软岩流变的尺寸效应

Scale effect of soft rock rheology

  • 摘要: 岩体内随机分布结构面对软岩流变的影响主要表现为尺寸效应.通过对四种不同尺寸砂质页岩试件的分级增量循环加、卸载单轴压缩蠕变实验,揭示了该类软岩的流变可以用萨乌斯托维奇模型来描述,模型的三个本构参数EH(线弹性参数)、EK(黏弹性参数)和ηK(黏性系数)值随软岩试件尺寸增大而不断减小并最终趋于一定值,这一规律可用具有极值条件的非线性回归方程来表达.由此获得了求解结构面随机分布条件下工程岩体连续微元尺寸的外推方法,利用该法可通过对室内不同尺寸岩石试件的流变力学实验确定在连续性概化范围内工程岩体的流变模型及其力学参数值.

     

    Abstract: The influence of random-distributing structure surfaces in rock mass on the soft rock rheology is mainly expressed by scale effect. Multi-step incremental cycling loading and unloading uniaxial compression creep tests on 4 different sizes of sand-shale specimens showed that soft rock rheology could be described by the Salustowicz model and the values of its constitutive parameters of E H(linear elastic parameter), EK(viscoelastic parameter) and ηK(viscous parameter) would decrease and tend towards being constant as the specimen size increased, which might be expressed by nonlinear regressive equations with extremum conditions. Then an extrapolation method was gained to determine the dimension of the continuous micro element of engineering rock mass with randomly distributing structure surfaces. It may be used to gain the rheological model and its mechanical parameters of engineering rock mass in the continuity schematization range by rheological tests on the different sizes of rock specimens in the laboratory.

     

/

返回文章
返回