Maxime Gautier, Stéphanie Gautier, Rodolphe Cattin
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引用次数: 0
摘要
电阻率层析成像(ERT)是一种广泛应用于地质灾害研究、土木工程和环境修复的地球物理方法。它通过分析在地面或钻孔中收集的电数据,提供有关地下电阻率分布的信息。然而,由于其分辨率的模糊性,解释ERT图像可能是复杂的。为了解决这个问题,我们提出了一种称为PyMERRY (Python iMprovement of Electrical电阻率层析成像可靠性)的后处理方法来提高ERT图像的可靠性。PyMERRY代码可以应用于ERT反演软件获得的任何二维电阻率模型。它计算一个覆盖掩码,该掩码定义了受数据和反演过程约束的域。并对ERT模型中电阻率的不确定性进行了评价。除了灵敏度方法外,PyMERRY还为所有覆盖的电池提供低电阻率和高电阻率值。综合测试表明,该方法是有效的,并突出了电阻率对比、网格选择、电极间距和剖面长度对ERT图像可靠性的重要性。与以前的研究相比,在不丹中南部使用PyMERRY可以更准确地解释ERT图像。它证实了地形前缘逆冲的高电阻率对比,并揭示了小尺度变化的存在。
PyMERRY: a Python solution for improved interpretation of electrical resistivity tomography images
Electrical Resistivity Tomography (ERT) is a widely used geophysical method for studying geological hazards, civil engineering, and environmental remediation. It provides information about the subsurfaces resistivity distribution by analyzing electrical data collected at the surface or in boreholes. However, interpreting ERT images can be complex due to the ambiguities in their resolution. To address this issue, we propose a post-processing method called PyMERRY (for Python iMprovement of Electrical Resistivity tomography ReliabilitY) to improve the reliability of ERT images. The PyMERRY code can be applied to any 2D resistivity model obtained from ERT inversion software. It computes a coverage mask that defines the domain well-constrained by both the data and the inversion process. It also evaluates the resistivity uncertainties in the ERT models. In addition to the sensitivity approaches, PyMERRY provides low and high resistivity values for all covered cells. Synthetic tests show that the approach is efficient and highlight the importance of resistivity contrasts, mesh selection, electrode spacing, and profile length in the reliability of ERT images. Compared to previous studies, using PyMERRY in south-central Bhutan allows a more accurate interpretation of ERT images. It confirms a high resistivity contrast across the Topographic Frontal Thrust and reveals the existence of small-scale variations.
期刊介绍:
Geophysics, published by the Society of Exploration Geophysicists since 1936, is an archival journal encompassing all aspects of research, exploration, and education in applied geophysics.
Geophysics articles, generally more than 275 per year in six issues, cover the entire spectrum of geophysical methods, including seismology, potential fields, electromagnetics, and borehole measurements. Geophysics, a bimonthly, provides theoretical and mathematical tools needed to reproduce depicted work, encouraging further development and research.
Geophysics papers, drawn from industry and academia, undergo a rigorous peer-review process to validate the described methods and conclusions and ensure the highest editorial and production quality. Geophysics editors strongly encourage the use of real data, including actual case histories, to highlight current technology and tutorials to stimulate ideas. Some issues feature a section of solicited papers on a particular subject of current interest. Recent special sections focused on seismic anisotropy, subsalt exploration and development, and microseismic monitoring.
The PDF format of each Geophysics paper is the official version of record.