TEM Response of a Large Loop Source over the Multilayer Earth Models

IF 1 Q3 GEOCHEMISTRY & GEOPHYSICS
A. K. Tiwari, S. P. Maurya, N. Singh
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引用次数: 2

Abstract

The general expression of TEM response of large loop source over the layered earth models is not available in the literature for arbitrary source-receiver positions, except for the case of central loop and coincident loop configurations over the homogeneous earth model. In the present study, an attempt is made to present the TEM response of a large loop source over the layered earth model for arbitrary receiver positions. The frequency domain responses of large loop source over the layer earth model for arbitrary receiver positions are converted into the impulse (time derivative of magnetic field) TEM response using Fourier cosine or sine transform. These impulse TEM responses in turn are converted into voltage responses for arbitrary receiver positions, namely, central loop, arbitrary in-loop, and offset-loop TEM responses over the layered earth models. For checking the accuracy of the method, results are compared with the results obtained using analytical expression over a homogeneous earth model. The complete matching of both of the results suggests that the present computational technique is capable of computing TEM response of large loop source over the homogeneous earth model with high accuracy. Thereafter, the technique is applied for computation of TEM response of a large loop source over the layered earth (2-layer, 3-layer, and 4-layer) models for the central loop, in-loop, and offset-loop configurations and the results are presented in voltage decay form. The results depict their characteristic variations. These results would be useful for modeling and inversion of large loop TEM data over the layer earth models for all the possible configurations resulting from a large loop source.
多层地球模型上大环源的TEM响应
除了均匀地球模型上的中心环和重合环配置的情况外,对于任意源-接收器位置,文献中没有层状地球模型上大环源TEM响应的一般表达式。在本研究中,试图在层状地球模型上呈现任意接收器位置的大回路源的TEM响应。使用傅立叶余弦或正弦变换,将任意接收器位置的层状地球模型上的大回路源的频域响应转换为脉冲(磁场的时间导数)TEM响应。这些脉冲TEM响应依次转换为任意接收器位置的电压响应,即层状地球模型上的中心环、任意环内和偏移环TEM响应。为了检验该方法的准确性,将结果与在均质地球模型上使用解析表达式获得的结果进行了比较。这两个结果的完全匹配表明,本计算技术能够高精度地计算均匀地球模型上大环源的TEM响应。然后,将该技术应用于层状地球(2层、3层和4层)模型上大回路源的TEM响应计算,计算了中心回路、回路内和偏移回路配置的TEM响应,结果以电压衰减形式呈现。结果描述了它们的特性变化。这些结果将有助于对由大回路源产生的所有可能配置的层状地球模型上的大回路TEM数据进行建模和反演。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
International Journal of Geophysics
International Journal of Geophysics GEOCHEMISTRY & GEOPHYSICS-
CiteScore
1.50
自引率
0.00%
发文量
12
审稿时长
21 weeks
期刊介绍: International Journal of Geophysics is a peer-reviewed, Open Access journal that publishes original research articles as well as review articles in all areas of theoretical, observational, applied, and computational geophysics.
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