Convolutional surrogate for 3D discrete fracture–matrix tensor upscaling

IF 4.4 2区 地球科学 Q1 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS
Computers & Geosciences Pub Date : 2026-03-01 Epub Date: 2026-01-14 DOI:10.1016/j.cageo.2026.106105
Martin Špetlík, Jan Březina
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引用次数: 0

Abstract

Modeling groundwater flow in three-dimensional fractured crystalline media requires capturing the spatial heterogeneity introduced by fractures. Direct numerical simulations using fine-scale discrete fracture–matrix (DFM) models are computationally demanding, particularly when repeated evaluations are needed. We aim to use a multilevel Monte Carlo (MLMC) method in the future to reduce computational cost while retaining accuracy. When transitioning between accuracy levels, numerical homogenization is used to upscale the impact of the hydraulic conductivity of sub-resolution fractures. To reduce the computational cost of conventional 3D numerical homogenization, we develop a surrogate model that predicts the equivalent hydraulic conductivity tensor, Keq, from a voxelized 3D domain representing a tensor-valued random field of matrix and fracture hydraulic conductivities. Fracture properties, including size, orientation, and aperture, are sampled from distributions informed by natural observations. The surrogate architecture combines a 3D convolutional neural network with feed-forward layers to capture both local spatial patterns and global interactions. Three surrogates are trained on data generated by discrete fracture–matrix (DFM) simulations, each corresponding to a different fracture-to-matrix conductivity ratio. Their performance is evaluated across varying fracture network parameters and correlation lengths of the matrix field. The trained surrogates achieve high prediction accuracy (NRMSE<0.22) in a wide range of test scenarios. To demonstrate practical applicability, we compare conductivities upscaled by numerical homogenization and by our surrogates in two macro-scale problems: computation of equivalent tensors of hydraulic conductivity and prediction of outflow from a constrained 3D area. In both cases, the surrogate-based approach preserves accuracy while substantially reducing computational cost. Surrogate-based upscaling achieves speedups exceeding 100× when inference is performed on a GPU.
三维离散裂缝矩阵张量升级的卷积代理
在三维裂隙晶体介质中模拟地下水流动需要捕捉裂缝引入的空间非均质性。使用精细尺度离散裂缝矩阵(DFM)模型进行直接数值模拟需要大量的计算量,特别是在需要重复评估的情况下。我们的目标是在未来使用多层蒙特卡罗(MLMC)方法来降低计算成本,同时保持准确性。在精度等级之间转换时,采用数值均质化方法提高了亚分辨率裂缝水力导流性的影响。为了降低传统三维数值均匀化的计算成本,我们开发了一个代理模型,从代表矩阵和裂缝水力导度的张量值随机场的体素化三维域预测等效水力导率张量Keq。裂缝性质,包括尺寸、方向和孔径,都是从自然观测的分布中采样的。代理架构结合了3D卷积神经网络和前馈层,以捕获局部空间模式和全局交互。在离散裂缝-基质(DFM)模拟生成的数据上训练三个代理,每个代理对应不同的裂缝-基质导电性比。通过不同的裂缝网络参数和矩阵场的相关长度来评估它们的性能。经过训练的代理在广泛的测试场景中实现了很高的预测精度(NRMSE<0.22)。为了证明实际的适用性,我们在两个宏观尺度问题中比较了通过数值均匀化和我们的替代品升级的电导率:水力电导率的等效张量的计算和从受限的3D区域流出的预测。在这两种情况下,基于代理的方法都保持了准确性,同时大大降低了计算成本。当在GPU上执行推理时,基于代理的升级可以实现超过100倍的加速。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Computers & Geosciences
Computers & Geosciences 地学-地球科学综合
CiteScore
9.30
自引率
6.80%
发文量
164
审稿时长
3.4 months
期刊介绍: Computers & Geosciences publishes high impact, original research at the interface between Computer Sciences and Geosciences. Publications should apply modern computer science paradigms, whether computational or informatics-based, to address problems in the geosciences.
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