2017
DOI: 10.1002/nag.2760
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Analytical approach for time‐dependent groundwater inflow into shield tunnel face in confined aquifer

Abstract: Summary Prediction of time‐dependent groundwater inflow into a shield tunnel is a significant task facing engineers. Published literature shows that there is no available method with which to predict time‐dependent groundwater inflow into a tunnel. This paper presents a prediction approach for time‐dependent groundwater inflow into a tunnel in both anisotropic and isotropic confined aquifers. The proposed solution can predict groundwater inrush from the tunnel cutting face. To obtain the time‐dependent groundw… Show more

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Cited by 99 publications
(41 citation statements)
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“…However, the groundwater inflow estimated by these classic equations is either the maximum value or the stable value, which cannot describe the time dependency of the groundwater inflow. Very recently, Liu et al have proposed a time‐dependent groundwater inflow formula at tunnel excavation face, which can be presented as follows: Q()t=16.11kxkyλSλ()tkz[]2MtkzSs+πlnkztSsM2, where k x , k y , and k z are hydraulic conductivities in three principle directions (m/d), M is aquifer thickness (m), t is time (d), S λ ( t ) is drawdown at a distance of λ (m), S s is specific storage (m −1 ), and λ is distance from a point source along y ‐axis (m).…”
Section: Formulationmentioning
confidence: 99%
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“…However, the groundwater inflow estimated by these classic equations is either the maximum value or the stable value, which cannot describe the time dependency of the groundwater inflow. Very recently, Liu et al have proposed a time‐dependent groundwater inflow formula at tunnel excavation face, which can be presented as follows: Q()t=16.11kxkyλSλ()tkz[]2MtkzSs+πlnkztSsM2, where k x , k y , and k z are hydraulic conductivities in three principle directions (m/d), M is aquifer thickness (m), t is time (d), S λ ( t ) is drawdown at a distance of λ (m), S s is specific storage (m −1 ), and λ is distance from a point source along y ‐axis (m).…”
Section: Formulationmentioning
confidence: 99%
“…7, Guangzhou city (China). Figure presents the longitudinal geotechnical profiles of investigated tunnel section . The mylonite fault is a dynamo‐metamorphic product of weathered siltstone and migmatite granite.…”
Section: Analytical Solutions Of a Groundwater Inflow Casementioning
confidence: 99%
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