Study on structural deformation characteristics and surface crack distribution of girder tunnel across Lenglongling fault caused by Menyuan earthquake#br#
ZHANG Yufang1,YUAN Kun1,ZHOU Wenjiao1,FAN Jiawei2
(1. Railway Engineering Research Institute,China Academy of Railway Sciences,Beijing 100081,China;2. China Academy of Railway Sciences,Beijing 100081,China)
Abstract:In order to explore the deformation characteristics and stress mechanism of tunnel structure under the dislocation of strike-slip fault,and clarify the mechanical status of strike-slip fault,the distribution rules of surface cracks caused by earthquake in Daliang tunnel are analysed by means of field investigation,geomechanical analysis and numerical simulation. The results show that:(1) the strike of the fault is NW60°,which is consistent with the location of the Lenglongling fault in the region and belongs to the Holocene Active fault. The occurrence of the interrupted layer of the tunnel is 195°∠79°,the width of weak layer is about 100 m,and the size of surface crack dislocation is 3 m. About 700 m to the south of the exit of Daliang tunnel,the horizontal displacement is 2.8 m,and the thrust displacement is 0.91 m,which has the characteristics of thrust strike-slip movement. (2) The mechanical mode of seismic failure is the combined action of NE-SW60° principal stress,unidirectional compression and pure shear. Considering the characteristics of thrust surface deformation at the boundary of the main fracture zone,the surface fractures have a thrust fault orogenic flower shape. (3) Through the analysis of geomechanics,under unidirectional force and moment on the fault,the distribution law of cracks on the surface is consistent with that of field investigation. (4) Before the Menyuan earthquake,the deformation and failure mode of Daliang tunnel was mainly affected by the regional principal compression stress on the direction of on SW60°. After the Menyuan earthquake,it was mainly affected by shearing and compression,and the tunnel structure was subjected to the principal compression stress on the direction of NE-SW60° and the strike-slip shear on the direction of NW60° accorded with Lenglongling fault. The investigation and analysis results provide a reference for the engineering design of high-speed railway tunnels crossing active faults.
张玉芳1,袁 坤1,周文皎1,范家玮2. 门源地震对跨冷龙岭断层的大梁隧道结构变形特征和地表裂缝分布规律研究[J]. 岩石力学与工程学报, 2023, 42(5): 1055-1069.
ZHANG Yufang1,YUAN Kun1,ZHOU Wenjiao1,FAN Jiawei2. Study on structural deformation characteristics and surface crack distribution of girder tunnel across Lenglongling fault caused by Menyuan earthquake#br#. , 2023, 42(5): 1055-1069.
[1] 贾俊峰,杜修力,韩 强. 近断层地震动特征及其对工程结构影响的研究进展[J]. 建筑结构学报,2015,36(1):1–12.(JIA Junfeng,DU Xiuli,HAN Qiang. A state-of-the-art review of near-fault earthquake ground motion characteristics and effects on engineering structures[J]. Journal of Building Structures,2015,36(1):1–12.(in Chinese))
[2] 汪 振,钟紫蓝,黄景琦,等. 走滑断层错动下山岭隧道关键断面变形及损伤演化[J]. 建筑结构学报,2020,41(增1):425–434.(WANG Zhen,ZHONG Zilan,HUANG Jingqi,et al. Deformation and damage evolution of critical cross section of mountain tunnels under strike-slip fault movement[J]. Journal of Building Structures,2020,41(Supp.1):425–434.(in Chinese))
[3] 雷东宁,刘 杰,刘姝妹,等. 2016年1月21日青海门源M 6.4地震发震构造模式[J]. 地震地质,2018,40(2):107–120.(LEI Dongning,LIU Jie,LIU Jianmei,et al. Seismogenic tectonic model of the Menyuan M 6.4 earthquake in Qinghai on January 21,2016[J]. Seismogeology,2018,40(2):107–120.(in Chinese))
[4] 姜文亮,李永生,田云锋,等. 冷龙岭地区2016年青海门源6.4级地震发震构造特征[J]. 地震地质,2017,39(3):536–549.(JIANG Wenliang,LI Yongsheng,TIAN Yunfeng,et al. Research of seismogenic structure of the Menyuan MS 6.4 earthquake on January 21,2016 in Lenglongling area of NE Tibetan plateau[J]. Seismology and Geology,2017,39(3):536–549.(in Chinese))
[5] 赵 颖,郭恩栋,刘 智,等. 走滑断层位错作用下城市铁隧道损伤分析[J]. 岩土力学,2014,35(增2):467–473.(ZHAO Ying,GUO Endong,LIU Zhi,et al. Damage analysis of urban metro tunnel under strike-slip fault[J]. Rock and Soil Mechanics,2014,35(Supp.2):467–473.(in Chinese))
[6] 刘学增,王煦霖,林亮伦. 60°倾角正断层黏滑错动对山岭隧道影响的试验研究[J]. 土木工程学报,2014,47(2):121–128.(LIU Xuezeng,WANG Xulin,LIN Lianglun. Model experimental study on influence of normal fault with 60° dip angle stick-slip dislocation on mountain tunnel[J]. China Civil Engineering Journal,2014,47(2):121–128.(in Chinese))
[7] 刘学增,林亮伦. 75°倾角逆断层黏滑错动对公路隧道影响的模型试验研究[J]. 岩石力学与工程学报,2011,30(12):2 523–2 530.(LIU Xuezeng,LIN Lianglun. Research on model experiment of effect of thrust fault with 75° dip angle stick-slip dislocation on highway tunnel[J]. Chinese Journal of Rock Mechanics and Engineering,2011,30(12):2 523–2 530.(in Chinese))
[8] 刘学增,王煦霖,林亮伦. 75°倾角正断层黏滑错动对公路隧道影响的模型试验研究[J]. 岩石力学与工程学报,2013,32(8):1 714–1 720. (LIU Xuezeng,WANG Xulin,LIN Lianglun. Model experiment on effect of normal fault with 75° dip angle stick-slip dislocation on highway tunnel[J]. Chinese Journal of Rock Mechanics and Engineering,2013,32(8):1 714–1 720.(in Chinese))
[9] LIU X Z,LI X F,SANG Y,et al. Experimental study on normal fault rupture propagation in loose strata and its impact on mountain tunnels[J]. Tunnelling and Underground Space Technology,2015,49:417–425.
