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冻融循环条件下岩石物理力学指标相关性分析

Interrelative Analysis on Physical and Mechanical Indicators of Rock underFreezing and Thawing Cycle Condition

  • 摘要: 为了得到冻融循环条件下岩石强度指标与物理指标的关系,在室内实验和理论分析的基础上,建立了冻融循环过程中岩石抗压、抗剪强度力学指标与纵波波速、孔隙率物理指标的关系。试验结果表明:随着冻融循环次数的增加,岩石的孔隙率增大,纵波波速、单轴抗压强度、弹性模量、黏聚力降低;冻融循环条件下粗砂岩的孔隙率、纵波波速与单轴抗压强度、弹性模量、黏聚力之间具有良好的相关性。通过测量经历不同冻融次数的岩石的孔隙率和纵波波速,较好地反映出冻融循环过程中岩石强度的衰减关系。

     

    Abstract: In order to study the interrelation between the strength indicators and physical indicators of rock under freezing and thawing cycle condition, the interrelation between the mechanical indicators such as the comprehensive strength and shear strength of rock and the physical indicators such as its longitudinal wave velocity and porosity under freezing and thawing cycle condition was established on the basis of laboratory experiments and theoretical analysis. The experimental results showed that with the increase of the number of freezing and thawing cycles, the porosity of the rock increased and its longitudinal wave velocity, axial comprehensive strength, elastic modulus and cohesion decreased;.under the freezing and thawing cycle condition, there was a good correlation between the porosity, longitudinal wave velocity, axial comprehensive strength, elastic modulus and cohesion of the coarse sandstone. Therefore, the measurement of the porosity and longitudinal wave velocity of rock can better reflect its strength attenuation relationship in the process of freezing and thawing cycle.

     

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