首页> 外文会议>Progress in electromagnetics research symposium 2005 (PIERS 2005) >Numerical Modeling on Transient Electromagnetic Responses of a 3-D Electric Dipole Source on 2-D Plarizable Earth Surface
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Numerical Modeling on Transient Electromagnetic Responses of a 3-D Electric Dipole Source on 2-D Plarizable Earth Surface

机译:2-D可极化地球表面上3-D电偶极子源瞬态电磁响应的数值模型

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Numerical modeling on transient electromagnetic responses of a 3-D electric dipole source on 2-D earth model is an important basic work in computation geophysics. In electromagnetic method of the geophysical exploration,when the dipole-dipole array is used, and response on the polarizable earth surface is studied in time domain,it is called time spectral resistivity method (TSR). In this paper,2. 5-dimensional numerical algorithm for TSR is established,whose characters are as following: (1) A 2-D finite element method is adopted in which two diagonal lines are increased in each rectangular net to form triangular networks. Unknown variable at central node of the rectangular net is eliminated by the Gauss elimination. So complex 2-D geoelectric section can be modeled more exactly but computation quantity is much less than that in rectangular network. (2) A new algorithm of computing secondary field directly is founded,which only needs computing two components of electric and magnetic primary field. Not only the computation accuracy is high,but also the computation time is not increasing much. (3) The new G-S inverse Laplace transform method based on the delay theorem of Laplace transform is used for the rapid calculation of the transient electromagnetic response with dense samples. (4) The algorithm can be used for computing the transient electromagnetic response on the conductive and polarizable earth.
机译:在二维地球模型上对三维电偶极子源的瞬态电磁响应进行数值建模是计算地球物理学的重要基础工作。在地球物理勘探的电磁方法中,当使用偶极子-偶极子阵列,并在时域研究极化极化表面上的响应时,称为时谱电阻率法(TSR)。本文2。建立了TSR的5维数值算法,其特征如下:(1)采用二维有限元法,在每个矩形网中增加两条对角线,形成三角形网络。矩形网中心节点的未知变量通过高斯消去法消除。因此,复杂的二维地电断面可以更精确地建模,但是计算量却比矩形网络少得多。 (2)建立了直接计算次级磁场的新算法,该算法只需要计算电场和磁场的两个分量。不仅计算精度高,而且计算时间也没有增加太多。 (3)基于拉普拉斯变换的延迟定理的新的G-S逆拉普拉斯变换方法被用于快速计算密集样本的瞬态电磁响应。 (4)该算法可用于计算导电和可极化地球上的瞬态电磁响应。

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