| 注册
首页|期刊导航|地震工程学报|地震作用下节理岩质边坡稳定性影响因素研究

地震作用下节理岩质边坡稳定性影响因素研究

滕光亮 陈永明 石玉成 孙崇绍 卢育霞 强正阳

地震工程学报2013,Vol.35Issue(1):119-125,7.
地震工程学报2013,Vol.35Issue(1):119-125,7.DOI:10.3969/j.issn.1000-0844.2013.01.0119

地震作用下节理岩质边坡稳定性影响因素研究

A Study on the Influencing Factors of Joint Rock Slope Stability under Earthquake Activity

滕光亮 1陈永明 2石玉成 3孙崇绍 3卢育霞 3强正阳3

作者信息

  • 1. 甘肃省地震局(中国地震局黄土地震工程重点实验室),甘肃兰州 730000
  • 2. 中国地震局兰州地震研究所,甘肃兰州730000
  • 折叠

摘要

Abstract

Disaster survey results of the Wenchuan earthquake show that seismic landslides mainly develop within thick-bedded or massive rock, in which local intensity is relatively large and joints are obvious. Although seismic landslides differ markedly from those induced by rainfall and other factors, this topic has not drawn sufficient attention. Moreover, numerical analysis methods of finite element and finite difference, both based on the assumption of continuous media and small deformation, are used in previous studies of slope stability. However, some limitations exist in dynamic analysis of large deformations of rock slope due to a large number of interfaces of discontinuity. To overcome those problems, the dynamic response of joint rock slope in this thesis is simulated by means of the discrete element numerical simulation, particularly deformation characteristics, failure mechanism, and influencing factors of slope stability. Here, a rock slope containing two groups of joints is used as the research object. In addition, discrete element numerical simulation is conducted, and actual earthquake records are input to simulate a large number of cases. The influencing factors of the joint rock slope stability are respectively explored under various conditions of slope height, seismic intensity, slope angle, and joint angle. Topographic amplification effects are observed from both acceleration and velocity of the monitoring points of the slope. Joint rock slope stability is reduced with slope height, slope angle, and seismic intensity. In addition, the stability of the rock slope that contains two groups of joints is complex and is influenced by other factors including joint inclination, slope angle, the tendency of joints, and the angle between two group joints. The regions of tension failure are gradually extended to the shear zone and eventually lead to slope instability and failure, compounded by tensile and shear failure. This study provides a reference for evaluation of the rock slope and joints stability under seismic loading in mountainous areas.

关键词

节理岩质边坡/地震作用/滑塌/离散元/影响因素

Key words

Joint rock slope/ Eearthquake action/ Slump/ Discrete element method/ Influencing factors

分类

建筑与水利

引用本文复制引用

滕光亮,陈永明,石玉成,孙崇绍,卢育霞,强正阳..地震作用下节理岩质边坡稳定性影响因素研究[J].地震工程学报,2013,35(1):119-125,7.

基金项目

中国地震局兰州地震研究所地震科技发展基金(2012M05) (2012M05)

地震工程学报

OA北大核心CSCDCSTPCD

1000-0844

访问量0
|
下载量0
段落导航相关论文