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首页> 外文期刊>Journal of Applied Geophysics >A fast forward algorithm for three-dimensional magnetic anomaly on undulating terrain
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A fast forward algorithm for three-dimensional magnetic anomaly on undulating terrain

机译:起伏地形三维磁异常的快速前进算法

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This paper presents a fast and high-precision three-dimensional magnetic anomaly forward algorithm on undulating terrain. Firslty, The forward algorithm for three-dimensional magnetic anomalies on a horizontal observation surface is developed with the Block-Toeplitz-Toeplitz-Block (BTTB) matrix. In the proposed algorithm, the cuboid elements are used to divide the underground space. And the position of the observation point is set as the projection of the central point of the cuboid element onto the observation surface. With the symmetry of the BTTB matrix, the coefficient matrix is compressed and stored to reduces the memory requirements during the computation process. In order to deal with the coefficient matrix and parameter vector computations, the matrix cross-multiplication computation is transformed into a point-multiplication computation with the fast Fourier transform (FFT) method. Then, to solve the problem of undulating terrain, a hierarchical interpolation method is proposed in forward algorithm, in which the undulating terrain is divided into several horizontal observation surfaces. Subsequently, the magnetic field on the undulating terrain is interpolated. Some 3D models with horizontal observation surface and undulating terrain are tested to verify the proposed algorithm. The results show that the forward algorithm has the advantages of fast computation speed, high precision, and low memory requirement. It is suitable for large-scale (ten millions of nodes) three-dimensional magnetic forward modeling. (C) 2019 Elsevier B.V. All rights reserved.
机译:本文介绍了起伏地形上快速高精度的三维磁异常前进算法。 FiRSLTY,用块 - Toplitz-Toeplitz-块(BTTB)矩阵显影了水平观察表面上的三维磁异常的前向算法。在所提出的算法中,长方体元件用于划分地下空间。观察点的位置被设定为长方体元件的中心点在观察表面上的投影。利用BTTB矩阵的对称性,压缩系数矩阵并存储以在计算过程期间降低存储器要求。为了处理系数矩阵和参数向量计算,将矩阵交叉乘法计算转换为具有快速傅里叶变换(FFT)方法的点乘法计算。然后,为了解决波浪状地形的问题,在向前算法中提出了一种分层插值方法,其中起伏的地形被分成几个水平观察表面。随后,内插的波状地形上的磁场。测试具有水平观察表面和起伏地形的一些3D模型以验证所提出的算法。结果表明,前进算法具有快速计算速度,高精度和低内存要求的优点。它适用于大规模(10万节节点)三维磁头建模。 (c)2019年Elsevier B.V.保留所有权利。

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