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首页> 外文期刊>Geophysical Prospecting >Electromagnetic fields generated by finite-length wire sources: comparison with point dipole solutions
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Electromagnetic fields generated by finite-length wire sources: comparison with point dipole solutions

机译:有限长度线源产生的电磁场:与点偶极子解决方案的比较

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摘要

In present-day land and marine controlled-source electromagnetic (CSEM) surveys, electromagnetic fields are commonly generated using wires that are hundreds of metres long. Nevertheless, simulations of CSEM data often approximate these sources as point dipoles. Although this is justified for sufficiently large source-receiver distances, many real surveys include frequencies and distances at which the dipole approximation is inaccurate. For ID layered media, electromagnetic (EM) fields for point dipole sources can be computed using well-known quasi-analytical solutions and fields for sources of finite length can be synthesized by superposing point dipole fields. However, the calculation of numerous point dipole fields is computationally expensive, requiring a large number of numerical integral evaluations. We combine a more efficient representation of finite-length sources in terms of components related to the wire and its end points with very general expressions for EM fields in ID layered media. We thus obtain a formulation that requires fewer numerical integrations than the superposition of dipole fields, permits source and receiver placement at any depth within the layer stack and can also easily be integrated into 3D modelling algorithms. Complex source geometries, such as wires bent due to surface obstructions, can be simulated by segmenting the wire and computing the responses for each segment separately. We first describe our finite-length wire expressions and then present ID and 3D examples of EM fields due to finite-length sources for typical land and marine survey geometries and discuss differences to point dipole fields.
机译:在当今的陆地和海洋受控源电磁(CSEM)调查中,电磁场通常是使用几百米长的电线产生的。尽管如此,CSEM数据的模拟通常将这些源近似为点偶极子。尽管这对于足够大的源接收器距离是合理的,但许多实际调查都包括偶极子近似不准确的频率和距离。对于ID分层介质,可以使用众所周知的准解析解来计算点偶极子源的电磁(EM)场,并且可以通过叠加点偶极子场来合成有限长度源的电磁场。然而,许多点偶极子场的计算在计算上是昂贵的,需要大量的数值积分评估。我们结合与导线及其端点有关的组件,将更有效的有限长度源表示与ID分层介质中EM字段的非常通用的表达方式相结合。因此,我们得到的公式所需要的数值积分比偶极子场的叠加要少,允许源和接收器放置在层堆栈内的任何深度,并且还可以轻松地集成到3D建模算法中。复杂的光源几何形状,例如由于表面障碍而弯曲的导线,可以通过对导线进行分段并分别计算每个分段的响应来进行仿真。首先,我们将描述有限长度的导线表达式,然后给出EM场的ID和3D示例(由于典型陆地和海洋测量几何的有限长度源),并讨论点偶极子场的差异。

著录项

  • 来源
    《Geophysical Prospecting》 |2011年第2期|p.361-374|共14页
  • 作者

    Rita Streich; Michael Becken;

  • 作者单位

    Potsdam University, Institute of Geosciences, Karl-Liebknecht-Str. 24, 14476 Potsdam-Golm, Germany,GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany;

    Potsdam University, Institute of Geosciences, Karl-Liebknecht-Str. 24, 14476 Potsdam-Golm, Germany,GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    electromagnetics; mathematical formulation; modelling; numerical study;

    机译:电磁学数学公式造型;数值研究;

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