Auto-weighted Bayesian Physics-Informed Neural Networks and robust estimations for multitask inverse problems in pore-scale imaging of dissolution

IF 2.1 3区 地球科学 Q3 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS
Sarah Perez, Philippe Poncet
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引用次数: 0

Abstract

In this article, we present a novel data assimilation strategy in pore-scale imaging and demonstrate that this makes it possible to robustly address reactive inverse problems incorporating Uncertainty Quantification (UQ). Pore-scale modeling of reactive flow offers a valuable opportunity to investigate the evolution of macro-scale properties subject to dynamic processes in the context of Carbon Capture and Storage (CCS). Yet, they suffer from imaging limitations arising from the associated X-ray microtomography (X-ray \(\mu \)CT) process, which induces discrepancies in the properties estimates. Assessment of the kinetic parameters also raises challenges, as reactive coefficients are critical parameters that can cover a wide range of values. We account for these two issues and ensure reliable calibration of pore-scale modeling, based on dynamical \(\mu \)CT images, by integrating uncertainty quantification in the workflow. The present method is based on a multitasking formulation of reactive inverse problems combining data-driven and physics-informed techniques in calcite dissolution. This allows quantifying morphological uncertainties on the porosity field and estimating reactive parameter ranges through prescribed PDE models, with a latent concentration field, and dynamical \(\mu \)CT observations. The data assimilation strategy relies on sequential reinforcement incorporating successively additional PDE constraints and suitable formulation of the heterogeneous diffusion differential operator leading to enhanced computational efficiency. We provide a robust and unbiased uncertainty quantification by straightforward adaptive weighting of Bayesian Physics-Informed Neural Networks (BPINNs), ensuring reliable micro-porosity changes during geochemical transformations. We demonstrate successful Bayesian Inference in 1D+Time calcite dissolution based on synthetic \(\mu \)CT images with meaningful posterior distribution on the reactive parameters and dimensionless numbers. We eventually apply this framework to a more realistic 2D+Time data assimilation problem involving heterogeneous porosity levels and synthetic \(\mu \)CT dynamical observations.

Abstract Image

自动加权贝叶斯物理信息神经网络和多任务反问题的鲁棒估计,用于孔隙尺度溶解成像
在这篇文章中,我们介绍了孔隙尺度成像中的一种新型数据同化策略,并证明这种策略可以稳健地解决包含不确定性量化(UQ)的反应逆问题。孔隙尺度的反应流建模为研究碳捕获与封存(CCS)背景下受动态过程影响的宏观尺度属性的演变提供了宝贵的机会。然而,由于相关的 X 射线显微层析成像(X-ray \(\mu \)CT)过程造成的成像限制,它们在属性估计方面存在差异。对动力学参数的评估也提出了挑战,因为反应系数是关键参数,其取值范围很广。我们考虑到了这两个问题,并通过在工作流程中集成不确定性量化,确保了基于动态 CT 图像的孔隙尺度建模的可靠校准。本方法基于反应逆问题的多任务表述,结合了方解石溶解过程中的数据驱动和物理信息技术。这样就可以量化孔隙度场的形态不确定性,并通过规定的 PDE 模型、潜浓度场和动态 CT 观测来估算反应参数范围。数据同化策略依赖于连续的强化,包括连续的附加 PDE 约束条件和异质扩散微分算子的适当表述,从而提高计算效率。我们通过贝叶斯物理信息神经网络(BPINNs)的直接自适应加权,提供了稳健、无偏的不确定性量化,确保了地球化学转换过程中微观孔隙度变化的可靠性。我们成功地展示了基于合成 CT 图像的 1D+Time 方解石溶解贝叶斯推理,其反应参数和无量纲数的后验分布非常有意义。最终,我们将这一框架应用于更现实的二维+时间数据同化问题,该问题涉及异质孔隙度水平和合成(\μ \)CT动态观测。
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来源期刊
Computational Geosciences
Computational Geosciences 地学-地球科学综合
CiteScore
6.10
自引率
4.00%
发文量
63
审稿时长
6-12 weeks
期刊介绍: Computational Geosciences publishes high quality papers on mathematical modeling, simulation, numerical analysis, and other computational aspects of the geosciences. In particular the journal is focused on advanced numerical methods for the simulation of subsurface flow and transport, and associated aspects such as discretization, gridding, upscaling, optimization, data assimilation, uncertainty assessment, and high performance parallel and grid computing. Papers treating similar topics but with applications to other fields in the geosciences, such as geomechanics, geophysics, oceanography, or meteorology, will also be considered. The journal provides a platform for interaction and multidisciplinary collaboration among diverse scientific groups, from both academia and industry, which share an interest in developing mathematical models and efficient algorithms for solving them, such as mathematicians, engineers, chemists, physicists, and geoscientists.
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