Zady Ouraga , Carlos Plúa , Minh-Ngoc Vu , Gilles Armand
{"title":"Thermo-hydro mechanical coupling in a discrete modelling: Large-scale 3D application to thermal hydrofracturing","authors":"Zady Ouraga , Carlos Plúa , Minh-Ngoc Vu , Gilles Armand","doi":"10.1016/j.gete.2025.100656","DOIUrl":null,"url":null,"abstract":"<div><div>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).</div></div>","PeriodicalId":56008,"journal":{"name":"Geomechanics for Energy and the Environment","volume":"41 ","pages":"Article 100656"},"PeriodicalIF":3.3000,"publicationDate":"2025-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geomechanics for Energy and the Environment","FirstCategoryId":"5","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S2352380825000218","RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"ENERGY & FUELS","Score":null,"Total":0}
引用次数: 0
Abstract
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).
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.