人民长江Issue(14)：32-35,4.DOI:10.16232/j.cnki.1001-4179.2015.14.010
高陡边坡深部卸荷张拉裂缝的成因机制探讨
Discussion on genetic mechanism of large-depth unloading tension fracture in high and steep slope
彭少文 1贺金明 1孙冠军 1刘培培1
作者信息
- 1. 长江三峡勘测研究院有限公司 武汉，湖北 武汉430074
- 折叠
摘要
Abstract
In high geo-stress area, many deep tension fractures developed in the inside of some high and steep slope with horizontal depth of 200 to 300 m or even deeper, which is beyond the understanding of unloading laws in practical experience. So a reasonable explanation of this special engineering and geological phenomenon becomes a new subject. The genetic mechanism of tension fracture in deep unloading condition is further discussed on the basis of the analysis and summary of previous research re-sults, in terms of around environment, rock structure and geological tectonics. The results in current stage showed that the ten-sion fracture in deep unloading condition can partially affect the slope stability;the fracture would develop and expand under in-ner force or water filling condition, so as to control the stability of the slope.关键词
高地应力/高陡边坡/卸荷/深部张拉裂缝/成因机制/边坡稳定性Key words
high geo-stress/high and steep slope/unloading/deep tension fracture/genetic mechanism/stability of slope分类
天文与地球科学引用本文复制引用
彭少文,贺金明,孙冠军,刘培培..高陡边坡深部卸荷张拉裂缝的成因机制探讨[J].人民长江,2015,(14):32-35,4.