[10] 汪 振,钟紫蓝,赵 密,等. 正断型断裂模拟及其对山岭隧道影响研究[J]. 岩土工程学报,2020,42(10):1 876–1 884.(WANG Zhen,ZHONG Zilan,ZHAO Mi,et al. Simulation of normal fault rupture and its impact on mountain tunnels[J]. Chinese Journal of Geotechnical Engineering,2020,42(10):1 876–1 884.(in Chinese))
[11] 邓起东,于贵华,叶文华. 地震地表破裂参数与震级关系的研究[M]. 北京:地震出版社,1992:247–263.(DENG Qidong,YU Guihua,YE Wenhua. Relationship between earthquake magnitude and parameters of surface ruptures associated with historical earthquakes[M]. Beijing:Seismological Press,1992:247–263.(in Chinese))
[12] 郭 鹏,韩竹军,安艳芬,等. 冷龙岭断裂系活动性与2016年门源6.4级地震构造研究[J]. 中国科学:地球科学,2017,47(5):617–630.(GUO Peng,HAN Zhujun,AN Yanfen,et al. Activity of the Lenglongling fault system and seismotectonics of the 2016 MS 6.4 Menyuan earthquake[J]. Scientia Sinica(Terrae),2017,47(5):617–630.(in Chinese))
[13] 何文贵,刘百篪,袁道阳,等. 冷龙岭活动断裂的滑动速率研究[J]. 西北地震学报,2000,22(1):90–97.(HE Wengui,LIU Baichi,YUAN Daoyang,et al. Research on slip rates of the Lenglongling active fault zone[J]. Northwestern Seismological Journal,2000,22(1):90–97.(in Chinese))
[14] 高 帆. 北祁连山冷龙岭断裂东段断错地貌、滑动速率与构造意义[硕士学位论文][D]. 北京:中国地震局地质研究所,2021.(GAO Fan. Faulted landforms,slip-rate,and tectonic implications of the eastern Lenglongling fault,northeastern Tibetan Plateau[M. S. Thesis][D]. Beijing:Institute of Geology,China Earthquake Administration,2021.(in Chinese))
[15] 郭 鹏,韩竹军,姜文亮,等. 青藏高原东北缘冷龙岭断裂全新世左旋滑动速率[J]. 地震地质,2017,39(2):323–341.(GUO Peng,HAN Zhujun,JIANG Wenliang,et al. Holocene Left-lateral slip rate of the Lenglongling fault,Northeastern margin of the Tibetan plateau[J]. Seismology and Geology,2017,39(2):323–341.(in Chinese))
[16] 张培震,李传友,毛凤英. 河流阶地演化与走滑断裂滑动速率[J]. 地震地质,2008,30(1):44–57.(ZHANG Peizhen,LI Chuanyou,MAO Fengying. Strath terrace formation and strike-slip faulting[J]. Seismology and Geology,30(1):44–57.(in Chinese))
[17] 康建成,朱俊杰,陈宏凯. 祁连山冷龙岭南坡晚第四纪冰川演化序列[J]. 冰川冻土,1992,14(4):352–359.(KANG Jiancheng,ZHU Junjie,CHEN Hongkai. Late Quaternary glacial sequence on the south slope of the Lenglongling,Qilian Mountains[J]. Journal of Glaciology and Geocryology,1992,14(4):352–359.(in Chinese))
[18] 王成虎,高桂云,杨树新,等. 基于中国西部构造应力分区的川藏铁路沿线地应力的状态分析与预估[J]. 岩石力学与工程学报,2019,38(11):2 422–2 433.(WANG Chenghu,GAO Guiyun,YANG Shuxin, et al. Analysis and prediction of stress fields of Sichuan—Tibet railway area based on contemporary tectonic stress field zoning in Western China[J]. Chinese Journal of Rock Mechanics and Engineering,2019,38(11):2 422–2 433.(in Chinese))
[19] 徐纪人,赵志新. 青藏高原及其周围地区区域应力场与构造运动特征[J]. 中国地质,2006,33(2):275–285.(XU Jiren,ZHAO Zhixin. Characteristics of the regional stress field and tectonic movement on the Qinghai—Tibet Plateau and in its surrounding areas[J]. Geology in China,2006,33(2):275–285.(in Chinese))
[20] 舒塞兵,谢富仁. 青藏高原北东边缘第四纪构造应力场转变的有关地质证据[C]// 地壳构造与地壳应力文集. [S. l.]:[s. n.],2000:61–65.(SHU Saibing,XIE Furen. Geological Evidences of the Grand Transformation in the Tectonic Stress Field in Northeastern Margin of the Qinghai-Tibet Plateau[C]// Proceedings of Crustal Structure and Crustal Stress. [S. l.]:[s. n.],2000:61–65.(in Chinese))