摘要
南大梁高速公路铜锣山隧道处于岩溶地区,而一般山区岩溶工程地质条件较复杂,勘察难度大。通过加大对隧道岩溶区的调查研究,采用区域地质环境条件分析、岩溶特征分析、岩溶水文地质条件的综合分析法,全面阐述了隧址区的岩溶发育特征和地下水文分布规律。
Tongluoshan Tunnel of Nanchong—Dazhu—Liangping Highway locates in karst area,while the engineering geological conditions are complicated in mountainous karst areas generally and the investigation is difficult. With intensified investigation on the karst area of Tunnel,the comprehensive analysis method,including the analysis of regional geological environment,karst characteristics and karst hydrogeological conditions,was used to explain the karst development characteristics and groundwater hydrological distribution law in the tunnel zone.
引文
[1] 四川省地质局.1/20万地质图及报告(达州幅)[R].成都:四川省地质局,1980.Sichuan Provincial Bureau of Geology.1/200000 Regional Geologic Map of Dazhou City[R].Chengdu:Sichuan Provincial Bureau of Gevlogy,1980.
[2] JTG C20—2011 公路工程地质勘察规范[S].北京:人民交通出版社,2011.JTG C20—2011 Code for Highway Engineering Geological Investigation[S].Beijing:China Communications Press,2011.
[3] 郭佳奇,王光勇,任连伟.宜万铁路岩溶地质特征及其发育模式[J].中国地质灾害与防治学报,2013,24(2):72-78.GUO J Q,WANG G Y,REN L W.Karst geological features of Yiwan Line and their basic modes[J].The Chinese Journal of Geological Hazard and Control,2013,24(2):72-78.
[4] 铁道部第一勘测设计院.铁路工程地质手册[K].2版.北京:中国铁道出版社,1999.China Railway First Survey and Design Institute Group Co.,Ltd.Railway Engineering Geology Manual[K].2nd ed.Beijing:China Railway Publishing House,1999.
[5] 李苍松,王石春,陈成宗.岩溶地区铁路工程地质研究[J].铁道工程学报,2005(增刊1):357-363.LI C S,WANG S C,CHEN C Z.Research on the railway engineering geology in karst area[J].Journal of Railway Engineering Society,2005(S1):357-363.