A matrix-free reformulation of the multi-parameter descent and conjugate-gradient method for isotropic elastic iterative reverse-time migration

W. Mulder
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Abstract

Multi-parameter inversion of linear systems appears in many problems. The focus here is on isotropic elastic iterative reverse-time migration for three position-dependent subsurface model parameters, which amounts to data fitting of processed seismic data with synthetics from the Born approximation of the elastic wave equation. In that case, the matrix of the linear system is the hessian. As it is impractical to form, a matrix-free formulation is needed, which is readily derived for the gradient descent method. For single-parameter inversion, the conjugate-gradient (CG) method is generally more efficient than simple descent. However, the multiple-parameter CG method has a significantly higher cost than the descent method. Here, first a matrix-free data-domain reformulation is derived. Then, its performance is compared to the simple descent method to see of its faster convergence justifies the higher cost. A comparison on a marine 2-D toy problem with a salt body and sea-bottom receivers shows that the multiple-parameter descent method wins in terms of efficiency if the number of iterations is limited and that the single-parameter CG method is even faster.
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各向同性弹性迭代逆时偏移的无矩阵多参数下降和共轭梯度法
线性系统的多参数反演出现在许多问题中。本文的重点是三个位置相关地下模型参数的各向同性弹性迭代逆时偏移,这相当于将处理过的地震数据与弹性波动方程的Born近似合成的数据拟合。在这种情况下,线性系统的矩阵就是黑森矩阵。由于不实际的形成,需要一个无矩阵的公式,这是很容易导出的梯度下降法。对于单参数反演,共轭梯度法(CG)通常比简单下降法更有效。然而,与下降法相比,多参数CG法的代价要高得多。在这里,首先推导了一个无矩阵的数据域重构公式。然后,将其性能与简单下降法进行比较,以证明其更快的收敛速度证明了较高的成本是合理的。对含盐体和海底接收机的海洋二维玩具问题进行了比较,结果表明,在迭代次数有限的情况下,多参数下降法的求解效率更高,单参数CG法的求解速度更快。
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