吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (5): 1546-1555.doi: 10.13278/j.cnki.jjuese.20180179
• 中国水利学会勘测专业委员会专栏 • 上一篇
唐军峰1, 唐雪梅2, 曾向农3, 杨军1, 李学政1
Tang Junfeng1, Tang Xuemei2, Zeng Xiangnong3, Yang Jun1, Li Xuezheng1
摘要: 水库蓄水极易诱发库区地质灾害,所以研究水库库岸堆积体边坡在蓄水前后的变形特征及其稳定性具有重要意义。本文基于现场详细的工程地质勘察资料和监测资料,分析了堆积体边坡的结构特征和变形特征;在此基础上,对堆积体的形成和变形机制进行了探讨;最后,采用离散元数值计算方法,对堆积体边坡在蓄水前后的稳定性进行了计算分析。研究结果表明:堆积体形成于古滑坡,水库在短时间(两个月)内大幅度抬高水位近40.00 m,从而激活了古滑坡,导致变形的产生;排水洞和排水孔的施工有效降低了坡体内地下水位,有效减缓了变形的发展,部分测点变形有收敛趋势,但仍需进一步观测。
中图分类号:
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