深部饱水岩石蠕变试验及其流变模型(英文)

选取冬瓜山铜矿的深部饱水岩石试样,以单轴压缩单级加载和分级增量循环加卸载两种方式进行蠕变试验,得到不同应力状态下饱水岩石的流变试验曲线。以同一地点的干燥岩石的蠕变规律为对比,分析深部岩石在饱水情况下的流变规律,并基于统一流变力学模型,对深部饱水岩石的流变模型进行辨识,确定流变模型的相关参数。结果表明:在低应力条件下,饱水岩石的蠕变曲线非常平稳,但在高应力时,蠕变曲线出现波动,有突变现象产生,岩样内部承载能力随着时间的延长而不断弱化;在深部高应力条件下,饱水岩石的流变特性与干燥情况下的差别很大,尤其是在高应力卸载时,岩石质量劣化、损伤加剧,水的影响不可忽略。选定HH|NN|S模型(SchofieldScottBlair模型)描述深部饱水岩石的流变规律,模型的拟合曲线与试验数据符合得很好,表明所选的模型是合理的。

Creep experiment and rheological model of deep saturated rock

By the methods of uniaxial single-stage loading and graded incremental cyclic loading, the creep experiments were performed on the deep saturated rock from Dongguashan Mine, and the creep curves of saturated rock under different loading stresses were obtained. By comparing with the creep rule of dry rock in the same location, the creep rule of deep saturated rock was analyzed. Based on the united rheological mechanical model, the rheological model of deep saturated rock was recognized, and the parameters of the model were determined. The results show that the creep curves are very smooth under low stress, but the phenomena of wave and catastrophe turn up under high stress, and the bearing capacity of rock is weakening over time. The rheological properties of saturated and dry rocks are very different under the condition of deep high stress, especially when unloading, degradation and damage of rock quality is more serious, and the effect of water cannot be neglected. The H—H|N—N|S model (Schofield-Scott-Blair model) was selected to represent the rheology rule of deep saturated rock, and the fitting curves of model agree well with the experiment data, so the selected model is reasonable.