摘要
岩体破坏可能是由于各类岩体工程的开挖引起的,同时影响其失稳破坏的主要外界因素就是地下水及其在岩体中的渗流.为了分析岩石卸荷量与渗透系数的关系,提出了岩石卸荷试验的方法和步骤.通过试验得到了不同阶段卸荷量与渗透系数之间的关系曲线.根据试验结果,建立了卸荷应力-渗透系数关系方程,探讨了岩石渗透系数与卸荷量之间的变化规律:在卸荷过程中的弹性阶段,其渗透系数基本无变化;当进入卸荷的塑性阶段,其渗透系数发生较大变化,尤其当卸荷量达到极限卸荷量的80%以上,渗透系数增长较快.
The destruction of rock mass arises from opening rock possibly, the main outside-factor of influence rock slope stability is groundwater and water seepage. To analyze the relationship of unloading and permeability coefficient, the method and step of experiment of unloading rock mass are put forward. The curve relationship of the seepage-unloading of different phase is found by experiment. According to the experimental result, the equation of the seepage-stress of unloading is established, the variational rule of the unloading and permeability coefficient is discussed. The permeability coefficient is almost unchanged in the elasticity phase of unloading process. The permeability coefficient changes very much in the plastic phase of unloading process, as the unloading is 80% of ultimate unloading especially, and the permeability coefficient is increasing very much.
出处
《重庆大学学报（自然科学版）》
EI
CAS
CSCD
北大核心
2005年第10期133-135,共3页
Journal of Chongqing University
基金
国家留学回国人员科研启动基金重点项目(教外司留[2002]247号)
重庆市应用基础研究项目(8020)
关键词
岩体
卸荷
渗透系数
试验
rock mass
unloading
permeability coefficient
experiment
