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    Excavation-Induced Groundwater Evolution of Noncircular Tunnels in Mountainous Regions: Analytical and Numerical Investigation

    Source: International Journal of Geomechanics:;2023:;Volume ( 023 ):;issue: 012::page 04023231-1
    Author:
    Yao Lu
    ,
    Ming Huang
    ,
    Qiwu Jiang
    ,
    Zhijie Chen
    ,
    Chaoshui Xu
    ,
    Yu Wang
    DOI: 10.1061/IJGNAI.GMENG-8667
    Publisher: ASCE
    Abstract: Excavation damage induced by the drill-and-blast method (DBM) of the surrounding rock zone in tunneling intensifies the loss of groundwater and causes serious hydroecological imbalance. Traditional theoretical analysis concerning tunnel seepage fields leads to an underestimation of groundwater inflow due to the ignoring of the factor of increased permeability in the DBM damage zone. Meanwhile, the composite liner widely used in DBM tunnels with the waterproofing and drainage system is difficult to simulate numerically. Taking into account the damaged zone, this work presents an analytical solution based on the axisymmetric modeling method suitable for deep tunnels to determine the groundwater inflow, permeability coefficient, and seepage force. The proposed solution combining the equivalent perimeter method is extended to noncircular tunnels. Comparisons of the numerical results with those of a previous study indicate that the proposed approach provides realistic predictions for the groundwater inflow and external water pressure. Introducing the concept of an equivalent liner, a series of numerical simulations for the center-diaphragm (CD) method are performed, in which 14 steps are divided for the tunnel construction and operation. The results indicate that the external water pressures significantly decrease after an upper-section excavation of the left drift and increase after support closure. The seepage velocity of the primary support and second liner reaches the maximum near the arch skewback. The maximum seepage volume Q occurs after a left-drift upper-section excavation and the maximum groundwater table drawdown h occurs before right-drift support closure. The impact of rainfall on h is far greater than that on Q. For damaged and grouting zones, the effects of permeability on Q and h are more significant than those of thickness. Furthermore, a significant advantage of the CD method compared with the full-face and bench methods is deduced for tunnels crossing unfavorable strata.
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      Excavation-Induced Groundwater Evolution of Noncircular Tunnels in Mountainous Regions: Analytical and Numerical Investigation

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4296245
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    • International Journal of Geomechanics

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    contributor authorYao Lu
    contributor authorMing Huang
    contributor authorQiwu Jiang
    contributor authorZhijie Chen
    contributor authorChaoshui Xu
    contributor authorYu Wang
    date accessioned2024-04-27T20:55:14Z
    date available2024-04-27T20:55:14Z
    date issued2023/12/01
    identifier other10.1061-IJGNAI.GMENG-8667.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4296245
    description abstractExcavation damage induced by the drill-and-blast method (DBM) of the surrounding rock zone in tunneling intensifies the loss of groundwater and causes serious hydroecological imbalance. Traditional theoretical analysis concerning tunnel seepage fields leads to an underestimation of groundwater inflow due to the ignoring of the factor of increased permeability in the DBM damage zone. Meanwhile, the composite liner widely used in DBM tunnels with the waterproofing and drainage system is difficult to simulate numerically. Taking into account the damaged zone, this work presents an analytical solution based on the axisymmetric modeling method suitable for deep tunnels to determine the groundwater inflow, permeability coefficient, and seepage force. The proposed solution combining the equivalent perimeter method is extended to noncircular tunnels. Comparisons of the numerical results with those of a previous study indicate that the proposed approach provides realistic predictions for the groundwater inflow and external water pressure. Introducing the concept of an equivalent liner, a series of numerical simulations for the center-diaphragm (CD) method are performed, in which 14 steps are divided for the tunnel construction and operation. The results indicate that the external water pressures significantly decrease after an upper-section excavation of the left drift and increase after support closure. The seepage velocity of the primary support and second liner reaches the maximum near the arch skewback. The maximum seepage volume Q occurs after a left-drift upper-section excavation and the maximum groundwater table drawdown h occurs before right-drift support closure. The impact of rainfall on h is far greater than that on Q. For damaged and grouting zones, the effects of permeability on Q and h are more significant than those of thickness. Furthermore, a significant advantage of the CD method compared with the full-face and bench methods is deduced for tunnels crossing unfavorable strata.
    publisherASCE
    titleExcavation-Induced Groundwater Evolution of Noncircular Tunnels in Mountainous Regions: Analytical and Numerical Investigation
    typeJournal Article
    journal volume23
    journal issue12
    journal titleInternational Journal of Geomechanics
    identifier doi10.1061/IJGNAI.GMENG-8667
    journal fristpage04023231-1
    journal lastpage04023231-12
    page12
    treeInternational Journal of Geomechanics:;2023:;Volume ( 023 ):;issue: 012
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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