Numerical analysis of surface subsidence in asymmetric parallel highway tunnels

被引:75
作者
Das, Ratan [1 ]
Singh, P. K. [1 ]
Kainthola, Ashutosh [2 ]
Panthee, Suman [1 ,3 ]
Singh, T. N. [1 ]
机构
[1] Indian Inst Technol, Dept Earth Sci, Bombay 400076, Maharashtra, India
[2] Natl Inst Technol, Dept Civil Engn, Srinagar, Jammu & Kashmir, India
[3] Tribhuvan Univ, Cent Dept Geol, Kirtipur, Nepal
关键词
Twin tunnels; Numerical analysis; Stability; Finite element method (FEM); Subsidence; TWIN-TUNNELS; SHALLOW TUNNELS; STABILITY ANALYSIS; ROCK MASSES; CONSTRUCTION; SETTLEMENT; BEHAVIOR; DEFORMATION; PARAMETERS; MOVEMENTS;
D O I
10.1016/j.jrmge.2016.11.009
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Tunnelling related hazards are very common in the Himalayan terrain and a number of such instances have been reported. Several twin tunnels are being planned for transportation purposes which will require good understanding for prediction of tunnel deformation and surface settlement during the engineering life of the structure. The deformational behaviour, design of sequential excavation and support of any jointed rock mass are challenging during underground construction. We have raised several commonly assumed issues while performing stability analysis of underground opening at shallow depth. For this purpose, Kainchi-mod Nerchowck twin tunnels (Himachal Pradesh, India) are taken for in-depth analysis of the stability of two asymmetric tunnels to address the influence of topography, twin tunnel dimension and geometry. The host rock encountered during excavation is composed mainly of moderately to highly jointed grey sandstone, maroon sandstone and siltstones. In contrast to equidimensional tunnels where the maximum subsidence is observed vertically above the centreline of the tunnel, the result from the present study shows shifting of the maximum subsidence away from the tunnel centreline. The maximum subsidence of 0.99 mm is observed at 4.54 m left to the escape tunnel centreline whereas the maximum subsidence of 3.14 mm is observed at 8.89 m right to the main tunnel centreline. This shifting clearly indicates the influence of undulating topography and inequidimensional noncircular tunnel. (C) 2017 Institute of Rock and Soil Mechanics, Chinese Academy of Sciences. Production and hosting by Elsevier B.V.
引用
收藏
页码:170 / 179
页数:10
相关论文
共 50 条
[1]  
Addenbrooke T.I., 2001, INT J GEOMECH, V1, P249, DOI [DOI 10.1061/(ASCE)1532-3641(2001)1:2(249), 10.1061/(asce)1532-3641(2001)1:2(249)]
[2]  
Ameri M., 2009, Asian Journal of Applied Sciences, V2, P197, DOI DOI 10.3923/AJAPS.2009.197.210
[3]  
[Anonymous], 2012, GEOLOGY MINERAL RESO
[4]  
Attewell P., 1985, GROUND ENG, V18, P17
[5]   Engineering geological characterization of low strength anisotropic rocks in the Himalayan region for assessment of tunnel support [J].
Bhasin, R ;
Barton, N ;
Grimstad, E ;
Chryssanthakis, P .
ENGINEERING GEOLOGY, 1995, 40 (3-4) :169-193
[6]  
Bieniawski Z.T., 1989, ENG ROCK MASS CLASSI
[7]   Analytical solutions for shallow tunnels in saturated ground [J].
Bobet, A .
JOURNAL OF ENGINEERING MECHANICS, 2001, 127 (12) :1258-1266
[8]  
Brown E.T., 1981, Rock characterization, Testing and monitoring, ISRM suggested methods
[9]   Determination of residual strength parameters of jointed rock masses using the GSI system [J].
Cai, M. ;
Kaiser, P. K. ;
Tasaka, Y. ;
Minami, M. .
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 2007, 44 (02) :247-265
[10]  
Carroll WF., 1998, A Primer for finite elements in elastic structures