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隧道建设(中英文) ›› 2023, Vol. 43 ›› Issue (S2): 230-236.DOI: 10.3973/j.issn.2096-4498.2023.S2.026

• 研究与探索 • 上一篇    下一篇

富水区输水隧洞开挖过程中掌子面周边孔压演化规律及纵向范围取值对其影响研究

叶焰中1, 邹德兵2, 王汉辉2, 苏凯3,*   

  1. 1. 深圳市原水有限公司, 广东 深圳 518000 2. 长江勘测规划设计研究有限责任公司, 湖北 武汉 4300103. 武汉大学水资源工程与调度全国重点实验室, 湖北 武汉 430072
  • 出版日期:2023-12-30 发布日期:2024-03-28
  • 作者简介:叶焰中(1984—),男,安徽太湖人,2009年毕业于三峡大学,水工结构专业,硕士,高级工程师,从事水利工程项目管理工作。Email: 642393528@qq.com。*通信作者: 苏凯, Email: ksu@whu.edu.cn。

Evolution of Pore Pressure Around Tunnel Face and Influence of Longitudinal Value of ThreeDimensional Seepage Calculation on It During Construction of a Water Conveyance Tunnel With Rich Water

YE Yanzhong1, ZOU Debing2, WANG Hanhui2, SU Kai3, *   

  1. (1. Shenzhen Raw Water Co., Ltd., Shenzhen 518000, Guangdong, China; 2. Changjiang Survey, Planning, Design and Research Co., Ltd., Wuhan 430010, Hubei, China; 3. State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan 430072, Hubei, China)

  • Online:2023-12-30 Published:2024-03-28

摘要: 为探明深埋隧洞开挖过程中孔压演化规律、确定三维渗流计算模型的纵向范围取值,以监测断面为中心建立深埋长隧洞整体三维有限元模型。首先,采用隧洞一次性挖穿计算方案,研究施工开挖期孔压消散的时间历程; 然后,基于隧洞掌子面推进历程,分析隧洞开挖地下水位线的降低特征与掌子面推进过程中孔压的演化规律; 最后,以构建监测断面上完整的孔压演变曲线为目标,研究开挖推进过程中掌子面的前后扰动范围,并最终给出三维渗流计算模型纵向范围取值以及监测断面设置的建议。研究结果表明: 1)分步开挖法比一次挖穿法更能反映出掌子面推进过程中渗透孔压的时空演化规律。2)当掌子面推进距离为22.5DD为洞径)时,掌子面向前扰动范围基本稳定在80D;当掌子面越过监测断面推进到155D时,掌子面向后扰动范围基本稳定在72D。可以看出,构建数值分析模型时需要较大的纵向模型范围,需要将监测断面选择在掌子面的前后影响范围之外,即要求模型纵向范围不小于174.5D

关键词: 深埋长隧洞, 输水隧道开挖, 渗透孔压, 掌子面扰动范围, 模型纵向范围

Abstract: To explore the evolution patterns of pore pressure during the excavation of a deep tunnel and determine the longitudinal value of a threedimensional seepage calculation model, a threedimensional finite element model of a deepburied long tunnel is established with the monitoring section as the center. First, a scheme, in which the tunnel is excavated through one time, is adopted and the timehistory of pore pressure dissipation during excavation is studied. Then, the drawdown of the water table and the evolution of pore water pressure are investigated with excavation process. To construct an entire curve of pore water pressure evolution on the monitoring section, the influence scope of the tunnel face in the process of excavation is explored. Finally, the suggestions for the longitudinal value in threedimensional seepage numerical model and the setting of monitoring section are given. The results show the following: (1) The stepped excavation method can better reflect the mechanism of pore water pressure evolution than the onetime excavation method. (2) When the excavation distance is 22.5WT〗D, where refers to the tunnel diameter, the forward influence scope of the tunnel face gradually reaches WT80D. WT5TNR》〗(3) When the tunnel face goes across the monitoring section and the excavation distance reaches WT155D, WT5TNR》〗the backward influence scope of the tunnel face gradually reaches WT72D. Therefore, a large longitudinal model range is required, and the monitoring section should be outside the forward and backward influence scope of tunnel face, which should be more than WT174.5D.

Key words: deepburied long tunnel, excavation of water conveyance tunnel, seepage pore water pressure, influence scope of tunnel face, model longitudinal range