缝带相关的低电阻率特征,该特征与跨斜坡的山底底部临时通道的表面位置高度相关。观察到,与分别由Wennera,Schlumberger和dipolea,dipole阵列相比,由两个阵列的累积数据反演产生的地电断面提供了更好的结果。

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