Stability evaluation and rockfall trajectory analysis of the Baimagou dangerous rock mass in Mingshan County of Sichuan Province
-
摘要:
危岩体是指由结构面切割形成的在一定诱发因素下失稳破坏的岩体,其作为常见的自然地质灾害之一,严重影响山区人类生命财产安全。对危岩体的勘查、稳定性评价、风险评价是地质灾害预防的研究难题。受人类工程活动影响,名山县新店镇白马沟内存在多处危岩体。通过对国内外研究文献的查阅分析并结合白马沟危岩体的分布特征、发育特征、崩塌落石运动特性进行分析与研究,初步总结出了白垩系上统灌口组(K2g)危岩体的形成、分布规律及成灾机理,并对该区4个危岩体利用Rockfall 进行数值模拟计算,计算其运动速度及运动轨迹,计算岩石弹跳高度及距离等。为此类工程地质条件下的的危岩体稳定性评价及运动轨迹的分析提供参考,同时对于崩塌危岩体灾害预防与减灾技术研究有积极意义 。
Abstract:Dangerous rock mass refers to the rock mass that is cut by the structural plane and fails under certain inducing factors. As one of the common natural geological disasters, it seriously affects the safety of human life and property in mountainous areas. The exploration, stability evaluation and risk evaluation of dangerous rock mass are difficult problems in the research of geological disaster prevention. Affected by human engineering activities, there are many dangerous rock masses in Baimagou, Xindian Town, Mingshan County. Based on the analysis and Research on the distribution and development characteristics of collapse dangerous rock mass in baimagou, this paper preliminarily summarizes the formation, distribution law and disaster mechanism of dangerous rock mass in Guankou formation (K2g) of Upper Cretaceous system, and carries out numerical simulation calculation for four collapse dangerous rock bodies in this area by using Rockfall, calculates their movement speed and trajectory, and calculates the rock bounce height and distance, It provides a reference for the stability evaluation and motion trajectory analysis of dangerous rock mass under such engineering geological conditions.
-
Key words:
- dangerous rock mass /
- structural plane /
- stability evaluation /
- Rockfall /
- path of particle
-
图 6 倾倒式危岩稳定性计算模型(危岩体重心在支点内侧)[14]
Figure 6.
图 7 坠落式危岩计算模型(后缘有陡倾裂隙)[15]
Figure 7.
表 1 危岩体稳定性定性评价统计表
Table 1. Statistical table for qualitative evaluation of stability of dangerous rock mass
编号 体积
/m3破坏
模式稳定性评价 天然工况 暴雨工况 地震工况 W2-1危岩体 250.8 坠落 基本稳定 欠稳定 欠稳定 W3-1危岩体 37.3 坠落 基本稳定 欠稳定 欠稳定 W4-1危岩体 270.3 坠落 基本稳定 欠稳定 欠稳定 W4-2危岩体 53.9 倾倒 基本稳定 欠稳定 欠稳定 表 2 勘查区岩石力学性质指标
Table 2. Mechanical property indexes of rocks in the exploration area
岩土名称 天然容重/
(kN·m−3)天然抗压
强度
/MPa抗拉强度
/MPa黏聚力
(饱和)
/MPa内摩擦角(饱和)
/(°)承载力特征值
/kPa基底摩擦系数 强风化泥质粉砂岩 22.0* 14.3* 0.20* 3.5* 35.0* 450 0.40 注:上述表中*根据地方经验取值。 表 3 各危岩单体稳定性计算统计表
Table 3. Stability calculation statistics of each dangerous rock mass
编号 体积/m3 破坏模式 稳定系数 安全系数 稳定性评价 天然 暴雨 地震 天然 暴雨 地震 W2-1 250.8 坠落 1.333 1.198 1.191 1.4 基本稳定 欠稳定 欠稳定 W3-1 37.3 坠落 1.236 1.192 1.196 1.4 基本稳定 欠稳定 欠稳定 W4-1 270.3 坠落 1.336 1.192 1.193 1.4 基本稳定 欠稳定 欠稳定 W4-2 53.9 倾倒 3.326 1.256 1.192 1.3 稳定 欠稳定 欠稳定 表 4 各危岩体坡段参数的取值
Table 4. Values of slope parameters of dangerous rock mass
危岩体
