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Analytical and numerical analysis for frost heaving stress distribution within rock joints under freezing and thawing cycles

机译:冻结和解冻循环下岩隙内冻结应力分布的分析与数值分析

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摘要

Water-bearing joints within rock engineering in cold areas are often subjected to frost heaving force in cold season due to water-ice phase transition. To evaluate the damage and stability of rock mass in cold regions, a 3D model that considers moisture migration loss during freezing and thawing was established to study the characteristics of frost heaving force within joints. Then, the numerical simulation of cyclic freeze-thawing of water-bearing joints was carried out through equivalent expansion coefficient and particle flow calculation methods. The distribution of frost heaving force in and around the joints was obtained. According to the results of the numerical tests and theoretical calculations, the frost heaving force in joints is basically stable, the tensile stress concentration area appears at the joint tip, and the frost heaving force decreases gradually away from the jointed rock mass area. The frost heaving force decreases considerably with increasing cycle number and moisture migration loss but it increases with increasing mechanical strength and joint geometric size of rock and ice. The comparison between the numerical solution of the equivalent expansion coefficient method and the theoretical solution shows that the force size and distribution law of frost heaving for the two methods are consistent.
机译:由于水冰相转变,寒冷地区岩石工程内的岩石工程中的含水接头常常在寒冷的季节进行霜冻。为了评估岩体在寒冷地区岩体的损伤和稳定性,建立了一种考虑冻融和解冻过程中水分迁移损失的3D模型,研究了关节内冻结力的特点。然后,通过等效的膨胀系数和颗粒流量计算方法进行循环接头的循环冷冻解扫描的数值模拟。获得关节和周围的冻结力的分布。根据数值测试和理论计算的结果,接头中的霜泡力基本稳定,张力浓度面积出现在关节尖端,霜冻力逐渐远离关节岩体区域逐渐降低。随着循环数量和水分迁移损失的增加,冻结力显着降低,但随着岩石和冰的机械强度和关节几何尺寸的增加,它增加。等效膨胀系数法的数值解决方案与理论求解的比较表明,两种方法的霜沉体的力尺寸和分布规律是一致的。

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