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Fast approximate 1D modelling and inversion of transient electromagnetic data

机译:快速近似一维建模和瞬态电磁数据反演

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摘要

A novel, fast, and approximate forward modelling routine for time-domain electromagnetic responses is presented. It is based on the separation of the forward problem into a configuration-independent part, mapping conductivity as a function of depth onto apparent conductivity as a function of time, and a configuration-dependent part, i.e., the half-space step response. The response of a layered model is then found as the half-space response for a half-space conductivity equal to the apparent conductivity. The mapping is ten times faster than traditional accurate forward modelling routines, and through stochastic modelling, it is found that the standard deviation of the modelling error is 0.7%. The forward mapping lends itself to integration in a modern state-of-the-art inversion formulation in exactly the same way as traditionally computed responses, and a field example is included where inversion results using the approximate forward response are compared with those of an accurate forward response for helicopterborne transient electromagnetic data. In addition to being used in its own right in inversion of transient data, the speed and accuracy of the approximate inversion mean that it is well suited for quality control and fast turnaround data delivery of survey results to a client. It can also be used in hybrid inversion formulations by supplying initial iterations and high-quality derivatives in an inversion based on accurate forward modelling.
机译:提出了一种新颖的,快速的,近似的正时建模例程,用于时域电磁响应。它基于将前向问题分离为与构型无关的部分,将与深度有关的电导率映射到与时间有关的视在电导率以及与结构有关的部分(即半空间阶跃响应)的映射。然后发现分层模型的响应为半空间电导率等于表观电导率的半空间响应。该映射比传统的精确正向建模例程快十倍,并且通过随机建模,发现建模误差的标准偏差为0.7%。正向映射将以与传统计算响应完全相同的方式使其集成到现代最新的反演公式中,并包括一个现场示例,其中将使用近似正向响应的反演结果与精确反演结果进行比较对直升机瞬变电磁数据的正向响应。除了可以单独使用瞬态数据反演外,近似反演的速度和准确性还意味着它非常适合用于质量控制和将测量结果快速周转给客户。通过提供基于精确正向建模的反演中的初始迭代和高质量导数,它也可以用于混合反演公式中。

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  • 来源
    《Geophysical Prospecting》 |2016年第6期|1620-1631|共12页
  • 作者

    Christensen Niels B.;

  • 作者单位

    Univ Aarhus, Dept Geosci, DK-8000 Aarhus C, Denmark;

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  • 正文语种 eng
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