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Mechanical properties of freeze-thaw and damage propagation law for rock

机译:岩石的冻融力学特性及损伤传播规律

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Using the experimental research method of ‘the temperature gradient under the open system’ recommended by the International Association of Ground Freezing, the freeze-thaw cycling and mechanical experiment were conducted for two types of rock which are red sandstone and shale in water-saturated state, the influence of the lithology and freeze-thaw cycle on rock mechanical characteristics were studied systematically. The unified damage propagation constitutive relation and damage evolution equation of the freeze-thaw and loaded rock under different free-thaw cycles were established by applying the mechanics of freeze-thaw media and damage. The damage evolutionary route of meso-structure and the macro mechanical behavior of rock materials were described. The result shows that three deterioration modes of freeze-thaw damage are spalling mode, fracture mode and crack mode. Sandstone is more sensitive to the freeze-thaw cycle and its freeze-thaw damage is more serious than shale. The initial microscopic differences within the materials determine the characteristics of damage propagation, showing the macroscopic differences in the final state. The freeze-thaw and loaded damage characteristics predicted by damage model are in good agreement with the freeze-thaw mechanical experiment. The impact of the freeze-thaw and loaded damage must be considered in rock engineering design and construction in cold regions.
机译:利用国际地面冻结协会推荐的“开放系统下温度梯度”的实验研究方法,对含水饱和状态的红砂岩和页岩两种岩石进行了冻融循环和力学实验。 ,系统地研究了岩性和冻融循环对岩石力学特性的影响。运用冻融介质和损伤力学,建立了冻融和加载岩石在不同自由冻融循环下的统一损伤传播本构关系和损伤演化方程。描述了细观结构的损伤演化路径和岩石材料的宏观力学行为。结果表明,冻融破坏的三种恶化模式为剥落模式,断裂模式和裂纹模式。砂岩对冻融循环更敏感,其冻融破坏比页岩更严重。材料中的初始微观差异决定了损伤传播的特性,显示了最终状态下的宏观差异。损伤模型预测的冻融载荷特性与冻融力学实验吻合良好。在寒冷地区的岩石工程设计和施工中,必须考虑冻融和荷载破坏的影响。

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