Deformation of the Zhangjiazhuang high-speed railway tunnel: an analysis of causal mechanisms using geomorphological surveys and D-InSAR monitoring
Deformation of the Zhangjiazhuang high-speed railway tunnel: an analysis of causal mechanisms using geomorphological surveys and D-InSAR monitoring作者机构:School of Earth SciencesLanzhou UniversityLanzhou 730000China College of Earth and Environmental SciencesMOE Key Laboratory of Western China's Environmental SystemsLanzhou UniversityLanzhou 730000China Gansu Tech Innovation Centre for Environmental Geology and Geohazard PreventionLanzhou 730000China School of ArchitectureBuilding and Civil EngineeringLoughborough UniversityLoughboroughLE113TUUK Key Laboratory of Qinghai Environmental Geological SurveyXining 810007China Xi’an Centre of China Geological SurveyXi’an 710054China
出 版 物:《Journal of Mountain Science》 (山地科学学报(英文))
年 卷 期:2021年第18卷第7期
页 面:1920-1936页
核心收录:
学科分类:081406[工学-桥梁与隧道工程] 0709[理学-地质学] 0819[工学-矿业工程] 08[工学] 0303[法学-社会学] 0818[工学-地质资源与地质工程] 0708[理学-地球物理学] 0705[理学-地理学] 0815[工学-水利工程] 0816[工学-测绘科学与技术] 0706[理学-大气科学] 0813[工学-建筑学] 0704[理学-天文学] 0814[工学-土木工程] 0833[工学-城乡规划学] 0713[理学-生态学] 0834[工学-风景园林学(可授工学、农学学位)] 082301[工学-道路与铁道工程] 0823[工学-交通运输工程]
基 金:funded by the National Key Research and Development Program of China (Grant No.2018YFC1504704) the National Natural Science Foundation of China (Grant No.41661144046) the Fundamental Research Funds for the Central Universities (Grant No.lzujbky-2018-k14) the Key Research and Development Program of Gansu Province (Grant No.18YF1WA114)
主 题:Gaojiawan Landslide group Zhangjiazhuang tunnel Deformation Fault activity Irrigation infiltration
摘 要:On 18 January 2016,the Zhangjiazhuang high-speed railway tunnel in Ledu,Qinghai Province,China,underwent serious deformation and structural damage.A crack formed at the top of the tunnel and the concrete on the crown peeled *** a result,the tunnel could not be operated for three *** order to determine the types and spatial distribution of the landslides in the region and the surface deformation characteristics associated with the tunnel deformation,we used field geological and geomorphological surveys,unmanned aerial vehicle image interpretation and differential interferometric synthetic aperture radar(D-In SAR) surface deformation *** ancient and old landslides were identified and analysed in the study *** deformation monitoring and investigation of buildings in several villages on the slope front showed that the tunnel deformation was not related to deep-seated gravitational slope ***,surface deformation monitoring revealed an active NEE–SWW fault in the area intersecting the tunnel at the location of the tunnel *** constitutes a plausible mechanism for the deformation of the *** study highlights the need for detailed engineering geomorphological investigations to better predict the occurrence of tunnel deformation events in the future.