Experimental and numerical analysis of injection-induced permeability changes in pre-existing fractures

IF 3.3 2区 工程技术 Q3 ENERGY & FUELS Geomechanics for Energy and the Environment Pub Date : 2024-07-20 DOI:10.1016/j.gete.2024.100576
Josselin Ouf , Julian Osten , Wen Luo , Kavan Khaledi , Mohammadreza Jalali , Philip J. Vardon , Florian Amann
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Abstract

This paper presents a combined laboratory and numerical investigation on the injection-induced permeability changes in pre-existing fractures. The analyses conducted were primarily based on the results of an innovative laboratory experiment designed to replicate the key mechanisms that occur during hydraulic stimulation of naturally fractured rocks and/or faulted zones. The experiment involved pressure-controlled fluid injection into a laboratory-scale pre-existing fracture within a granite block, which was subjected to true triaxial stress conditions. Rough and smooth fractures are investigated, and the results are discussed. Based on the experimental results, two contributing mechanisms were considered to describe the pressure-driven permeability changes in pre-existing fractures: (1) elastic opening/closure leading to a reversible permeability change, and (2) fracture sliding in shear mode, causing dilation and hence an irreversible permeability increase. With these assumptions, an aperture-dependent permeability function was adopted to couple the hydraulic flow with the mechanical deformations along the fracture. Subsequently, a 3D coupled hydro-mechanical model was developed to replicate fluid-injection tests conducted at various conditions, including different stress conditions and fracture surface roughness. The employed modeling framework effectively captured the experimental observations. Our results indicate that the maximum permeability increases twofold.

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对已有裂缝中注水引起的渗透性变化的实验和数值分析
本文介绍了一项实验室和数值相结合的研究,研究内容是注水引起的原已存在裂缝的渗透率变化。分析主要基于一项创新性实验室实验的结果,该实验旨在复制天然裂缝岩石和/或断层带水力刺激过程中发生的关键机制。实验是将压力控制流体注入实验室规模的花岗岩岩块中预先存在的裂缝中,使其承受真正的三轴应力条件。对粗糙和光滑断裂进行了研究,并对结果进行了讨论。根据实验结果,认为有两种机制可用于描述压力驱动的预存裂缝渗透率变化:(1) 弹性开闭导致可逆的渗透率变化;(2) 断裂在剪切模式下滑动,造成扩张,从而导致不可逆的渗透率增加。根据这些假设,采用了与孔径相关的渗透率函数,将水力流动与裂缝沿线的机械变形耦合起来。随后,建立了一个三维水力机械耦合模型,以复制在不同条件下进行的注液试验,包括不同的应力条件和裂缝表面粗糙度。所采用的建模框架有效地捕捉到了实验观测结果。结果表明,最大渗透率增加了两倍。
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来源期刊
Geomechanics for Energy and the Environment
Geomechanics for Energy and the Environment Earth and Planetary Sciences-Geotechnical Engineering and Engineering Geology
CiteScore
5.90
自引率
11.80%
发文量
87
期刊介绍: The aim of the Journal is to publish research results of the highest quality and of lasting importance on the subject of geomechanics, with the focus on applications to geological energy production and storage, and the interaction of soils and rocks with the natural and engineered environment. Special attention is given to concepts and developments of new energy geotechnologies that comprise intrinsic mechanisms protecting the environment against a potential engineering induced damage, hence warranting sustainable usage of energy resources. The scope of the journal is broad, including fundamental concepts in geomechanics and mechanics of porous media, the experiments and analysis of novel phenomena and applications. Of special interest are issues resulting from coupling of particular physics, chemistry and biology of external forcings, as well as of pore fluid/gas and minerals to the solid mechanics of the medium skeleton and pore fluid mechanics. The multi-scale and inter-scale interactions between the phenomena and the behavior representations are also of particular interest. Contributions to general theoretical approach to these issues, but of potential reference to geomechanics in its context of energy and the environment are also most welcome.
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