土工基础 ›› 2021, Vol. 35 ›› Issue (3): 323-328.

• 工程实录 • 上一篇    下一篇

安石隧道突水涌泥原因分析与协同治理技术研究

陈德金   

  1. (临沧市高速公路开发投资有限责任公司,云南临沧 677000)
  • 收稿日期:2021-06-01 修回日期:2021-06-03 出版日期:2021-06-25 发布日期:2021-06-25
  • 作者简介:陈德金(1979-),男,工程师,研究方向为高速公路相关的工程建设及管理。

Analysis and Integrated Mitigation of Water and Mud Inrushing Hazard in Anshi Tunnel Excavation

CHEN Dejin   

  1. (Lincang Expressway Development Investment Co. Ltd., Lincang 677000)
  • Received:2021-06-01 Revised:2021-06-03 Online:2021-06-25 Published:2021-06-25

摘要: 云凤高速公路安石隧道施工中,右线隧道距离出口614 m处的掌子面(YK42+951.6)发生了两次大规模突水涌泥灾害。结合安石隧道工程地质和水文地质条件,对其突水涌泥原因及处治措施进行了深入研究。结果表明:安石隧道突涌水灾害具有突发性强、灾变演化速度快及影响范围大的特征。造成突水涌泥灾害事故发生的主要原因是右洞里程桩号K42+955处右上方存在一隐伏含水破碎带,现场并未准确勘探出。该破碎带呈不规则风化囊形态,距隧道拱项仅3 m左右。掌子面通过该风化囊时,隧道拱顶石英片岩处于相对完好状态,没有明显的涌水突泥前兆,但随着时间推移和隧道施工扰动产生的裂缝逐步贯通、渗流通道扩张,当隧道拱顶围岩强度达到极限临界状态时,突发第一次涌水突泥。第一次涌水突泥后,大量物源迅速淤积在局部堵塞点,涌水突泥暂时终止,随着补给水的不断涌入汇聚,其势能急剧增高,压力增大,造成第二次涌水突泥。综合考虑隧道施工环境后,制定了“排堵结合、分段治理、动态施工”的协同治理技术体系,并成功应用于安石隧道隐伏含水破碎带突涌水灾害的防治实践中,可供类似隧道工程参考和借鉴。


关键词: 隧道, 突水涌泥, 含水破碎带, 协同治理

Abstract: During the excavation of Anshi Tunnel of Yunfeng Expressway Project, two large-scale water and mud inrush incidents occurred at the excavated and supported face of the tunnel (Station YK42+951.6), which was 614 m away from the exit apron of the right tunnel. Combined with engineering geology and hydrogeology conditions in the Anshi tunnel, the factors that might induce the hazards and integrated mitigation measures of water and mud inrush incidents are studied in this paper. The results show that the water inrush hazards occurred suddenly and had a strongly destructive influence with a high evolution rate. The main reason for the water inrush and mud hazard was that there was a hidden saturated fracture zone at the upper right of the right tunnel mileage post K42+955, which had not been accurately characterized during the subsurface investigation stage. The fracture zone was in the shape of an irregular weathering lens, only about 3 meters away from the tunnel arch. When the tunnel excavation face passed through the weathering rock lens, although the quartz schist of the tunnel vault was in a relatively intact state, there was no obvious sign of water inrush and mud inrush. The cracks caused by the passage of time and the disturbance of the tunnel construction gradually penetrated and the seepage channel expanded. When the strength of the surrounding rock of the tunnel vault reached the critical limit state, the first burst of water and followed the mud inrush. After the first water and mud inrush, a large number of debris material quickly accumulated in the excavated area, and the water and mud inrush could be stopped temporarily. With the continuous inflow and convergence of the supply groundwater, the potential energy increased sharply, and the pressure increased, resulting in the second water and mud inrush. After an comprehensive considering the tunnel excavation environment, an integrated mitigation system was implemented, and it was successfully applied to the practice of minimizing and controlling water inrush hazards in the hidden saturated fracture zone of the Anshi Tunnel, which can be used as a reference for similar tunnel projects.

Key words: Tunnel Excavation, Water and Mud inrush, Saturated Fracture Zone, Integrated Mitigation

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