编号坡段岩性 法向阻尼
系数Rn切向阻尼
系数Rt滚动摩擦
系数滚动摩擦
角/(°)W2-1 强风化泥质粉砂岩 0.35 0.85 0.48 35 W3-1 强风化泥质粉砂岩 0.35 0.85 0.48 35 W4-1 强风化泥质粉砂岩 0.35 0.85 0.48 35 W4-2 强风化泥质粉砂岩 0.35 0.85 0.48 35 表 5 各危岩体运动路径与弹跳高度、总动能、速度的关系表
Table 5. Relationship between movement path of each dangerous rock body and jumping height, total kinetic energy and speed
-
[1] 胡显明,晏鄂川,杨建国,等. 巫溪南门湾危岩体稳定性分区研究[J]. 工程地质学报,2011,19(3):397 − 403. [HU Xianming,YAN Echuan,YANG Jianguo,et al. Stability assessment of unstable rock blocks at nanmenwan in Wuxi County[J]. Journal of Engineering Geology,2011,19(3):397 − 403. (in Chinese with English abstract) doi: 10.3969/j.issn.1004-9665.2011.03.016
[2] MANZELLA I,LABIOUSE V. Qualitative analysis of rock avalanches propagation by means of physical modelling of non-constrained gravel flows[J]. Rock Mechanics and Rock Engineering,2008,41(1):133 − 151. doi: 10.1007/s00603-007-0134-y
[3] ZAMBRANO O M. Large rock avalanches:A kinematic model[J]. Geotechnical and Geological Engineering,2008,26(3):283 − 287. doi: 10.1007/s10706-007-9164-1
[4] DORREN L K A,MAIER B,PUTTERS U S,et al. Combining field and modelling techniques to assess rockfall dynamics on a protection forest hillslope in the European Alps[J]. Geomorphology,2004,57(3/4):151 − 167.
[5] CROSTA G B,AGLIARDI F. A methodology for physically based rockfall hazard assessment[J]. Natural Hazards and Earth System Sciences,2003,3(5):407 − 422. doi: 10.5194/nhess-3-407-2003
[6] 何宇航,裴向军,梁靖,等. 基于Rockfall的危岩体危险范围预测及风险评价—以九寨沟景区悬沟危岩体为例[J]. 中国地质灾害与防治学报,2020,31(4):24 − 33. [HE Yuhang,PEI Xiangjun,LIANG Jing,et al. Risk assessment and range prediction of dangerous rockmass based on rockfall:A case study of the Xuangou Collapse[J]. The Chinese Journal of Geological Hazard and Control,2020,31(4):24 − 33. (in Chinese with English abstract)
[7] 程宇,张健,陈进,等. 贵州纳雍骔岭镇危岩带稳定性及危害范围分析[J]. 中国地质灾害与防治学报,2019,30(4):9 − 15. [CHENG Yu,ZHANG Jian,CHEN Jin,et al. Analysis on stability and hazard zone of dangerous rock mass in Zongling Town,Nayong of Guizhou Province[J]. The Chinese Journal of Geological Hazard and Control,2019,30(4):9 − 15. (in Chinese with English abstract)
[8] 陈洪凯,王蓉,唐红梅. 危岩研究现状及趋势综述[J]. 重庆交通学院学报,2003,22(3):18 − 22. [CHEN Hongkai,WANG Rong,TANG Hongmei. Review of current situation and trend of dangerous rock research[J]. Journal of Chongqing Jiaotong University,2003,22(3):18 − 22. (in Chinese with English abstract)
[9] 陈洪凯,唐红梅. 危岩主控结构面强度参数计算方法[J]. 工程地质学报,2008,16(1):37 − 41. [CHEN Hongkai,TANG Hongmei. Method for calculating strength parameters of structural planes controlling the rock block stablity[J]. Journal of Engineering Geology,2008,16(1):37 − 41. (in Chinese with English abstract) doi: 10.3969/j.issn.1004-9665.2008.01.008
