高应变率下红砂岩"冻伤效应"

"Frostbite effect" of red sandstone under high strain rates

  • 摘要: 对低温冻结红砂岩进行动态冲击实验,研究高应变率下红砂岩动态力学特性的温度效应,运用损伤理论和能量理论,分析不同负温对红砂岩强度、损伤变量及能量耗散的影响,结合断口形貌分析,探究红砂岩在较低负温下动态力学强度出现劣化的原因.研究表明:较低的负温(-30℃后)会使红砂岩出现"冻伤",导致高应变率下岩石动态力学强度的急剧降低,宏观上则容易出现动力扰动下的瞬时工程灾变.根据断口形貌分析,较低的负温会导致红砂岩内部组成物质间界面处生成大量裂纹,这些裂纹尖端塑性变形能力差,在高应变率加载下极易失稳扩展发生低应力脆性破坏,而胶结物由于组成矿物成分复杂更易受负温影响,因此在动荷载和负温双重作用下往往是胶结物处先产生破坏,进而引起红砂岩整体的破裂.

     

    Abstract: Under the action of negative temperature, the static strength of a rock increases; however, the rock will tend to be brittle, failure strain will decrease, and the rock will also bear the action of internal ice heave force, which leads to complex dynamic behavior of rocks under high strain rate loading. In addition, the geotechnical structures in cold regions are prone to sudden engineering disasters under dynamic disturbance. In this study, a dynamic impact experiment of low-temperature frozen red sandstone was carried out to investigate the temperature effect on the dynamic mechanical properties of red sandstone under high strain rate. Based on the damage theory and energy theory, the effects of different negative temperatures on the strength, damage variables, and energy dissipation of red sandstone were analyzed, and the reasons for the dynamic mechanical strength deterioration of red sandstone at lower negative temperatures were explored using fracture morphology analysis. Research shows that the low negative temperature (after -30℃) can cause a "frostbite" red sandstone, resulting in a sharp decrease in the dynamic mechanical strength of rocks under high strain rate, and transient engineering disasters can easily occur under dynamic disturbance. According to the fracture morphology analysis, the low negative temperature will cause a large number of cracks to be generated at the interface between the components in the red sandstone. The plastic deformation ability of the crack tip is poor, and the crack can easily lose stability and expand under high strain rates, resulting in the low-stress brittle failure. However, due to the complex mineral composition of the cementitious materials, they are more susceptible to negative temperature. Therefore, under the double action of dynamic load and negative temperature, the damage usually occurs first at the cementitious materials and then results in the fracture of the whole red sandstone.

     

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