基于强度折减法的花石崖危岩体稳定因素数值分析

高德军,郑居华,贾蕴翔,朱小冬,李昆,丁绪蒙

长江科学院院报 ›› 2017, Vol. 34 ›› Issue (10) : 114-117.

PDF(2750 KB)
PDF(2750 KB)
长江科学院院报 ›› 2017, Vol. 34 ›› Issue (10) : 114-117. DOI: 10.11988/ckyyb.20160651
岩土工程

基于强度折减法的花石崖危岩体稳定因素数值分析

  • 高德军1,郑居华1,贾蕴翔2,朱小冬1,李昆1,丁绪蒙1
作者信息 +

Numerical Analysis on Stability Factors of Potentially Unstable Rockat Huashi Cliff Based on Strength Reduction Method

  • GAO De-jun1, ZHENG Ju-hua1, JIA Yun-xiang2, ZHU Xiao-dong1, LI Kun1, DING Xu-meng1
Author information +
文章历史 +

摘要

危岩体一般处于非稳定或极限平衡状态,影响危岩体稳定的因素很多,而地质勘探往往难以给出危岩体的准确参数。以金沙江花石崖危岩体为例,主要考虑了危岩体裂缝位置和深度、裂缝中水压力大小、危岩体强度参数以及危岩体下部软弱岩层参数等因素。使用FLAC3D软件基于强度折减法计算分析各因素变化对危岩体安全系数的影响。对比计算分析结果表明,裂隙水压力和危岩体下部软弱岩层参数对危岩体稳定影响较大,在危岩体治理中应加固下部软弱岩层以及封闭上部裂缝,防止雨水汇集。

Abstract

Potentially unstable rock mass is generally in unsteady or limit equilibrium state. There are many factors (that affect the stability of potentially unstable rock mass, but geological exploration is often difficult to give accurate parameters about the potentially unstable rock mass. With the potentially unstable rock mass at Huashi cliff on Jinsha River as an example, we took in consideration factors including crack position and depth, fissure water pressure, strength parameters of potentially unstable rock mass, and parameters of weak rock strata under the potentially unstable rock mass. Furthermore, we calculated the effect of the above factors on the safety coefficient of rock mass by using FLAC3D based on strength reduction method. Through comparisons, we concluded that fissure water pressure and parameters of weak rock strata under the potentially unstable rock mass have great influence on the stability of the potentially unstable rock mass. Therefore, weak rock strata under the potentially unstable rock mass should be reinforced, and the fissures must be closed to prevent from rainwater collection.

关键词

危岩体治理 / 失稳破坏 / 强度折减法 / 影响因素 / FLAC3D软件

Key words

Key words: treatment of potentially unstable rock / instability and failure / strength reduction method / influence factor / FLAC3D

引用本文

导出引用
高德军,郑居华,贾蕴翔,朱小冬,李昆,丁绪蒙. 基于强度折减法的花石崖危岩体稳定因素数值分析[J]. 长江科学院院报. 2017, 34(10): 114-117 https://doi.org/10.11988/ckyyb.20160651
GAO De-jun, ZHENG Ju-hua, JIA Yun-xiang, ZHU Xiao-dong, LI Kun, DING Xu-meng. Numerical Analysis on Stability Factors of Potentially Unstable Rockat Huashi Cliff Based on Strength Reduction Method[J]. Journal of Changjiang River Scientific Research Institute. 2017, 34(10): 114-117 https://doi.org/10.11988/ckyyb.20160651
中图分类号: TU413.62   

参考文献

[1] 陈洪凯,欧阳仲春,廖世荣.三峡库区危岩综合治理技术及应用.地下空间,2002,22(2):97-101.
陈洪凯,王 蓉,唐红梅.危岩研究现状及趋势综述.重庆交通学院学报,2003,22(3):18-22.
陈鹏宇,曾红彪,师华鹏,等.危岩稳定性评价的颗粒流断裂力学法.自然灾害学报,2016,25(3):87-95.
PEILA D, PELIZZA S, SASSUDELLI F. Evaluation of Behavior of Rockfall Restraining Nets by Full-scale Tests. Rock Mechanics and Rock Engineering, 1998, 31(1):1-24.
FRANKS C A M. Characteristics of Some Rainfall-induced Landslides on Natural Slopes Lantau Island, Hong Kong. Quarterly Journal of Engineering Geology and Hydrogeology, 1999, 32(3): 247-259.
刘景元,宋立军,戴晓敏. 1998年3月19日阿图什6.0级地震震害特征.内陆地震,1999,13(1):44-49.
殷坤龙.重庆市崩塌滑坡地质灾害规律.中国地质灾害与防治学报,1994,5(增):18-23.
陈洪凯,唐红梅,王 蓉.三峡库区危岩稳定性计算方法及应用.岩石力学与工程学报,2004,23(4):614-619.
欧武涛,王 伟.层次分析法在危岩稳定性评价中的应用:以重庆市渝北区老岩危岩为例.重庆交通大学学报:自然科学版,2011,30(增1):650-651,696.
李凤明.长江三峡链子崖危岩体产生机理工程治理.煤炭科学技术,2005,33(10):13-16.
刘传正,王洪德,涂鹏飞,等.长江三峡链子崖危岩体防治工程效果研究.岩石力学与工程学报,2006,25(11):2771-2179.
刘传正,张明霞.长江三峡链子崖危岩体防治工程研究.岩石力学与工程学报,1999,18(5):497-502.
李 剑,陈善雄,余 飞.基于最大剪应变增量的边坡潜在滑动面搜索.岩土力学,2013,34(增1):371-378.
陈育民,徐鼎平.FLAC/FLAC3D基础与工程实例[M].北京:中国水利水电出版社,2008.
田 林.基于FLAC3D的危岩高边坡稳定性研究.昆明:昆明理工大学,2012.
董 倩,朱正伟,刘东燕.崩塌堆积体破坏及稳定性分析.西安建筑科技大学(自然科学版),2010,42(3):358-363.

基金

防灾减灾湖北省重点实验室(三峡大学)开放基金资助项目(2016KJZ09)

PDF(2750 KB)

Accesses

Citation

Detail

段落导航
相关文章

/