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首页> 外文期刊>Journal of Applied Geophysics >Structurally coupled inversion of ERT and refraction seismic data combined with cluster-based model integration
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Structurally coupled inversion of ERT and refraction seismic data combined with cluster-based model integration

机译:结构耦合的ert和折射地震数据的反演与基于簇的模型集成相结合

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摘要

Electrical resistivity tomography (ERT) and refraction seismics are among the most frequently used geophysical methods for site-investigations and the combined results can be very helpful to fill in the gaps between the point measurements made by traditional geotechnical methods such as Cone Penetration Test (CPT), core-drilling and geophysical borehole logging. The interpretation of the results from a geophysical investigation constituting a single method often yields ambiguous results. Hence, an approach utilizing multiple techniques is often necessary. To facilitate interpretation of such a combined dataset, we propose a more controlled and objective approach and present a method for a structurally coupled inversion of 2D electrical resistivity and refraction seismic data using unstructured meshes. Mean shift clustering is used to combine the two images and to compare the separate and coupled inversion methodologies. Two synthetic examples are used to demonstrate the method, and a field-data example is included as a proof of concept. In all cases a significant improvement by the coupling is visible. The methodology can be used as a tool for improved data interpretation and for obtaining a more comprehensive and complete picture of the subsurface by combining geophysical methods. (C) 2017 Elsevier B.V. All rights reserved.
机译:电阻率断层扫描(ERT)和折射地震是现场调查的最常用的地球物理方法之一,并且组合结果可以非常有帮助填补传统地岩石方法(如锥形渗透试验)所做的点测量之间的间隙(CPT ),核心钻孔和地球物理钻孔测井。由构成单一方法的地球物理调查结果的解释通常会产生模糊的结果。因此,通常需要利用多种技术的方法。为了便于解释这种组合数据集,我们提出了一种更受控和客观的方法,并使用非结构化网格提出了一种用于结构上的2D电阻率和折射地震数据的结构耦合反转的方法。平均移位聚类用于组合两个图像并比较单独和耦合的反转方法。使用两个合成示例来证明该方法,并且存在现场数据示例作为概念证明。在所有情况下,通过耦合显着改善。该方法可以用作改进数据解释的工具,并通过组合地球物理方法来获得地下的更全面和完整的地下图像。 (c)2017 Elsevier B.v.保留所有权利。

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