Failure and deformation mode for soil and tunnel structure crossing multiple slip surfaces of strike-slip fault in model test

被引:10
作者
Zhang, Xi [1 ]
Shen, Yusheng [1 ,2 ]
Qiu, Jutao [1 ]
Chang, Mingyu [1 ]
Zhou, Pengfa [1 ]
Huang, Haifeng [1 ]
Zhu, Penglin [1 ]
机构
[1] Southwest Jiaotong Univ, Minist Educ, Key Lab Transportat Tunnel Engn, Chengdu 610031, Sichuan, Peoples R China
[2] Southwest Jiaotong Univ, Natl Engn Res Ctr Geol Disaster Prevent Technol La, Chengdu 610031, Sichuan, Peoples R China
关键词
Tunnel engineering; Fault fracture zone; Multiple slip surfaces; Deformation and failure mode; Fortification length; Model test; DAMAGE; ZONE; EARTHQUAKE; MOUNTAIN; BEHAVIOR; GEOMETRY;
D O I
10.1016/j.soildyn.2024.108541
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Relying on the tunnel engineering crossing large active fault fracture zone in high intensity seismic area in Western China, a large-scale model test of tunnel through multiple slip surfaces under strike slip motion was carried out. The deformation patterns and damage characteristics of tunnel structure and surrounding rock were studied based on displacement, strain and internal force response, as well as crack morphology. The results revealed that microscopically the model soil experienced the process of contacting, compaction and relative movement under fault dislocation, and was macroscopically accompanied with fracture occurring, and further expansion. Compared with fault movement form containing single slip surface, the active wall produced nonlinear linkage displacement to fault fracture zone when there existed multiple slip surfaces. The model soil exhibited a multistage dislocation along longitudinal direction after test. The dislocation of model soil on both sides of major slip surfaces reached to 25.9 mm and 18.8 mm, which was about 2.2-3.4 times of the dislocation on both sides of the minor slip surfaces in fault fracture zone. The overall deflection of lining segments and the torsion of flexible joints corporately undertook the fault dislocation. Lining segments near the major slip surfaces had opposite trends of tensile and compressive deformation, where the failure of tensile bending damage was dominant. Tunnel segments near minor slip surfaces underwent integral linear deflection along with surrounding rock, and were less affected by fault dislocation. The fragile sections of tunnel structure were located near main slip surfaces, the fragile parts were invert, arch springing and arch spandrel, which were mainly damaged by tensile, compressive and shear affection. Based on the deflection corner beta of each lining segment, combined with damage pattern and internal force distribution trend, it is suggested that 2d similar to 3d (d represents the span of tunnel) in range near major slip surfaces is the main affected zone, while the range of 4d in the middle of fault fracture zone is the minor affected zone. The partitioned fortification needs to be adopted when tunnel is to cross fault fracture zone.
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页数:16
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