What is it about?
I've developed a new technique that consists of the finite-difference (FD) and finite-elements (FE) numerical technique to obtain the forward modeling response of a 3D Magnetotelluric problem. The newly developed approach is almost as fast as the pure FD and it can also represent the topographic features as easily as the FE method.
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Why is it important?
While it is easier to employ the finite-difference (FD) technique to a given problem, it is an overburden to represent a topographic feature with this numerical technique. While it is easier to represent the topographic features with the finite-elements (FE) technique, it is slower to solve the linear system arising from FE discretization. That is why, in this study, a structured mesh is picked and the some parts of the mesh are distorted to represent the topographic features. After that, the FD method is used on the non-distorted part of the mesh while the distorted parts of it are handled with the FE numerical technique. This study is the first hybrid FE-FD technique for the 3D Magnetotelluric forward modeling in frequency domain.
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This page is a summary of: A Hybrid Finite Difference Finite Element Approach for 3D Magnetotelluric Forward Modeling, June 2018, EAGE Publications,
DOI: 10.3997/2214-4609.201801208.
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