|
|
|
| Study on permanent displacement characteristics of seismic landslide considering vertical earthquake motion |
| HE Yuhang,PEI Xiangjun,CUI Shenghua |
| (State Key Laboratory of Geohazard Prevention and Geoenvironment Protection,Chengdu University of Technology,Chengdu,Sichuan 610059,China) |
|
|
|
|
Abstract The Daguangbao landslide(12×108 m3) is the largest landslide triggered by the Wenchuan Ms8.0 magnitude earthquake in 2008. The seismic records show that the landslide area not only suffered strong horizontal ground motions,but also received almost equal vertical ground motions. In this paper,an improved Newmark model considering vertical seismic force is used to study the influence of the shear strength parameters of the sliding surface on the earthquake permanent displacement response of the landslide. The results show that vertical ground motions increase the cumulative permanent displacement of the landslide(the maximum increase is 903%),and the contribution of vertical ground motion to the permanent displacement(cumulative total amount and cumulative rate) is significantly affected by the friction angle of the sliding surface(the influence level ranges from 87.8% to 90.7%),but is less affected by cohesion(the influence range is only 5%–27.4%). The maximum cumulative rate and duration of the permanent displacement of the landslide during the seismic process are determined by the concentrated release period of the seismic energy,and 50% of the energy is released within 30–50 s during the 120 s earthquake holding time in the Daguangbao landslide area. It is inferred that the instability of Daguangbao landslide may be in the early stage of earthquake. The improved Newmark method used in this paper can be used to evaluate the contribution of vertical ground motion to the initiation of the seismic landslide.
|
|
|
|
|
|
| [1] 罗 强,赵炼恒,李 亮,等. 地震效应和坡顶超载对均质土坡稳定性影响的拟静力分析[J]. 岩土力学,2010,31(12):3 835–3 842.(LUO Qiang,ZHAO Lianheng,LI Liang,et al. Quasi-static stability analysis of homogeneous soil slopes under effect of surcharge and earthquake[J]. Rock and Soil Mechanics,2010,31(12):3 835–3 842.(in Chinese))
[2] 胡 成,卢坤林,朱大勇,等. 三维边坡拟静力抗震稳定性分析[J]. 岩石力学与工程学报,2011,30(增1):2 904–2 912.(HU Cheng,LU Kunlin,ZHU Dayong,et al. Analysis of pseudo-static seismic stability for three-dimensional slope[J]. Chinese Journal of Rock Mechanics and Engineering,2011,30(Supp.1):2 904–2 912.(in Chinese))
[3] 吕擎峰,殷宗泽,王叔华,等. 拟静力法边坡稳定分析的改进[J]. 岩土力学,2005,26(增1):35–38.(LU Qingfeng,YIN Zongze,WANG Shuhua,et al. Improvement of pseudo-static method for slope stability analysis[J]. Rock and Soil Mechanics,2005,26(Supp.1):35–38.(in Chinese))
[4] 朱亚林,孔宪京,邹德高,等. 高土石坝地震反应和破坏机理分析[J]. 岩土工程学报,2010,32(9):1 362–1 367.(ZHU Yalin,KONG Xianjing,ZOU Degao,et al. Dynamic response and failure mechanism of high earth-rockfill dams[J]. Chinese Journal of Geotechnical Engineering,2010. 32(9):1 362–1 367.(in Chinese))
[5] NEWMARK N M. Effects of earthquakes on dams and embankments[J]. Geotechnique,1965,15(2):139–160.
[6] WILSON R C,KEEFER D K.Dynamic analysis of a slope failure from the 6 August 1979 Coyote lake,California,earthquake[J]. Bulletin of Engineering Geology and the Environment,1983,73(3):863–877.
[7] WARTMAN J,BRAY J D,SEED R B. Inclined plane studies of the Newmark sliding block procedure.[J]. Journal of Geotechnical and Geoenvironmental Engineering,129:673–684.
[8] 邵龙潭,唐洪祥,孔宪京,等. 随机地震作用下土石坝边坡的地震稳定性分析[J]. 水利学报,1999,26(11):66–71.(SHAO Longtan,TANG Hongxiang,KONG Xianjin,et al. Finite element analysis for slope stability of earth-rock dam under the action of stochastic seismic[J]. Journal of Hydraulic Engineering,1999,26(11):66–71.(in Chinese))
[9] 刘立平,雷尊宇,周富春. 地震边坡稳定分析方法综述[J]. 重庆交通学院学报,2001,20(3):83–88.(LIU Liping,LEI Zunyu,ZHOU Fuchun. The evaluation of seismic slope stability analysis methods[J]. Journal of Chongqing Jiaotong University,2001,20(3):83–88.(in Chinese))
[10] 沈珠江,陆培炎. 评当前岩土工程实践中的保守倾向[J]. 岩土工程学报,1997,19(4):115–118.(SHEN Zhujiang,LU Peiyan. On the conservative tendency in geotechnical engineering practice[J]. Chinese Journal of Geotechnical Engineering,1997,19(4):115–118.(in Chinese))
[11] 刘红帅,薄景山,刘德东. 岩土边坡地震稳定性分析研究评述[J]. 地震工程与工程振动,2005,25(1):165–172.(LIU Hongshuai,BO Jingshan,LIU Dedong. Review on study of seismic stability analysis of rock-soil slopes[J]. Earthquake Engineering and Engineering Vibration,2005,25(1):165–172.(in Chinese))
[12] MAKDISI F I,SEED H B. Simplified procedure for estimation dam and embankment earthquake induced deformations[J]. Journal of the Geotechnical Engineering Division,ASCE,1978,104(GT7):849–868.
