摘要
剪切裂纹(breakout or spalling)是硬岩地下洞室开挖损伤区的主要破裂形式,对实际岩体工程的稳定性起到了控制作用.选取了粉砂岩圆孔试件进行了双向不等压加载,采用贴应变片的电测法作为监测手段,对剪切裂纹形成演化规律及进一步诱发的破坏形式进行了实验研究.得到了试件表面观测点应力演化规律,在此基础上分析了不等压条件下剪切裂纹的发生机理:不等压下脆性硬岩洞壁不容易破坏,但当加载到一定水平时,破坏很突然,并迅速诱发了"V"形区;孔壁附近发生的是剪切破坏,孔壁深处发生的是拉剪复合型的破坏.
"Breakout or spalling" often occurs at the excavation damage zone of hardrock underground chamber, which controls the stability of rock body. Experiment of circular borehole sample of siltstone in hidireetional unequal pressure loading is conducted, and strain gauge is adopted to monitor the defo mation, then the "breakout and spalling" formation, evolution, and further destruction form are inves- tigated. By experimental studying the stress evolution curves of the observation point on the borehole specimen surface, the mechanism of "breakout or spalling" is analyzed. It showed that the brittle hardrock borehole wall is not easy to damage in bidirectional unequal pressure loading, but when the loading reach a particular level, the borehole wall form develop rapidly. It is found that shear failure mixed failure is deep inside the borehole wall. begin to damage suddenly and the breakout-" V" is near the borehole wall, while compression-shear
出处
《北京交通大学学报》
CAS
CSCD
北大核心
2011年第4期78-82,共5页
JOURNAL OF BEIJING JIAOTONG UNIVERSITY
基金
国家"973"计划项目资助(2010CB226803)
铁道部科技研究开发计划项目资助(2009G005-B)
辽宁工程技术大学优秀青年基金资助项目(2008)
关键词
脆性硬岩
电测法
开挖损伤区
破坏机理
brittle hard rock
strain gauges
excavation damage zone
failure mechanism