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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >A 2.5D finite-element-modeling difference method for marine CSEM modeling in stratified anisotropic media
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A 2.5D finite-element-modeling difference method for marine CSEM modeling in stratified anisotropic media

机译:分层各向异性介质中海洋CSEM建模的2.5D有限元建模差异方法

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摘要

We have developed a 2.5D finite-element modeling (FEM) method for marine controlled-source electromagnetic (CSEM) applications in stratified anisotropic media. The main feature of the method is that delta sources are used to solve the governing partial differential equations for cases with and without a resistive target and to obtain the difference of these two solutions as the scattered field from the target. The total field is then the sum of the analytical background field calculated with a 1D modeling method and the difference or scattered field mentioned above. Compared with a conventional direct solution (using delta sources directly in a 2.5D formulation), the new method has smaller near-field error as a result of the source singularity and smaller boundary reflections. The new method does not require a dense mesh in the source region, which thereby reduces the total number of variables to be solved. In this way, the modeling time can be kept within a few minutes for some cases. We show that the maximum relative error of the calculation can be kept within 2% for targets at depths of approximately 1 km. The method is valid for stratified anisotropic media. The anisotropic modeling examples show that (1) marine CSEM is predominantly sensitive to target vertical resistivity and not to target horizontal resistivity, provided that the targets are thin, horizontal, high-resistivity layers and (2) marine CSEM is sensitive to the horizontal resistivity of the conductive sediments surrounding the target (e.g., the overburden).
机译:我们已经为分层各向异性介质中的海洋受控源电磁(CSEM)应用开发了2.5D有限元建模(FEM)方法。该方法的主要特点是,在有或没有电阻性目标的情况下,使用增量源来求解控制偏微分方程,并获得这两种解的差异作为目标的散射场。然后,总场就是通过一维建模方法计算出的分析背景场与上述差异或散射场之和。与常规直接解决方案(在2.5D公式中直接使用增量源)相比,新方法由于源奇异性和较小的边界反射而具有较小的近场误差。新方法不需要源区域中的密集网格,从而减少了要解决的变量总数。这样,在某些情况下,建模时间可以保持在几分钟之内。我们表明,对于大约1 km深度的目标,计算的最大相对误差可以保持在2%以内。该方法对分层各向异性介质有效。各向异性建模实例表明,(1)海洋CSEM主要对目标垂直电阻率敏感,而对目标水平电阻率不敏感,前提是目标是薄的,水平的,高电阻率层;(2)海洋CSEM对水平电阻率敏感围绕目标的导电沉积物(例如上覆岩层)。

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