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Rapid frequency domain three-dimensional electromagnetic forward modeling and inversion.

机译:快速频域三维电磁正演建模与反演。

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摘要

The future perspective in electromagnetic (EM) geophysical methods lies in the development of multitransmitter and multireceiver methods. Interpretation of massive electromagnetic data sets is impossible without efficient computerized modeling and inversion capable of handling inhomogeneous three dimensional geological structures. The mathematical complexity and computational cost of the three-dimensional (3-D) EM problems currently prevents extensive use of these methods. The goal of this dissertation is to develop rapid integral-based forward modeling and inversion algorithms to produce geologically meaningful models using limited computer resources.; First, I consider quick, reasonably accurate integral approximations for the solution of the EM forward problem. A new family of approximations based on the quasi-analytical (QA) technique are proposed as a combination of existing approximations, providing not only a fast forward modeling tool, but also a rapid inversion scheme as well.; Accurate EM forward modeling is one of the most difficult and time consuming problems in computational geophysics. In Chapter 3, the solution of the electromagnetic integral equation using iterative schemes is discussed. I introduce the contraction integral equation method, which leads to a new set of diagonal preconditioners. These preconditioners speed up the solution many fold.; The ultimate goal in exploration geophysics is the reconstruction of underground geological structures by inversion of the measured data. In Chapter 4 the aspects of 3-D electromagnetic inversion based on the diagonalized quasi-analytical (DQA) method are studied. The DQA approach provides an extremely fast algorithm enabling practitioners with no supercomputer access to perform inversions on large models and data sets almost interactively. The DQA approach is applied to the inversion of massive synthetic and real data sets. The inversion results show that the method is fast and efficient.
机译:电磁地球物理方法的未来前景在于多发射器和多接收器方法的发展。没有有效的计算机化建模和能够处理非均匀三维地质结构的反演,就不可能解释大量的电磁数据集。三维(3-D)EM问题的数学复杂性和计算成本目前阻止了这些方法的广泛使用。本文的目的是开发基于积分的快速前向建模和反演算法,以利用有限的计算机资源生成具有地质意义的模型。首先,我考虑了用于解决EM正向问题的快速,合理准确的积分近似方法。提出了一种基于拟分析(QA)技术的新的近似族,它是现有近似的组合,不仅提供了快速前向建模工具,而且还提供了快速反演方案。精确的EM正演模型是计算地球物理学中最困难,最耗时的问题之一。在第三章中,讨论了使用迭代方案求解电磁积分方程。我介绍了收缩积分方程方法,这产生了一组新的对角前置条件。这些预处理器可将解决方案加快很多倍。勘探地球物理学的最终目标是通过反演测量数据来重建地下地质结构。在第四章中,研究了基于对角准分析(DQA)方法的3-D电磁反演的各个方面。 DQA方法提供了一种非常快速的算法,使没有超级计算机访问权限的从业人员几乎可以交互地对大型模型和数据集执行反演。 DQA方法适用于海量综合和真实数据集的反演。反演结果表明该方法是快速有效的。

著录项

  • 作者

    Hursan, Gabor.;

  • 作者单位

    The University of Utah.;

  • 授予单位 The University of Utah.;
  • 学科 Geophysics.
  • 学位 Ph.D.
  • 年度 2001
  • 页码 137 p.
  • 总页数 137
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球物理学;
  • 关键词

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