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FAST RESISTIVITY IP INVERSION USING A LOW-CONTRAST APPROXIMATION

机译:低对比度近似的快速电阻率IP转换

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By computing only the diagonal terms of the volume integral equation forward solution of the 3-D DC resistivity problem, we have achieved a fast forward solution accurate at low to moderate resistivity contrasts. The speed and accuracy of the solution make it practical for use in 2-D or 3-D inversion algorithms. The low-contrast approximation is particularly well-suited to the smooth nature of minimum structure inversion, since complete forward solutions may be computationally expensive. By using this approximate 3-D solution as the forward model in an inversion algorithm, and by constraining the resistivities and polarizabilities along any row of cells in the strike direction to be held constant, we effect a fast 2-D resistivity inversion that contains end corrections. Because the low-contrast solution is inaccurate for cells near the electrodes, we employ a full solution to compute the response of the near-surface when the nearsurface environment is substantially different from the host rock. This response is stored and used in the iterative resistivity inversion in conjunction with the approximate solution. Once an adequate estimated resistivity model has been found, derivatives from this model are used with Seigel's formula to compute the inverse solution to the linear polarizability problem in a single iteration. [References: 17]
机译:通过仅计算3-D DC电阻率问题的体积积分方程正解的对角项,我们获得了在中低电阻率对比下准确的快速正解。该解决方案的速度和准确性使其可用于2D或3D反演算法。低对比度逼近特别适合于最小结构反转的平滑特性,因为完整的前向解在计算上可能会很昂贵。通过将这种近似的3-D解用作反演算法中的正向模型,并通过将沿罢工方向上任何单元格的电阻率和极化率约束为恒定,我们实现了包含端部的快速2-D电阻率反演更正。由于低对比度解决方案对于电极附近的单元格来说是不准确的,因此当近地表环境与宿主岩石存在显着差异时,我们采用完整解决方案来计算近地表的响应。存储该响应,并与近似解一起用于迭代电阻率反演。一旦找到了足够的估计电阻率模型,就可以将该模型的导数与Seigel公式一起使用,以在一次迭代中计算线性极化率问题的逆解。 [参考:17]

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