首页> 外文期刊>Near surface geophysics >Borehole effect causing artefacts in cross-borehole electrical resistivity tomography: A hydraulic fracturing case study
【24h】

Borehole effect causing artefacts in cross-borehole electrical resistivity tomography: A hydraulic fracturing case study

机译:钻孔效应导致交叉钻孔电阻率断层扫描的艺术品:液压压裂案例研究

获取原文
获取原文并翻译 | 示例
           

摘要

Electrical resistivity tomography is a technique widely used for the investigation of the structure and fluid dynamics of the shallow subsurface, particularly for hydro-geophysical purposes, sometimes using cross-borehole configurations. The results of electrical resistivity tomography inversion and their usefulness in solving hydrogeophysical problems, even though invariably limited by resolution issues, depend strongly on the accuracy of inversion, which in turn depends on a proper estimation and handling of data and model errors. Among model errors, one approximation often applied in cross-hole electrical resistivity tomography is that of neglecting the effects of boreholes and the fluids therein. Such effects inevitably impact the current and potential patterns as measured by electrodes in the boreholes themselves. In the presence of very saline fluids, in particular, this model approximation may prove inadequate and the tomographic inversion may yield images strongly contaminated by artefacts. In this paper, we present a case study where highly saline water was used for hydraulic fracturing to improve permeability of a shallow formation impacted by hydrocarbon contamination, with the final aim of improving the effectiveness ofin situcontaminant oxidation. The hydraulic fracturing was monitored via time-lapse cross-hole electrical resistivity tomography. Arrival of the saline water in the monitoring borehole likely caused a strong borehole effect that significantly affected the quality and usefulness of electrical resistivity tomography inversions. In this paper, we analyse the experimental dataset and produce, via three-dimensional electrical resistivity tomography forward modelling, a viable explanation for the observed, paradoxical field results.
机译:电阻率断层扫描是一种广泛用于调查浅层地下的结构和流体动力学的技术,特别是对于水力地球物理目的,有时使用交叉钻孔配置。电阻率断层扫描反转的结果及其在解决水文中的有用性,即使通过分辨率问题总是限制,依赖于反演的准确性,这又取决于数据和模型错误的适当估计和处理。在模型误差中,通常在交叉孔电阻率断层扫描中应用的一个近似是忽略其中钻孔和流体的影响。这种效果不可避免地影响通过钻孔本身的电极测量的电流和潜在图案。特别地,在非常盐水的存在下,特别地,该模型近似可能证明不足,断层反转可以产生由人工制品强烈污染的图像。在本文中,我们展示了一种案例研究,其中高盐水用于液压压裂,以提高碳氢化合物污染影响的浅层的渗透性,最终目的是提高不含琥珀酸氧化的有效性。通过延时交叉电阻率断层扫描监测液压压裂。盐水在监测钻孔中的到达可能导致强烈的钻孔效应,显着影响电阻率断层摄影反转的质量和有用性。在本文中,我们通过三维电阻率断层扫描前向建模分析了实验数据集并产生了观察到的矛盾场结果的可行解释。

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