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首页> 外文期刊>Computers & geosciences >Note on: 'EMDPLER: A F77 program for modeling the EM response of dipolar sources over the non-magnetic layer earth models' by NP Singh and T. Mogi, Computers & Geosciences 36 (2010) 430-440
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Note on: 'EMDPLER: A F77 program for modeling the EM response of dipolar sources over the non-magnetic layer earth models' by NP Singh and T. Mogi, Computers & Geosciences 36 (2010) 430-440

机译:关于“ EMDPLER:F77程序,用于在非磁性层地球模型上对偶极子源的EM响应进行建模的F77程序”,NP Singh和T. Mogi,计算机与地球科学36(2010)430-440

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In this paper some mistakes arising in Singh and Mogi (2010) that are: (1) wrong formulation of the intrinsic impedance of the layers of an N-layered earth (Z(i)) and reflection coefficient of the EM wave in TM-mode (r(TM)), (2) using wrong and the very same algorithms for computing reflection coefficients of the EM wave in both the TE- and the TM-mode (r(TE) and r(TM)) and (3) using flawed algorithms for computing phase and normalized phase values, relating to electric and magnetic components of the EM wave, are noted and corrected form of these mistakes are presented. Moreover, in order to illustrate how these mistakes can affect forward modeling results different two- and three-layered earth models, the same as the models used in Singh and Mogi (2010), are chosen; afterwards EMDPLER and corrected version of this program, presented in this paper titled "EMDPLER_Corr", are conducted on these models and real and imaginary parts of H-z and H-y components of the magnetic field intensity, their normalized amplitudes (vertical bar H-z/H-z0 vertical bar and vertical bar H-y/H-y0 vertical bar) and the corresponding normalized phases are computed, plotted versus frequency and compared with each other. (C) 2016 Elsevier Ltd. All rights reserved.
机译:在本文中,Singh和Mogi(2010)出现了一些错误,这些错误是:(1)N-层地球层的固有阻抗(Z(i))和EM波在TM-中的反射系数的错误公式模式(r(TM)),(2)使用错误的和非常相同的算法来计算TE和TM模式(r(TE)和r(TM))中的EM波的反射系数,以及(3 )使用有缺陷的算法来计算与EM波的电磁分量有关的相位和归一化相位值,并给出这些错误的纠正形式。此外,为了说明这些错误如何影响正向建模结果,选择了与Singh和Mogi(2010)中使用的模型相同的两层和三层地球模型;之后,对这些模型以及磁场强度的Hz和Hy分量的实部和虚部,它们的归一化幅度(垂直线Hz / H-z0)进行EMDPLER和此程序的更正版本(本文以“ EMDPLER_Corr”表示)垂直条和垂直条(Hy / H-y0垂直条)以及相应的归一化相位进行计算,绘制频率曲线并相互比较。 (C)2016 Elsevier Ltd.保留所有权利。

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