离散建模中的热-水力学耦合:热水力压裂的大规模3D应用

IF 3.7 2区 工程技术 Q3 ENERGY & FUELS
Zady Ouraga , Carlos Plúa , Minh-Ngoc Vu , Gilles Armand
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引用次数: 0

摘要

这项工作旨在模拟由法国国家放射性废物管理局(Andra)在默兹/上马恩地下研究实验室(MHM URL)内进行的现场加热测试(CRQ),采用离散方法。CRQ试验的建模是通过国际研究项目DECOVALEX进行的数值模拟的一部分。CRQ测试的目的是研究Callovo-Oxfordian粘土岩(COx)地层的热水力压裂条件,并确定其对孔隙压力演化的影响。该离散模型将热-水-机械(THM)耦合引入到Itasca离散代码3DEC中,该代码表示弹性可变形块的组合,其界面建模为关节。THM公式在3DEC代码中使用迭代方法实现。在每一步中,这种迭代数值求解从热模拟开始。然后,通过一系列水力和力学计算进行水-力学计算,直至达到平衡。这个迭代过程在每个时间步重复,直到达到最终的计算时间。为了模拟COx中的压裂过程,对节理采用了基于莫尔库仑的抗拉截止破坏准则。通过考虑无限饱和多孔介质中的热源,首先对多孔弹性闭型解进行了THM耦合实现的验证。之后,考虑CRQ实验,特别关注热压裂现象,因为离散模型的主要优势在于它明确地表示裂缝。该研究还证明了离散模型处理包含多个过程(THM耦合和岩石破坏)的大型模型的能力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Thermo-hydro mechanical coupling in a discrete modelling: Large-scale 3D application to thermal hydrofracturing
This work aims to model an in-situ heating test (CRQ) conducted by the French National Radioactive Waste Management Agency (Andra) within the Meuse/Haute-Marne Underground Research Laboratory (MHM URL), using a discrete approach. The modelling of the CRQ test is part of numerical simulations performed through the international research project DECOVALEX. The goal of the CRQ test is to study the conditions under which thermal hydrofracturing can occur in the Callovo-Oxfordian claystone (COx) formation and to identify its influence on pore pressure evolution. The present discrete model introduces thermo-hydro-mechanical (THM) coupling into the Itasca discrete code 3DEC, which represents an assembly of elastic deformable blocks with interfaces modelled as joints. The THM formulation is implemented in the 3DEC code using an iterative approach. At each step, this iterative numerical solving starts by the thermal simulation. Then, the hydro-mechanical calculation is carried out by a series of hydraulic and mechanical computations until equilibrium is reached. This iterative process repeats at each timestep until the final calculation time is achieved. To model the fracturing process in the COx, a failure criterion based on Mohr Coulomb with tensile cut-off is used for the joints. The THM coupling implementation is first validated against a poro-elastic closed-form solution by considering a heat source within an infinite saturated porous medium. Afterwards, the CRQ experiment is considered with particular attention to the phenomenon of thermal fracturing, as the main advantage of the discrete model lies in its explicitly representation of fractures. This study also demonstrates the ability of a discrete model in dealing with a large model that includes multiple processes (THM coupling and rock failure).
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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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