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湘桂铁路二塘车站路基岩溶塌陷成因与防治对策

刘昭京 蒋小珍 冯涛 黄胜平 周富彪 伊小娟

刘昭京,蒋小珍,冯 涛,等. 湘桂铁路二塘车站路基岩溶塌陷成因与防治对策[J]. 中国岩溶,2023,42(1):109-118 doi: 10.11932/karst20230109
引用本文: 刘昭京,蒋小珍,冯 涛,等. 湘桂铁路二塘车站路基岩溶塌陷成因与防治对策[J]. 中国岩溶,2023,42(1):109-118 doi: 10.11932/karst20230109
LIU Zhaojing, JIANG Xiaozhen, FENG Tao, HUANG Shengping, ZHOU Fubiao, YI Xiaojuan. Formation mechanism and prevention countermeasures for karst collapse in Ertang railway station, Guilin[J]. CARSOLOGICA SINICA, 2023, 42(1): 109-118. doi: 10.11932/karst20230109
Citation: LIU Zhaojing, JIANG Xiaozhen, FENG Tao, HUANG Shengping, ZHOU Fubiao, YI Xiaojuan. Formation mechanism and prevention countermeasures for karst collapse in Ertang railway station, Guilin[J]. CARSOLOGICA SINICA, 2023, 42(1): 109-118. doi: 10.11932/karst20230109

湘桂铁路二塘车站路基岩溶塌陷成因与防治对策

doi: 10.11932/karst20230109
基金项目: 中国铁路南宁局集团有限公司科研计划项目(建18-5);国家自然科学基金(42077273);中国地质调查局项目(DD20190266);岩溶所基本科研业务费项目(2021003)
详细信息
    作者简介:

    刘昭京(1966-),男,正高级工程师,工程建设专业带头人

    通讯作者:

    蒋小珍(1970-),女,博士,研究员,博导,主要从事岩溶地质灾害防治研究。E-mail:511036641@qq.com

  • 中图分类号: P642.25

Formation mechanism and prevention countermeasures for karst collapse in Ertang railway station, Guilin

  • 摘要: 湘桂铁路二塘车站高铁区段1996-2016年间发生岩溶塌陷险情27起,虽经过多期悬挂式帷幕注浆整治,但塌陷问题仍是行车安全的极大隐患。通过资料收集、场地野外调查、岩溶地下水气压力长期监测站的监测资料分析,细化了研究区的地质构造、岩溶水文地质条件及岩溶发育特征,从地质结构、岩溶地下水动力特征等方面分析,认为岩溶塌陷形成的成因为临桂地区房地产基坑开挖抽排水影响岩溶地下水水位变化,造成基岩面上覆土体的潜蚀,形成土洞,进而发展至地面形成塌陷坑。针对铁路运行段地下水位埋深具承压性,隐伏溶洞充填率高的复杂岩溶地质条件以及注浆压力的限制,提出加强基岩面上覆土层抗渗强度、管控岩溶地下水降深的岩溶塌陷防治对策。

     

  • 图  1  场地基岩地质与构造图

    Figure  1.  Geological structure of bedrock of the site

    图  2  水文地质图

    Figure  2.  Hydrogeological map of the site

    图  3  场地内人可进入的溶洞分布图

    Figure  3.  Distribution map of accessible caves

    图  4  溶洞照片

    Figure  4.  Cave photo

    图  5  区内岩溶塌陷分布图

    Figure  5.  Distribution map of karst sinkhole pits

    图  6  铁路线内塌陷坑照片

    Figure  6.  Photos of karst collapse pits

    图  7  注浆钻孔土层厚度统计图

    Figure  7.  Statistics of Quaternary thickness of grouting drilling

    图  8  铁路沿线地下水降落漏斗分布图

    Figure  8.  Contour map of karst groundwater along the railway

    图  9  滑石厂、饲料厂监测点岩溶水位动态(2019.7-2021.2)

    Figure  9.  Relationship between groundwater-air pressure and rainfall (from July, 2019 to February, 2021)

    表  1  调查区地下岩溶发育特征表

    Table  1.   Development characteristics of underground karst in the survey area

    区段统计孔数/个遇洞孔数/个钻孔遇洞率/%有水孔数/个平均有水钻孔
    出水量/L·s−1
    充填、半充填溶洞
    充填率/%
    空洞率/%
    临桂城区25187218117026.3
    下载: 导出CSV

    表  2  岩溶发育深度特征统计表

    Table  2.   Statistics of karst development depth

    钻孔编号钻孔深度/m孔口标高/m初见水位/m稳定水位/m土层厚度/m裂隙发育段/m
    zk2-180160.931.161.983.74.8~9.9,68.9~71
    zk6-180171.991.81.631.940~54.3,63.2~69.8
    zk7-180158.211.13.661.21.2~38.4
    zk7-232.3161.622.92.94.54.5~14,28.3~30.1
    zk9-180159.912.762.82.513.7~18.4,34.6~37.2,41.9~46.6
    zkD-180157.11.81.673.811.5~13.8,19.7~28,50.2~57.2,77.3~80
    zk9-280158.222.332.336.422.6~24.9
    zk10-180158.110.70.72.327.3~32
    zk11-180158.981.11.13.87.4~12.7,17.9~31.4,39.3~41.3,48.5~70.6
    zk12-330160.130.60.64.615.7~17.3
    zk12-480151.591.911.953.220.2~22.6,24.9~29.6,32~43.7,48.3~50.7
    zk13-380155.563.033.034.417.2~23.4,25.5~30.2,32.8~39.6,47.5~63.4,75.8~77.5
    zk14-280151.130.70.722~28.1,40.1~63.6,68.3~70.9
    zk15-130163.523.53.577~8.5,10.9~24.9
    zk15-480157.857.056.98.450~80
    下载: 导出CSV
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  • 收稿日期:  2022-01-20
  • 刊出日期:  2023-02-25

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