首页> 外文期刊>Current Science: A Fortnightly Journal of Research >Field evaluation of 3D geo-electrical resistivity imaging for environmental and engineering studies using parallel 2D profiles
【24h】

Field evaluation of 3D geo-electrical resistivity imaging for environmental and engineering studies using parallel 2D profiles

机译:使用并行2D轮廓对环境和工程研究进行3D地电阻率成像的现场评估

获取原文
获取原文并翻译 | 示例
       

摘要

Eight parallel two-dimensional (2D) geo-electrical resistivity profiles were generated in hard-rock (Pulivendla) area of Andhra Pradesh, India using a Lund imaging multi-electrode system adopting Wenner array. The aim of the survey was to experimentally evaluate the effectiveness of using parallel 2D profiles for three-dimensional (3D) geo-electrical resistivity imaging for better understanding of aquifer geometry and its characteristics. The observed 2D apparent resistivity data were independently inverted, and then collated to 3D data set. The inversion of the resulting 3D data set was carried out using a full 3D inversion code. The 3D inverse model of resistivity images obtained are presented as horizontal depth slices. The 2D images extracted from 3D inverse models showed no distortions that are observed in 2D models obtained by 2D inversion. The 3D inverse model resistivity appears to be more realistic, considering the hydrogeology of the area. The unusually high resistivity values observed in the 2D inverse models were not observed in the 3D inverse models. The very low near-surface inverse model resistivity observed is thought to be structurally influenced. The results, which are consistent with numerical evaluation, show that high resolution 3D geoelectrical resistivity imaging can be successfully conducted using parallel 2D profiles if appropriate survey parameters are carefully chosen.
机译:使用采用Wenner阵列的隆德成像多电极系统,在印度安得拉邦的硬岩(Pulivendla)地区生成了八个平行的二维(2D)地电电阻率曲线。该调查的目的是通过实验评估将并行2D轮廓用于三维(3D)地电电阻率成像的效果,以更好地了解含水层的几何形状及其特征。将观察到的2D表观电阻率数据独立地反转,然后整理为3D数据集。使用完整的3D反转代码对生成的3D数据集进行反转。所获得的电阻率图像的3D逆模型表示为水平深度切片。从3D逆模型提取的2D图像未显示在通过2D反演获得的2D模型中观察到的失真。考虑到该地区的水文地质学,3D反演模型的电阻率似乎更为现实。在2D逆模型中未观察到异常高的电阻率值,而在3D逆模型中未观察到。观察到的极低的近地表反演模型电阻率在结构上受到影响。结果与数值评估一致,表明如果仔细选择合适的测量参数,则可以使用平行2D轮廓成功进行高分辨率3D地电阻率成像。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号