[13] 李红军,迟世春,林 皋. 基于黏着滑动耦合动力分析的Newmark 滑块位移法[J]. 岩石力学与工程学报,2007,26(9):1 787–1 793.(LI Hongjun,CHI Shichun,LIN Gao. An improved Newmark sliding block method based on stick-slip coupled dynamic response[J]. Chinese Journal of Rock Mechanics and Engineering,2007,26(9):1 787–1 793.(in Chinese))
[14] HUANG C C. Influence of surface-normal ground acceleration on the initiation of the Jih-Feng-Erh-Shan Landslide during the 1999 Chi-Chi,Taiwan,Earthquake[J]. Bulletin of the Ssmological Society of America,2001,91(5):953–958.
[15] INGLES J,JOSé DARROZES,SOULA J C. Effects of the vertical component of ground shaking on earthquake-induced landslide displacements using generalized Newmark analysis[J]. Engineering Geology,2006,86(2-3):134–147.
[16] YUAN R M,TANG C L,DENG Q H. Effect of the acceleration component normal to the sliding surface on earthquake-induced landslide triggering[J]. Landslides,2015,12(2):335–344.
[17] 许 强,裴向军,黄润秋. 汶川地震大型滑坡研究[M]. 北京:科学出版社,2009:53–91.(XU Qiang,PEI Xiangjun,HUANG Runqiu. A study on large-scale landslide in Wenchuan Earthquake[M]. Beijing:Science Press,2009:53–91.(in Chinese))
[18] 黄润秋,裴向军,李天斌. 汶川地震触发大光包巨型滑坡基本特征及形成机理分析[J]. 工程地质学报,2008,16(6):12–23.(HUANG Runqiu,PEI Xiangjun,LI Tianbin. Basic characteristics and formation mechanism of the largest scale landslide at Daguangbao occurred during wenchuan earthquake[J]. Journal of Engineering Geology,2008,16(6):12–23.(in Chinese))
[19] 崔圣华,裴向军,黄润秋,等. 大光包滑坡不连续地质特征及其工程地质意义[J]. 西南交通大学学报,2019,54(1):65–76.(CUI Shenghua,PEI Xiangjun,HUANG Runqiu,et al. Discontinuities and engineering geological significances of strong earthquake-induced Daguangbao Landslide[J]. Journal of Southwest Jiaotong University,2019,54(1):65–76.(in Chinese))
[20] 黄润秋,张伟锋,裴向军. 大光包滑坡工程地质研究[J]. 工程地质学报,2014,22(4):557–585.(HUANG Runqiu,ZHANG Weifeng,PEI Xiangjun. Engineering geological study on Daguangbao landslide[J]. Journal of Engineering Geology,2014,22(4):557–585.(in Chinese))
[21] 张伟锋,黄润秋,裴向军. 大光包滑坡运动特征及其过程分析[J]. 工程地质学报,2015,23(5):866–885.(ZHANG Weifeng,HUANG Runqiu,PEI Xiangjun. Analysis on kinematics characteristics and movement process of Daguangbao landslide[J]. Journal of Engineering Geology,2015,23(5):866–885.(in Chinese))
[22] 黄润秋,裴向军,崔圣华. 大光包滑坡滑带岩体碎裂特征及其形成机制研究[J]. 岩石力学与工程学报,2016,35(1):1–15.(HUANG Runqiu,PEI Xiangjun,CUI Shenghua. Cataclastic characteristics and formation mechanism of rock mass in sliding zone of Daguangbao landslide[J]. Chinese Journal of Rock Mechanics and Engineering,2016,35(1):1–15.(in Chinese))
[23] 崔圣华. 强震巨型滑坡滑带碎裂岩体微细观分析及静动力破损机制研究[硕士学位论文][D]. 成都:成都理工大学,2014.(CUI Shenghua. Microstructure and static dynamics damage mechanism of the sliping cataclastic rock of the largest scale landslide-a case of Daguangbao landslide in Anxian[M. S. Thesis][D]. Chengdu:Chengdu University of Technology,2014.(in Chinese))
[24] WANG G H,SASSA K. Seismic loading impacts on excess pore-water pressure maintain landslide triggered flowslides[J]. Earth Surface Processes and Landforms,2009,34(2):232–241.
[25] WILSON R C,KEEFER D K. Dynamic analysis of a slope failure from the 6 August 1979 Coyote Lake,California,earthquake[J]. Bulletin of the Seismological Society of America,1983,73(3):863–877.
[26] TRIFUNAC M D. Energy of strong motion at earthquake source [J]. Soil Dynamics and Earthquake Engineering,2008,28(1):1–6.
