首页> 外文会议>International symposium on unsaturated soil mechanics and deep geological nuclear waste disposal >NUMERICAL STUDY OF LONG-TERM THM COUPLING BEHAVIOR OF ARGILLITE FILLING WITH SWELLING CLAY
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NUMERICAL STUDY OF LONG-TERM THM COUPLING BEHAVIOR OF ARGILLITE FILLING WITH SWELLING CLAY

机译:膨胀黏土填充硅藻土的长期THM耦合数值研究

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摘要

To investigate the long-term thermo-hydro-mechanical coupling behavior of the host rock filling with barrier materials near nuclear waste cans, a numerical model is employed to study the variation of deformation, temperature and pore pressure in the rock mass with time up to 10,000 years. The simulation process includes excavation, backfill and heating of the swelling clay and host rock. The curve of temperature variation of clay is used to simulate the corruption of waste can. Based on the study of variation of pore pressure, displacement and temperature at different point in the host rock along radial direction, the maximum disturbed extent of host rock due to the temperature variation of swelling clay is discussed. The whole process of the tHM response of the host rock up to 10,000 year is also simulated in this research. It shows that the temperature and pore pressure of the rock mass will increase at the beginning and the then decrease. When time goes up to 10,000year, the pore pressure of the rock mass go back to its original state, but the temperature and deformation will not restore its original state.
机译:为了研究核废料罐附近填充有阻挡层材料的主体岩石的长期热-水-机械耦合行为,采用数值模型研究了岩体中变形,温度和孔隙压力随时间的变化。 10,000年模拟过程包括膨胀粘土和基质岩石的开挖,回填和加热。用粘土的温度变化曲线来模拟废物罐的破坏。在研究基岩沿径向不同点的孔隙压力,位移和温度变化的基础上,探讨了膨胀黏土温度变化对基岩最大扰动程度。这项研究还模拟了长达10,000年的宿主岩石的tHM反应全过程。结果表明,岩体的温度和孔隙压力在开始时会先升高然后降低。当时间延长到10,000年时,岩体的孔隙压力会恢复到其原始状态,但温度和变形将无法恢复其原始状态。

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