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An overview of geophysical technologies appropriate for characterization and monitoring at fractured-rock sites

机译:适用于压裂岩石现场表征和监测的地球物理技术概述

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摘要

Geophysical methods are used increasingly for characterization and monitoring at remediation sites in fractured-rock aquifers. The complex heterogeneity of fractured rock poses enormous challenges to groundwater remediation professionals, and new methods are needed to cost-effectively infer fracture and fracture-zone locations, orientations and properties, and to develop conceptual site models for flow and transport. Despite the potential of geophysical methods to "see" between boreholes, two issues have impeded the adoption of geophysical methods by remediation professionals. First, geophysical results are commonly only indirectly related to the properties of interest (e.g., permeability) to remediation professionals, and qualitative or quantitative interpretation is required to convert geophysical results to hydrogeologic information. Additional demonstration/evaluation projects are needed in the site remediation literature to fully transfer geophysical methods from research to practice. Second, geophysical methods are commonly viewed as inherently risky by remediation professionals. Although it is widely understood that a given method may or may not work at a particular site, the reasons are not always clear to end users of geophysical products. Synthetic modeling tools are used in research to assess the potential of a particular method to successfully image a target, but these tools are not widely used in industry. Here, we seek to advance the application of geophysical methods to solve problems facing remediation professionals with respect to fractured-rock aquifers. To this end, we (1) provide an overview of geophysical methods applied to characterization and monitoring of fractured-rock aquifers; (2) review case studies showcasing different geophysical methods; and (3) discuss best practices for method selection and rejection based on synthetic modeling and decision support tools.
机译:地球物理方法越来越多地用于表征和监测裂隙岩层含水层中的修复位置。裂隙岩的复杂非均质性给地下水修复专业人员带来了巨大挑战,因此需要新的方法来经济有效地推断裂隙和裂隙带的位置,方向和性质,并开发用于流动和运输的概念性场地模型。尽管地球物理方法有可能在井眼之间“看到”,但有两个问题阻碍了补救专业人员采用地球物理方法。首先,地球物理结果通常仅与修复专业人员感兴趣的特性(例如渗透性)间接相关,并且需要定性或定量解释才能将地球物理结果转换为水文地质信息。现场修复文献中还需要其他示范/评估项目,以将地球物理方法从研究完全转移到实践中。其次,修复专家通常认为地球物理方法具有固有的风险。尽管众所周知,给定方法可能在特定站点上起作用或可能不起作用,但对于地球物理产品的最终用户而言,原因并不总是很清楚。合成建模工具用于研究中,以评估特定方法成功成像目标的潜力,但这些工具并未在工业中广泛使用。在这里,我们寻求推进地球物理方法的应用,以解决修复专家在裂隙岩层中所面临的问题。为此,我们(1)概述了用于描述和监测裂隙含水层的地球物理方法; (2)审查案例研究,展示不同的地球物理方法; (3)讨论基于综合建模和决策支持工具的方法选择和拒绝的最佳实践。

著录项

  • 来源
    《Journal of Environmental Management》 |2017年第2期|709-720|共12页
  • 作者单位

    formerly Rutgers University Newark, now at U.S. Geological Survey, Office of Groundwater, Branch of Geophysics, Storrs, CT, USA;

    Rutgers University Newark, Department of Earth and Environmental Sciences, Rutgers University, Newark, NJ, USA;

    Rutgers University Newark, Department of Earth and Environmental Sciences, Rutgers University, Newark, NJ, USA;

    formerly Rutgers University Newark, now at U.S. Geological Survey, Office of Groundwater, Branch of Geophysics, Storrs, CT, USA;

    formerly Rutgers University Newark, now at U.S. Geological Survey, Office of Groundwater, Branch of Geophysics, Storrs, CT, USA;

    U.S. Environmental Protection Agency, Office of Research and Development, 944 E. Harmon Ave., Las Vegas, NV, USA;

  • 收录信息 美国《科学引文索引》(SCI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Fractured rock; Characterization; Geophysics; Borehole logging; Technology transfer; Remediation;

    机译:岩石破裂;表征;地球物理学;钻孔测井;技术转让;整治;

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