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首页> 外文期刊>Computers & geosciences >EMDPLER: A F77 program for modeling the EM response of dipolar sources over the non-magnetic layer earth models
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EMDPLER: A F77 program for modeling the EM response of dipolar sources over the non-magnetic layer earth models

机译:EMDPLER:一个F77程序,用于在非磁性层地球模型上对偶极源的EM响应进行建模

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摘要

A program EMDPLER coded in FORTRAN 77 is presented for modeling the electromagnetic (EM) response of a wide class of dipolar sources (namely, vertical magnetic dipole, horizontal magnetic dipole and horizontal electric dipole) over the layered earth model in induction (f≤ 50 kHz) as well as higher frequency (50 kHz ≤f≤ 1000 kHz) regions. The program is based on a semi-analytical numerical approach for evaluating infinite integrals occurring in the expressions of EM field components. It is capable of computing the EM response with or without the displacement current factor for any arbitrary position of source and/or receiver either in air or on the surface of the model due to all the conventional EM dipole sources where other available algorithms fail due to one or other reasons. The program is well documented, easy to understand and amenable to modification for the user's specification. The validity and accuracy of the program is demonstrated by computing the EM response of dipolar sources over homogeneous and multi-layer earth models, and comparing the computed results with those of published results in the literature. Response curves depict their characteristic variations. The computed results match very well with the published results for the induction region (f≤ 50 kHz) and are extension of their characteristic variation in the higher frequency (50kHz≤f≤ 1000 kHz) region. The matching of computed results with the published results illustrates the validity of the program.
机译:提出了用FORTRAN 77编码的EMDPLER程序,用于在感应(f≤50)的层状地球模型上对多种偶极子源(即垂直磁偶极子,水平磁偶极子和水平电偶极子)的电磁(EM)响应进行建模。 kHz)以及更高频率(50 kHz≤f≤1000 kHz)的区域。该程序基于半解析数值方法,用于评估EM场分量表达式中出现的无限积分。由于所有常规的EM偶极子源,而其他可用算法由于以下原因而失效,因此它能够在源或接收器在空气中或模型表面上的任意位置上计算带有或不带有位移电流因数的EM响应。一个或其他原因。该程序文档齐全,易于理解,并可以根据用户要求进行修改。通过在均匀和多层地球模型上计算偶极子源的电磁响应,并将计算结果与文献中已发表的结果进行比较,证明了该程序的有效性和准确性。响应曲线描述了它们的特征变化。计算结果与感应区域(f≤50 kHz)的已发布结果非常吻合,并且是它们在较高频率(50kHz≤f≤1000 kHz)区域中特性变化的扩展。计算结果与已发布结果的匹配说明了该程序的有效性。

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