強(qiáng)震區(qū)隧道工程地震響應(yīng)特征分析
[Abstract]:With the development of modernization in China, tunnels and underground projects in many areas will inevitably encounter problems near active faults or in high-intensity seismic areas. Therefore, it is of profound social significance to study the seismic response characteristics of regional tunnel stability in seismic zone. In order to study the influence of earthquake on tunnel, this paper first summarizes the damage form and influencing factors of tunnel by combining with the examples of tunnel damage caused by large earthquakes at home and abroad, and then summarizes the damage form and influencing factors of tunnel caused by earthquake. Based on the study of the relationship between magnitude and surface rupture of Wells et al., combined with the earthquake damage of tunnel in Wenchuan earthquake, the aseismic design method of tunnel is analyzed. The influence of incident angle of seismic wave on tunnel is simulated by using 3D finite element software ANSYS. Finally, the variation of ground stress before and after Kunlun Mountain, Wenchuan and Hanshin earthquakes is analyzed. The influence law of ground stress change on tunnel before and after Wenchuan earthquake was simulated by using 3D finite element software 3D-sigma. Based on the above studies, the preliminary conclusions and progress of the paper are as follows: (1) through the research of tunnel damage cases in large earthquakes at home and abroad, Combined with the earthquake damage of the tunnel in Wenchuan earthquake, the damage forms of the tunnel and underground engineering are summarized. The main failure modes of the tunnel body are: (1) shear dislocation of lining, (2) longitudinal cracking of lining, Ring cracking of lining, diagonal cracking of lining, uplift of bottom plate, etc. The failure modes of the orifice and portal are as follows: (1) rock collapse, (2) landslide extrusion, (2) crack of the end wall, etc. (2) it is found that, The parameter directly related to the seismic design of underground engineering and tunnel is the surface rupture length SRL (km), the largest coearthquake rupture displacement MD (m), average co-seismic rupture displacement AD (m). At the time of Wenchuan earthquake, the secondary faults between the central fault and Longmenshan fault will also produce certain activities, so the earthquake damage of three tunnels between the two faults is very serious. It can be seen that the subsidiary faults near the seismogenic faults will also produce co-seismic displacement during the earthquake, and will destroy the underground structure and the tunnel. (3) from the simulation results, the magnitude of the stress at the different monitoring points of the tunnel is different in terms of the principal stress. The position of arch shoulder and arch foot are affected by the maximum and minimum principal stress, and the maximum and minimum principal stress of arch top and arch bottom are smaller. The arch foot and arch roof are seriously affected by the earthquake, which is consistent with the actual earthquake damage in the middle tunnel. (4) by comparing the magnitude of the ground stress before and after the Kunlun Mountain, Wenchuan and Hanshin earthquakes, it is found that the earthquake can cause the decrease of the magnitude of the earth stress in the epicenter area. The influence of the variation of ground stress before and after the earthquake on the tunnel stability is simulated by using the three-dimensional finite element software 3D-sigma. The results show that the maximum principal stress and the minimum principal stress at the monitoring point of the tunnel section after the earthquake are smaller than those before the earthquake. The influence of earthquake on the left and right arches of the tunnel is the most obvious, followed by the left and right arches, and the arch roof and the arch bottom are the least affected by the earthquake.
【學(xué)位授予單位】:中國(guó)地震局地殼應(yīng)力研究所
【學(xué)位級(jí)別】:碩士
【學(xué)位授予年份】:2015
【分類號(hào)】:U452.28;P315.9
【參考文獻(xiàn)】
相關(guān)期刊論文 前10條
1 雷謙榮;地震帶的隧道開挖[J];地下空間;1994年02期
2 肖林萍;李永樹;趙玉光;;基于有限元法的隧道圍巖壓力計(jì)算與分析方法研究[J];地礦測(cè)繪;2008年02期
3 李方全,王連捷;華北地區(qū)地應(yīng)力測(cè)量[J];地球物理學(xué)報(bào);1979年01期
4 郭U_良;王成虎;馬洪生;王崇艮;;汶川M_S8.0級(jí)大震前后的水壓致裂原地應(yīng)力測(cè)量[J];地球物理學(xué)報(bào);2009年05期
5 龍鋒;聞學(xué)澤;徐錫偉;;華北地區(qū)地震活斷層的震級(jí)-破裂長(zhǎng)度、破裂面積的經(jīng)驗(yàn)關(guān)系[J];地震地質(zhì);2006年04期
6 冉洪流;;中國(guó)西部走滑型活動(dòng)斷裂的地震破裂參數(shù)與震級(jí)的經(jīng)驗(yàn)關(guān)系[J];地震地質(zhì);2011年03期
7 葉文華,,徐錫偉,汪良謀;中國(guó)西部強(qiáng)震的地表破裂規(guī)模與震級(jí)、復(fù)發(fā)時(shí)間間隔關(guān)系的研究[J];地震地質(zhì);1996年01期
8 王成虎;張彥山;熊玉珍;孔德虎;;喀什河水電站工程區(qū)構(gòu)造穩(wěn)定性研究[J];地質(zhì)力學(xué)學(xué)報(bào);2008年02期
9 羅利銳;劉志剛;;斷層對(duì)隧道圍巖穩(wěn)定性的影響[J];地質(zhì)力學(xué)學(xué)報(bào);2009年03期
10 劉志剛,崔洪慶,孫殿卿;斷裂多期活動(dòng)及其研究意義[J];地質(zhì)力學(xué)學(xué)報(bào);1995年01期
相關(guān)會(huì)議論文 前1條
1 何川;耿萍;晏啟祥;;汶川大地震隧道工程震害初步分析[A];汶川大地震工程震害調(diào)查分析與研究[C];2009年
相關(guān)碩士學(xué)位論文 前3條
1 呂淑杰;隧道地震反應(yīng)若干影響因素研究[D];大連理工大學(xué);2007年
2 唐錁;山嶺隧道洞口段地震動(dòng)力響應(yīng)影響因素規(guī)律研究[D];西南交通大學(xué);2009年
3 趙占雷;地震區(qū)山嶺隧道地震動(dòng)力響應(yīng)影響因素規(guī)律及減震措施研究[D];北京交通大學(xué);2012年
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