关键词: 泥质砂岩, 砂质泥岩, 卸荷, 蠕变, 力学特性, 本构模型, 数值模拟

Abstract: The long-term creep deformation of soft and hard rock strata may be very uncoordinated, which poses a great threat to the safety and stability of excavation engineering. A series of creep tests and numerical simulations were carried out on two types of rocks (i.e., sandy mudstones and argillaceous sandstones) with large differences of hardness in the same excavation section of diversion tunnel of a hydropower station under unloading conditions. Results show that under the condition of unloading confining pressure, the lateral creep deformation of the specimen develops more rapidly than the axial deformation and a significant lateral expansion occurs. The specimen under a higher initial confining pressure exhibited a greater lateral expansion effect in the unloading creep failure. The deformation rate of argillaceous sandstone in the steady creep stage was slower than that of the sandy mudstone. Meanwhile, the strain values of argillaceous sandstone in the creep failure were smaller than those of the sandy mudstone with weaker signs. Based on the Burgers model, damage variables were introduced to establish a creep damage constitutive model. The model curve well described the linear creep characteristics of rocks before the failure deviatoric stress level and the nonlinear accelerated creep characteristics under the failure deviatoric stress level. The numerical simulations of creep deformation of soft and hard rock strata show that at the early stage, the deformation difference between soft and hard rock contact points was not large. With the increase of time, interlayer dislocation occurs at the interface, which is very unfavorable to the overall stability of surrounding rock and should deserve sufficient attention in the engineering practice.

Key words: 泥质砂岩, 砂质泥岩, 卸荷, 蠕变, 力学特性, 本构模型, 数值模拟