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Fully coupled THM constitutive model for clay rocks:Formulation and application to laboratory tests
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作者 Fei Song Antonio Gens +2 位作者 Stefano Collico Dragan Grgic Huaning Wang 《Journal of Rock Mechanics and Geotechnical Engineering》 2025年第4期1941-1960,共20页
This study presents a fully coupled thermo-hydro-mechanical (THM) constitutive model for clay rocks. The model is formulated within the elastic-viscoplasticity framework, which considers nonlinearity and softening aft... This study presents a fully coupled thermo-hydro-mechanical (THM) constitutive model for clay rocks. The model is formulated within the elastic-viscoplasticity framework, which considers nonlinearity and softening after peak strength, anisotropy of stiffness and strength, as well as permeability variation due to damage. In addition, the mechanical properties are coupled with thermal phenomena and accumulated plastic strains. The adopted nonlocal and viscoplastic approaches enhance numerical efficiency and provide the possibility to simulate localization phenomena. The model is validated against experimental data from laboratory tests conducted on Callovo-Oxfordian (COx) claystone samples that are initially unsaturated and under suction. The tests include a thermal phase where the COx specimens are subjected to different temperature increases. A good agreement with experimental data is obtained. In addition, parametric analyses are carried out to investigate the influence of the hydraulic boundary conditions (B.C.) and post-failure behavior models on the THM behavior evolution. It is shown that different drainage conditions affect the thermally induced pore pressures that, in turn, influence the onset of softening. The constitutive model presented constitutes a promising approach for simulating the most important features of the THM behavior of clay rocks. It is a tool with a high potential for application to several relevant case studies, such as thermal fracturing analysis of nuclear waste disposal systems. 展开更多
关键词 Hard soil Soft rocks Unsaturated/saturated conditions THM coupling processes Thermal pressurization Constitutive model
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Impact of Changing Climate in the Kairouan Hydrological Basin (Central Tunisia)
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作者 B. Chulli G. Favreau +1 位作者 N. Jebnoun M. Bedir 《Journal of Environmental Science and Engineering》 2011年第6期682-688,共7页
The Merguellil catchment (central Tunisia) has undergone rapid hydrological changes over the last decades. The most visible signs are a marked decrease in surface runoff in the upstream catchment and a complete chan... The Merguellil catchment (central Tunisia) has undergone rapid hydrological changes over the last decades. The most visible signs are a marked decrease in surface runoff in the upstream catchment and a complete change in the recharge processes of the Kairouan aquifer downstream. Fluctuations in rainfall have had a real but limited hydrological impact. Much more important are the consequences of human activities such as soil and water conservation works, small and large dams, pumping for irrigation. Several independent approaches were implemented: hydrodynamics, thermal surveys, geochemistry including isotopes. They helped to identify the different terms of the regional water balance and to characterize their changes over time. 展开更多
关键词 Climate change water balance GEOCHEMISTRY HYDRODYNAMICS Tunisia.
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New Structural Elements in Tellian Foreland Domain of the Northeastern Tunisia(Mateur Plain)after Integrating Geological and Geophysical Data
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作者 Sofien Alyahyaoui Hakim Gabtni +1 位作者 Hedi Zouari Houcem Mzali 《International Journal of Geosciences》 2013年第7期1061-1072,共12页
The following paper presents an integrated geological (field observations, wells data) and geophysical data (Gravity measurements and seismic profiles) in Tellian foreland domain of the northeastern Tunisia (Mateur pl... The following paper presents an integrated geological (field observations, wells data) and geophysical data (Gravity measurements and seismic profiles) in Tellian foreland domain of the northeastern Tunisia (Mateur plain) served for a new proposed structural map with many faults already recognized or supposed by traditional structural studies and highlights major regional accidents. 展开更多
关键词 Northeastern Tunisia WELLS Bouguer Gravity Upward Continuation Seismic Lines LINEAMENTS
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