摘要
利用2009年链子崖T8~T12缝段危岩体变形监测中张开、闭合月变量和降雨量数据,以图形的方式来显示其变形趋势和特征,以数理统计的方法进行比较和分析。最后得出大气降雨对链子崖T8~T12缝段危岩体变形影响很弱,变形在允许范围内。
This paper made use of the opening and closing month variables, rainfall data from T8 - T12 fracture sections in Lianzi Cliff deformation monitoring. By the way of graph its deforming trend and eharacteristics were shown. Mathematieal statistics method was used for comparison and analysis. Finally it was concluded that the atmospheric rainfall impact on T8 - T12 fracture sections deformation is very weak, and the deformation is within the permissible range.
出处
《浙江水利科技》
2015年第1期64-66,共3页
Zhejiang Hydrotechnics
基金
国家自然科学基金(41172298
41302260)
湖北省自然科学基金创新群体项目(2012FFA040)
关键词
链子崖
危岩体
大气降雨
变形机制
防水防渗措施
dangerous rock mass
Lianzi cliff
atmospheric rainfall
deformation mechanism
water seepage control measures
