Characteristics, causes and control measures of disasters for the soft-rock tunnels in the Wenchuan seismic regions

The Guang(yuan)–Gan(su) Expressway is located in the core areas where the Wenchuan earthquake occurred. The surrounding soft-rocks of several tunnels in this region, such as the Dujiashan and Yangjiashan tunnels, are mainly broken into phyllites due to the severe action of the earthquake. Through analyzing the effects of large deformations, lining damage and collapses, which happen frequently in the soft-rock tunnels in the Guang–Gan Expressway, the characteristics and causes of such geological disasters are obtained. It is demonstrated that the large deformation and collapse occur near the vault and tunnel face. The poor mechanical properties and weak self-bearing capacity of the surrounding rock and the softening caused by groundwater are important contributing factors to these disasters. The lack of experience in the design and construction of tunnels in the meizoseismal area, as well as the aftershocks are other important factors to consider. Field test results indicate that the three-bench and the reserved core soil construction method should be applied to control the stability of broken phyllite tunnels, and that this key technology should be strictly controlled during its construction. In particular, increasing the stiffness of the supporting structure and enclosing of the lining in time are efficient methods to control large deformations and collapses in soft-rock tunnels in the meizoseismal area.

[1]  Song Yuan,et al.  Investigation and assessment on mountain tunnels and geotechnical damage after the Wenchuan earthquake , 2009 .

[2]  L. Weile,et al.  RESEARCH ON DEVELOPMENT AND DISTRIBUTION RULES OF GEOHAZARDS INDUCED BY WENCHUAN EARTHQUAKE ON 12TH MAY,2008 , 2008 .

[3]  Chen Wen-wu WAVE VELOCITY CHARACTERISTICS OF DYNAMO-RELAXED ROCK MASS AT SITE OF DALIUSHU DAM , 2006 .

[4]  Xu Jin-hua Analysis of supporting effect of systematic bolts applied to weak and broken phyllite tunnels in meizoseismal area , 2013 .

[5]  Li Tianbin,et al.  BASIC CHARACTERISTICS AND FORMATION MECHANISM OF THE LARGEST SCALE LANDSLIDE AT DAGUNGBAO OCCURRED DURING THE WENCHUAN EARTHQUAKE , 2008 .

[6]  Yin Yueping,et al.  RESEARCHES ON THE GEO-HAZARDS TRIGGERED BY WENCHUAN EARTHQUAKE,SICHUAN , 2008 .

[7]  Iunio Iervolino,et al.  Closed‐form aftershock reliability of damage‐cumulating elastic‐perfectly‐plastic systems , 2014 .

[8]  Li Tianbin,et al.  FAILURE CHARACTERISTICS AND INFLUENCE FACTOR ANALYSIS OF MOUNTAIN TUNNELS AT EPICENTER ZONES OF GREAT WENCHUAN EARTHQUAKE , 2008 .

[9]  Shen Yusheng Lessons Learnt from Damage of Highway Tunnels in Wenchuan Earthquake , 2009 .

[10]  Quanwang Li,et al.  Performance evaluation and damage assessment of steel frame buildings under main shock–aftershock earthquake sequences , 2007 .

[11]  Xiaoqing Chen,et al.  The Wenchuan Earthquake (May 12, 2008), Sichuan Province, China, and resulting geohazards , 2011 .

[12]  Tianbin Li,et al.  Damage to mountain tunnels related to the Wenchuan earthquake and some suggestions for aseismic tunnel construction , 2012, Bulletin of Engineering Geology and the Environment.

[13]  Sherong Zhang,et al.  Damage evaluation of concrete gravity dams under mainshock–aftershock seismic sequences , 2013 .

[14]  Ying Chun Li,et al.  Source mechanism of strong aftershocks (Ms⩾5.6) of the 2008/05/12 Wenchuan earthquake and the implication for seismotectonics , 2009 .

[15]  B. Gutenberg,et al.  Effects of ground on earthquake motion , 1957 .

[16]  Zhou Yi ANALYSIS OF FAILURE PROPERTIES AND FORMATTING MECHANISM OF SOFT ROCK TUNNEL IN MEIZOSEISMAL AREAS , 2012 .

[17]  Wang Bo EXPERIMENTAL STUDY OF COMPARISON AND OPTIMIZATION OF TUNNELING SCHEMES IN CRUSHING PHYLLITE , 2013 .

[18]  Tian-zhong Zhang,et al.  Relocation of the M8.0 Wenchuan earthquake and its aftershock sequence , 2008 .

[19]  Tian-zhong Zhang,et al.  Aftershock Distribution of the MS8.0 Wenchuan Earthquake and 3‐D P‐Wave Velocity Structure in and Around Source Region , 2009 .