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用于多孔弹性介质中裂缝扩展的耦合相场与反应输运框架。

A coupled phase-field and reactive-transport framework for fracture propagation in poroelastic media.

作者信息

Clavijo Santiago Pena, Addassi Mouadh, Finkbeiner Thomas, Hoteit Hussein

机构信息

King Abdullah University of Science and Technology (KAUST), Thuwal, 23955-6900, Saudi Arabia.

出版信息

Sci Rep. 2022 Oct 24;12(1):17819. doi: 10.1038/s41598-022-22684-1.

Abstract

We present a novel approach to model hydro-chemo-mechanical responses in rock formations subject to fracture propagation within chemically active rock formations. The framework developed integrates the mechanisms of reactive transport, fluid flow and transport in porous media, and phase-field modelling of fracture propagation in poroelastic media. The solution approach integrates the geochemical package PHREEQC with a finite-element open-source platform, FEniCs. The PHREEQC solver is used to calculate the localized chemical reaction, including solid dissolution/precipitation. The resulting solid weakening by chemical damage is estimated from the reaction-induced porosity change. The proposed coupled model was verified with previous numerical results and applied to a synthetic case exhibiting hydraulic fracturing enhanced with chemical damage. Simulation results suggest that mechanical failure could be accelerated in the presence of ongoing chemical processes due to rock weakening and porosity changes, allowing the nucleation, growth, and development of fractures.

摘要

我们提出了一种新方法,用于模拟在化学活性岩层中发生裂缝扩展时岩层的水力 - 化学 - 力学响应。所开发的框架整合了反应输运、多孔介质中的流体流动与输运以及多孔弹性介质中裂缝扩展的相场建模等机制。求解方法将地球化学软件包PHREEQC与有限元开源平台FEniCs相结合。PHREEQC求解器用于计算局部化学反应,包括固体溶解/沉淀。由反应引起的孔隙度变化来估算因化学损伤导致的固体弱化。所提出的耦合模型通过先前的数值结果进行了验证,并应用于一个展示化学损伤增强水力压裂的合成案例。模拟结果表明,由于岩石弱化和孔隙度变化,在持续的化学过程存在的情况下,机械破坏可能会加速,从而使裂缝成核、生长和发展。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/add5/9592620/6046a6daaa22/41598_2022_22684_Fig1_HTML.jpg

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