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A tetrahedral mesh generation approach for 3D marine controlled-source electromagnetic modeling

机译:用于3D海洋受控源电磁建模的四面体网格生成方法

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3D finite-element (FE) mesh generation is a major hurdle for marine controlled-source electromagnetic (CSEM) modeling. In this paper, we present a FE discretization operator (FEDO) that automatically converts a 3D finite difference (FD) model into reliable and efficient tetrahedral FE meshes for CSEM modeling. FEDO sets up wireframes of a background seabed model that precisely honors the seafloor topography. The wireframes are then partitioned into multiple regions. Outer regions of the wireframes are discretized with coarse tetrahedral elements whose maximum size is as large as a skin depth of the regions. We demonstrate that such coarse meshes can produce accurate FE solutions because numerical dispersion errors of tetrahedral meshes do not accumulate but oscillates. In contrast, central regions of the wireframes are discretized with fine tetrahedral elements to describe complex geology in detail. The conductivity distribution is mapped from FD to FE meshes in a volume-averaged sense. To avoid excessive mesh refinement around receivers, we introduce an effective receiver size. Major advantages of FEDO are summarized as follow. First, FEDO automatically generates reliable and economic tetrahedral FE meshes without adaptive meshing or interactive CAD workflows. Second, FEDO produces FE meshes that precisely honor the boundaries of the seafloor topography. Third, FEDO derives multiple sets of FE meshes from a given FD model. Each FE mesh is optimized for a different set of sources and receivers and is fed to a subgroup of processors on a parallel computer. This divide and conquer approach improves the parallel scalability of the FE solution. Both accuracy and effectiveness of FEDO are demonstrated with various CSEM examples.
机译:3D有限元(FE)网格生成是海洋受控源电磁(CSEM)建模的主要障碍。在本文中,我们提出了一种有限元离散化算子(FEDO),该函数可将3D有限差分(FD)模型自动转换为可靠且有效的四面体有限元网格,用于CSEM建模。 FEDO设置背景海底模型的线框,以精确地反映海底地形。然后将线框划分为多个区域。线框的外部区域被粗糙的四面体元素离散,其最大尺寸与区域的趋肤深度一样大。我们证明了这种粗糙的网格可以产生精确的有限元解,因为四面体网格的数值分散误差不会累积,而是会振荡。相反,线框的中心区域用精细的四面体元素离散化,以详细描述复杂的地质情况。电导率分布以体积平均的方式从FD网格映射到FE网格。为了避免在接收器周围进行过多的网格细化,我们引入了有效的接收器大小。 FEDO的主要优点总结如下。首先,FEDO自动生成可靠且经济的四面体FE网格,而无需自适应网格划分或交互式CAD工作流程。其次,FEDO生成的FE网格恰好符合海底地形的边界。第三,FEDO从给定的FD模型导出多组FE网格。每个FE网格针对不同的源和接收器集进行了优化,并被馈送到并行计算机上的处理器子组。这种分而治之的方法提高了有限元解决方案的并行可扩展性。 FEDO的准确性和有效性都通过各种CSEM示例得到了证明。

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