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    基于迭代求解的储层时移大地电磁法三维有限元正演研究

    Iterative finite element solution for three-dimensional time-lapse magnetotelluric forward modeling of reservoir structures

    • 摘要: 储层时移大地电磁(MT)监测需要对同一区域在不同开发阶段反复进行三维正演计算,模型规模大、频率点多,传统基于LU分解等直接求解器的矢量有限元方法内存消耗随自由度急剧增长,难以满足大规模时移正演的实际需求。针对这一问题,采用灵活广义最小残差法(FGMRES)作为外层迭代求解器,结合辅助空间Maxwell求解器(AMS)替代直接求解器。将复系数线性方程组拆分为等价的实数对称形式,构造2×2分块对角预条件矩阵,内层利用AMS对每个实对称子块进行预条件求解,有效加速了Krylov子空间的收敛。通过层状模型验证了算法的正确性,视电阻率和相位与一维解析解吻合良好;在含储层时移电阻率异常体的三维模型中,所有频率均在20次迭代内收敛,求解结果与PARDISO直接解的视电阻率与相位响应特征一致,峰值内存降低约60%。结果表明,该迭代求解方案在保证计算精度的前提下显著降低了内存消耗,能够支撑多期次重复正演的计算需求,为大规模储层时移大地电磁三维正演提供了高效可行的技术途径。

       

      Abstract: Time-lapse magnetotelluric (MT) monitoring of reservoirs requires repeated three-dimensional (3D) forward modeling over the same region at different development stages. Due to the large model size and the large number of frequencies involved, conventional vector finite element methods based on direct solvers such as LU decomposition suffer from memory consumption that grows rapidly with the number of degrees of freedom, making them impractical for large-scale time-lapse forward modeling. To address this issue, we employ the flexible generalized minimum residual method (FGMRES) as the outer iterative solver, combined with an auxiliary-space Maxwell solver (AMS) preconditioner to replace the direct solver. The complex-valued linear system is reformulated into an equivalent real-valued symmetric form, and a 2×2 block-diagonal preconditioner is constructed, in which AMS is applied to each real symmetric sub-block as the inner preconditioner, effectively accelerating the convergence of the Krylov subspace iteration. The algorithm is first validated against a layered model, where the apparent resistivity and phase show good agreement with the 1-D analytical solution. For a 3-D model containing a time-lapse resistivity anomaly representing a reservoir, convergence is achieved within 20 iterations at all frequencies, and the iterative results exhibit consistent apparent-resistivity and phase responses with those of the PARDISO direct solver, while peak memory usage is reduced by approximately 60%. These results demonstrate that the proposed iterative solution scheme significantly reduces memory consumption without compromising accuracy, and is capable of supporting the computational demands of multi-vintage repeated forward modeling, thus providing an efficient and viable approach for large-scale 3D time-lapse MT forward modeling of reservoirs.

       

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