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Transforming a time-domain electromagnetic signal to a frequency-domain electromagnetic response using regularization inversion

机译:使用正则化反转将时域电磁信号转换为频域电磁响应

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摘要

Wide applications of time-domain electromagnetic (TEM) data require 3D inversion. A possible strategy is to use the developed 3D inversion algorithms in frequency-domain (FD) electromagnetic (EM) methods. Thus, the key of the strategy is how to transform the time-domain (t-d) EM signal into the FD. An inversion algorithm has been developed to transform the t-d signal into a corresponding FD response. In this method, a step-off current is presumed. Under this assumption, the Fourier transform relating the EM FD response to the t-d signal becomes a sine or cosine transformation. Using the polynomial approximation method, the transformation turns into a linear equation. From a set of t-d signals, FD responses could be obtained by solving these linear equations in the least-squares sense. To reduce the nonuniqueness of the solution, and enhance the solution stability, an additional smoothness constraint on the FD response is imposed, thus converting the minimization problem into a regularization inversion problem. The algorithm is applied to synthetic and field vertical magnetic data in the in-loop TEM surveying mode. The numerical results show that in the entire audio-frequency range, the relative errors between the inversed and theoretical FD responses of the real and imaginary parts are almost all less than 1%, with the largest discrepancy of 5% occurring at high frequencies. There are two significances behind our work: First, the possibility of accurately transforming t-d response into FD response in audio-frequency range is coming into true, thereby (from the mathematical perspective) implementing the equivalence between the responses of the EM method in the time domain and the FD. Second, the algorithm provides a new approach to interpret TEM data in 3D mode by using developed 3D FEM inversion techniques.
机译:时间域电磁(TEM)数据的广泛应用需要3D反转。可能的策略是在频域(FD)电磁(EM)方法中使用开发的3D反转算法。因此,策略的关键是如何将时域(T-D)EM信号转换为FD。已经开发了一种反转算法以将T-D信号转换为相应的FD响应。在该方法中,假设降级电流。在这种假设下,将EM FD对T-D信号的响应相关的傅里​​叶变换变为正弦或余弦变换。使用多项式近似方法,变换变成了线性方程。从一组T-D信号,可以通过在最小二乘意义上求解这些线性方程来获得FD响应。为了减少解决方案的非承诺,并增强解决方案稳定性,施加了对FD响应的附加平滑约束,从而将最小化问题转换为正则化反演问题。该算法应用于环路TEM测量模式中的合成和现场垂直磁数据。数值结果表明,在整个音频范围内,实体和虚部的反转和理论FD响应之间的相对误差几乎全部小于1%,最大差异为5%,在高频时发生5%。我们的工作背后有两个意义:首先,在音频范围内将TD响应准确地转换为FD响应的可能性是真的,从而实现了在时间的时间响应之间实现等效的等效。域和FD。其次,该算法通过使用开发的3D FEM反演技术提供了一种新方法来解释3D模式中的TEM数据。

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    Jilin Univ Coll Geoexplorat Sci &

    Technol Changchun Jilin Peoples R China;

    Jilin Univ Coll Geoexplorat Sci &

    Technol Changchun Jilin Peoples R China;

    Jilin Univ Coll Geoexplorat Sci &

    Technol Changchun Jilin Peoples R China;

    Jilin Univ Coll Geoexplorat Sci &

    Technol Changchun Jilin Peoples R China;

    Jilin Univ Coll Geoexplorat Sci &

    Technol Changchun Jilin Peoples R China;

    Jilin Univ Coll Geoexplorat Sci &

    Technol Changchun Jilin Peoples R China;

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  • 正文语种 eng
  • 中图分类 地球物理学;
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