[10] 王在泉,张黎明,贺俊征. 岩石边坡工程块体系统稳定性预测、监测与控制[J]. 岩石力学与工程学报,2004,23(10):1658 − 1661. [WANG Zaiquan,ZHANG Liming,HE Junzheng. Stability prediction,monitoring and control of key block system in rock slope engineering[J]. Chinese Journal of Rock Mechanics and Engineering,2004,23(10):1658 − 1661. (in Chinese with English abstract) doi: 10.3321/j.issn:1000-6915.2004.10.013
[11] 陈昌彦,王思敬,沈小克. 边坡岩体稳定性的人工神经网络预测模型[J]. 岩土工程学报,2001,23(2):157 − 161. [CHEN Changyan,WANG Sijing,SHEN Xiaoke. Predicting models to estimate stability of rock slope based on artificial neural network[J]. Chinese Journal of Geotechnical Engineering,2001,23(2):157 − 161. (in Chinese with English abstract) doi: 10.3321/j.issn:1000-4548.2001.02.006
[12] 董好刚,陈立德,黄长生. 三峡库区云阳—江津段危岩形成的影响因素及稳定性评价[J]. 工程地质学报,2010,18(5):645 − 650. [DONG Haogang,CHEN Lide,HUANG Changsheng. Influence factors and stability assessment of dangerous rocks in Yunyang-Jiangjin on Three Gorges Reservoir[J]. Journal of Engineering Geology,2010,18(5):645 − 650. (in Chinese with English abstract) doi: 10.3969/j.issn.1004-9665.2010.05.006
[13] 刘传正. 重庆武隆鸡尾山危岩体形成与崩塌成因分析[J]. 工程地质学报,2010,18(3):297 − 304. [LIU Chuanzheng. Mechanism analysis on the Jiweishan rockfall disaster happened in Wulong,Chongqing,June 5,2009[J]. Journal of Engineering Geology,2010,18(3):297 − 304. (in Chinese with English abstract) doi: 10.3969/j.issn.1004-9665.2010.03.002
[14] 陈洪凯,鲜学福,唐红梅,等. 危岩稳定性分析方法[J]. 应用力学学报,2009,26(2):278 − 282. [CHEN Hongkai,XIAN Xuefu,TANG Hongmei,et al. Stability analysis method for perilous rock[J]. Chinese Journal of Applied Mechanics,2009,26(2):278 − 282. (in Chinese with English abstract)
[15] 周根郯. 坠落式危岩稳定性计算方法的比较法[J]. 岩土工程学报, 2014, 34(5): 122 − 126;
ZHOU Gentan. Comparison method of calculation methods of falling dangerous rock stability[J]. Journal of Geotechnical Engineering, 2014, 34(5): 122 − 126. ( in Chinese with English abstract)
[16] 张帅,罗永健. 基于Rockfall模拟的高陡岩质建筑边坡孤石滚落防治方法探讨[J]. 广东土木与建筑,2019,26(2):54 − 57. [ZHANG Shuai,LUO Yongjian. Discussion on prevention and control method of rockfalling of high and steep rock slope based on Rockfall simulation[J]. Guangdong Architecture Civil Engineering,2019,26(2):54 − 57. (in Chinese with English abstract)
[17] 陈洪凯, 唐红梅, 叶四桥, 等. 三峡库区危岩发育链式机理及失稳运动路径研究[C]//第八次全国岩石力学与工程学术大会论文集, 2004
CHEN Hongkai, TANG Hongmei, YE Siqiao, et al. Study on chain mechanism of dangerous rock development and instability movement path in the Three Gorges Reservoir area[C]//Proceedings of the Eighth National Academic Conference on Rock Mechanics and Engineering, 2004. ( in Chinese with English abstract)
[18] 刘卫华. 高陡边坡危岩体稳定性、运动特征及防治对策研究[D]. 成都: 成都理工大学, 2008
LIU Weihua. Study on stability, movement characteristics and countermeasures of potential unstable rock mass in high-steep slope[D]. Chengdu: Chengdu University of Technology, 2008. (in Chinese with English abstract)