[27] TRIFUNAC M D,BRADY A G. A study on the duration of strong earthquake ground motion[J]. Bulletin of the Seismological Society of America,1975,65(3):581–626.
[28] 孟祥瑞,裴向军,黄润秋,等. 大光包滑坡层间错动带岩体剪切特性研究[J]. 工程地质学报,2018,26(2):34–43.(MENG Xiangrui,PEI Xiangjun,HUANG Runqiu,et al. Shear behaviors of rock mass in the interlayer fault zone of Daguangbao landslide[J]. Journal of Engineering Geology,2018,26(2):34–43.(in Chinese))
[29] 裴向军,崔圣华,黄润秋. 大光包滑坡启动机制:强震过程滑带动力扩容与水击效应[J]. 岩石力学与工程学报,2018,37(2):430–448.(PEI Xiangjun,CUI Shenghua,HUANG Runqiu. A model of initiation of Daguangbao landslide:dynamic dilation and water hammer in sliding zone during strong seismic shaking[J]. Chinese Journal of Rock Mechanics and Engineering,2018,37(2):430–448.(in Chinese))
[30] 崔圣华. 强震过程软弱层带地震动响应及大型滑坡启动机制研究[J]. 岩石力学与工程学报,2018,37(6):1 560.(CUI Shenghua. Seismic response of wake interlayer and initiation mechanisms of large landslides during strong earthquake[J]. Chinese Journal of Rock Mechanics and Engineering,2018,37(6):1 560.(in Chinese))
[31] 冯文凯,王 琦,张光鑫,等. Hoek-Brown准则的改进及在大光包滑坡滑带碎裂岩体力学强度评价中的应用[J]. 岩石力学与工程学报,2017,36(增1):335–342.(FENG Wenkai,WANG Qi,ZHANG Guangxin,et al. Improvement of Hoek-Brown criterion and application of landslide zone of cataclastic rock mass mechanical strength in evaluation of Daguangbao landslide[J]. Chinese Journal of Rock Mechanics and Engineering,2017,36(Supp.1):335–342.(in Chinese))
[32] 朱 雷,王小群. 大型岩质滑坡地震变形破坏过程物理试验与数值模拟研究[J]. 工程地质学报,2013,21(2):228–235.(ZHU Lei,WANG Xiaoqun. Physical modelling and numerical simulation of deformation and failure process of large rockslide in earthquake[J]. Journal of Engineering Geology,2013,21(2):228–235.(in Chinese))
[33] 李天涛,裴向军,黄润秋. 强震触发大光包巨型滑坡运动特征研究[J]. 水文地质工程地质,2014,41(2):122–127.(LI Tiantao,PEI Xiangjun,HUANG Runqiu. A study of motion features of the Daguangbao large-scale landslide induced by the Wenchuan Earthquake[J]. Hydrogeology and Engineering Geology,2014,41(2):122–127.(in Chinese))
[34] 殷跃平,王 猛,李 滨,等. 汶川地震大光包滑坡动力响应特征研究[J]. 岩石力学与工程学报,2012,31(10):29–42.(YIN Yueping,WANG Meng,LI Bin,et al. Dynamic Response Characteristics of Daguangbao Landslide triggered by Wenchuan Earthquake[J]. Chinese Journal of Rock Mechanics and Engineering,2012,31(10):29–42.(in Chinese))
[35] 王 琦. 大光包震旦系灯影组顺层剪切带强度特性研究[硕士学位论文][D]. 成都:成都理工大学,2017.(WANG Qi. Strength characteristics of Sinian Dengying formation in bedding shear zone of Daguangbao landslide[M. S. Thesis][D]. Chengdu:Chengdu University of Technology,2017.(in Chinese))
[36] 冯文凯,易小宇,葛 华,等. 大光包滑坡滑带碎裂岩体原位钻孔剪切试验研究[J]. 岩土工程学报,2017,39(9):1 718–1 723.(FENG Wenkai,YI Xiaoyu,GE Hua,et al. In-situ borehole shear test on cataclastic rock mass of Daguangbao landslide[J]. Chinese Journal of Geotechnical Engineering,2017,39(9):1 718–1 723.(in Chinese))
[37] DONG J J,TSAO C C,YANG C M. The geometric characteristics and initiation mechanisms of the earthquake-triggered Daguangbao Landslide[J]. Geotechnical Hazards from Large Earthquakes and Heavy Rainfalls,2016,(9):203–213.
[38] 崔圣华,裴向军,黄润秋. 大光包滑坡启动机制:强震过程滑带非协调变形与岩体动力致损[J]. 岩石力学与工程学报,2019,38(2):237–253.(CUI Shenghua,PEI Xiangjun,HUANG Runqiu. An initiation model of DGB landslide:non-coordinated deformation inducing rock damage in sliding zone during strong seismic shaking[J]. Chinese Journal of Rock Mechanics and Engineering,2019,38(2):237–253.(in Chinese))
[39] WIECZOREK G F,WILSON R C,HARP E L. Map showing slope stability during earthquakes in San Mateo County,California[J]. Annals of the New York Academy of Ences,1985,681(6431):155–164.
|
|
|
|