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Experiment of Water Phase-change Cycles and Analysis of Damage Characteristics for Argillaceous Dolomite

机译:水相变循环试验及泥虫白云岩损伤特征分析

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For the purpose of research on behavior of argillaceous dolomite suffering from extreme weather impacts in Guizhou region, Study the behavior of the physical properties of rock samples after the water phase transition effect. By wet and dry cycle test, freeze-thaw cycle test, wet freeze-thaw cycle test on rock samples, studying the longitudinal wave velocity, the macro scale and quality parameters of the rock samples after each cycle, while observing the appearance of the rock sample characteristics, and explaining the reason for the parameters change of the rocks macroscopic properties from the microscopic. The results show that in the water phase-change cycle (wet and dry cycle test, freeze-thaw cycle test, wet freeze-thaw cycle test) process, the rock sample degradation forms performance for chipping, flaking mode, longitudinal wave velocity decreases obviously, and Longitudinal wave velocity decreased respectively by 18.01%, 14.88% and 17.05% on average, while mass has a small increase, maximum change rate of 0.5%. Macroscopic properties of the rock are significantly affected by water phase-change cycle.
机译:为贵州地区遭受极端天气影响的骨质白云石的行为的目的,研究水相过渡效果后岩石样品物理性质的行为。通过湿循环试验,冻融循环试验,岩石样品上的湿冻结循环试验,研究每个循环后岩石样品的宏观尺度和质量参数,同时观察岩石的外观样本特性,并解释岩石宏观特性的参数变化的原因。结果表明,在水相变循环(湿循环试验,冻融循环试验,湿冷冻结循环试验)过程中,岩石样品劣化形式的碎裂性能明显减小,纵向波速度降低并且平均分别降低18.01%,14.88%和17.05%的纵波速度,而质量较小,最大变化率为0.5%。岩石的宏观性质受到水相变循环的显着影响。

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