A Generalized Multiscale Iterative Finite Element Method for Parameterized Dual-Continuum Models
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摘要: 含参双重连续介质模型在地下地层相关的多种应用建模中具有重要的理论意义与实际价值. 该模型能够有效描述地质体中高度非均质性、强对比度的多尺度结构特征,并体现出显著的不确定性. 针对此类复杂模型的数值求解,采用合适的降阶方法已成为提升计算效率与保持求解精度的关键手段. 本文针对含参双重连续介质模型,提出了一种基于广义多尺度有限元方法的迭代求解策略. 该方法首先将原始的参数依赖型双重介质模型重新表述为一个包含多尺度扩散系数和转移函数(均与参数无关)以及参数相关右端项的新模型. 在此基础上,所提出的迭代方法划分为离线与在线两个阶段. 在离线阶段,本文在每个粗网格区域内,根据确定性多尺度参数构造多尺度基函数,并生成相应的降阶空间;在在线阶段,利用构建好的降阶空间,通过迭代方法对模型进行高效求解. 该方法的显著优势在于,离线阶段构造完成后,在线阶段每次迭代均可使用高效的直接求解器,并能重复利用矩阵逆,从而显著降低计算成本. 此外,本文还给出了该迭代方法的收敛性分析. 最后,通过参数依赖的双重连续介质模型的数值算例,验证了所提出方法的有效性与计算效率,并进一步验证了理论收敛结果的正确性.
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关键词:
- 双重连续介质模型 /
- 广义多尺度有限元方法 /
- 迭代方法 /
- 不确定性量化
Abstract: The parameterized dual-continuum model plays a significant theoretical and practical role in various subsurface geological modeling applications. This model effectively captures the highly heterogeneous, high-contrast, and multiscale structural features of geological formations, while also exhibiting considerable uncertainty. To address the numerical challenges posed by such complex models, adopting appropriate model reduction techniques has become a key approach to improving computational efficiency while maintaining solution accuracy. Herein an iterative solution strategy was proposed based on the uncoupled generalized multiscale finite element method (GMsFEM) for the parameterized dual-continuum model. The original parameter-dependent model was reformulated as a new one consisting of multiscale diffusion coefficients and transfer functions (both parameter-independent), along with a parameter-dependent source term. The proposed iterative method was divided into offline and online stages. In the offline stage, multiscale basis functions were constructed in each coarse grid block based on deterministic multiscale parameters to generate a reduced-order space. In the online stage, the model was solved efficiently within the reduced space with an iterative scheme. A major advantage of this method lies in the fact that, once the multiscale basis space is constructed offline, each online iteration can leverage efficient direct solvers and reuse matrix inverses, thus significantly reducing computational costs. Furthermore, the convergence of the proposed iterative method was analyzed. Finally, numerical experiments on the parameterized dual-continuum model were conducted to demonstrate the effectiveness and efficiency of the multiscale-based iterative approach, and validate the theoretical convergence results. -
表 1 不同粗网格大小H下,变量u(x; ξ)在L2范数意义下的相对误差
Table 1. The relative L2 errors with different coarse mesh sizes H for u(x; ξ)
relative error H=1/2 H=1/4 H=1/6 H=1/8 H=1/10 H=1/12 H=1/24 eugms 6.996 8E-1 4.820 2E-1 3.099 6E-1 1.124 4E-1 2.844 9E-4 1.913 1E-4 1.208 5E-5 euGms-Iter 2.873 3E-1 2.243 0E-1 1.983 5E-1 1.615 3E-1 5.824 6E-3 6.213 6E-3 1.245 7E-3 表 2 不同粗网格大小下,变量u(x; ξ)在能量范数下的相对误差
Table 2. The relative energy errors with different coarse mesh sizes H for u(x; ξ)
relative error H=1/2 H=1/4 H=1/6 H=1/8 H=1/10 H=1/12 H=1/24 eugms 2.492 0E-1 1.662 1E-1 1.415 8E-1 1.278 9E-1 6.701 0E-4 7.189 8E-4 4.979 2E-4 euGms-Iter 2.873 9E-1 2.244 5E-1 1.985 4E-1 1.617 6E-1 6.247 9E-3 6.636 7E-3 1.675 9E-3 表 3 使用5个基函数的收敛性
Table 3. Convergences with 5 local basis functions
$\underline{\boldsymbol{\kappa}}_1^0(x)$ $\underline{\boldsymbol{\kappa}}_2^0(x)$ ep1, Gms-Iter ep2, Gms-Iter aQGms-Iter 1 1 1.747 0E101 3.970 0E105 1.644E107 3 3 3.670 3E52 9.801 2E57 4.323E59 10 10 2.409 0E-1 8.186 6E5 3.872 2E7 15 15 4.105 7E-3 1.338 5E-2 1.032E-2 20 20 2.822 0E-3 8.364 3E-3 8.832E-3 表 4 基于L2范数意义的收敛结果
Table 4. Convergences based on the L2-norm
H eugms order euGms-Iter order 1/2 6.079 4E-1 - 6.789 1 - 1/4 4.991 3E-1 0.284 5 5.535 8 0.294 4 1/8 2.991 3E-2 2.172 5 2.577 4E-2 4.020 6 1/16 2.366 1E-5 4.883 0 4.999 8E-3 3.469 0 1/32 4.960 3E-6 4.225 8 5.509 3E-3 2.566 8 表 5 基于能量范数意义的收敛结果
Table 5. Convergences based on the energy norm
H eugms order euGms-Iter order 1/2 6.648 8E-1 - 6.650 4E-1 - 1/4 5.821 0E-1 0.191 8 5.823 0E-1 0.191 7 1/8 5.419 5E-2 1.743 9 5.465 2E-2 3.478 4 1/16 3.546 3E-3 2.516 9 4.017 8E-3 2.457 0 1/32 1.680 7E-3 2.157 0 2.152 8E-3 2.067 8 -
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