A semi-analytical solution for seepage field and soil deformation induced by coupled pre-excavation dewatering and groundwater recharge with a suspended waterproof curtain considering delayed phreatic surface response

IF 4.2 2区 环境科学与生态学 Q1 WATER RESOURCES
Weitao Yang , Liang Xiao , Guoxiong Mei
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Abstract

Accurate prediction and effective control of soil deformation induced by pre-excavation dewatering are essential for construction safety in underground space development. However, the coupled effects of suspended waterproof curtains and external groundwater recharge on drawdown and soil deformation in unconfined aquifers remain unclear, particularly considering the delayed response of the phreatic surface. This study develops an improved theoretical model to characterize soil deformation induced by pre-excavation dewatering and external recharge under plane strain conditions, explicitly considering a suspended waterproof curtain and the time-dependent behavior of the water table. A semi-analytical solution is then derived using integral transform techniques and verified through laboratory model tests, degradation solutions, and numerical simulations. Parametric analyses indicate that prolonging time required for the groundwater level within the pit to reach the target value can substantially decrease soil settlement before excavation, which has minimal effect on the final steady-state settlement. Increasing the horizontal distance between recharge wells and the foundation pit mitigates far-field drawdown but may increase soil settlement within the pit, whereas longer well screens enhance phreatic surface recovery near the excavation. Furthermore, increasing the penetration depth of the waterproof curtain and appropriately scheduling the initiation of recharge wells can effectively limit external groundwater inflow, thereby reducing groundwater drawdown and soil settlement outside the foundation pit. Specifically, increasing the penetration depth of the waterproof curtain from 6 m to 12 m reduces internal settlement by 6.7% and external settlement by 77.9%, suggesting a stronger mitigation effect on the external side. These findings not only extend existing theoretical models by explicitly incorporating the coupled effects of suspended waterproof curtains and external recharge wells with delayed phreatic surface response, but also support and broaden prior findings by demonstrating how recharge design parameters and initiation timing critically govern drawdown and soil deformation in deep excavations.
考虑延迟表层响应的开挖前降水与悬挂式防水帷幕耦合回灌渗流场及土体变形半解析解
准确预测和有效控制基坑降水引起的土体变形对地下空间开发施工安全至关重要。然而,悬式防水帷幕和外部地下水补给对无承压含水层下陷和土壤变形的耦合效应尚不清楚,特别是考虑到潜水面的延迟响应。本研究建立了一个改进的理论模型来描述平面应变条件下开挖前降水和外部补给引起的土壤变形,明确考虑了悬挂防水帷幕和地下水位的时间依赖性行为。然后使用积分变换技术推导出半解析解,并通过实验室模型试验、退化解和数值模拟进行验证。参数分析表明,延长基坑内地下水位达到目标值所需的时间可以显著降低基坑开挖前土体沉降,对最终稳态沉降影响最小。增加补给井与基坑之间的水平距离可以减轻远场下沉,但可能会增加基坑内的土壤沉降,而较长的井筛可以提高基坑附近的表层恢复。增加防水帷幕的侵深,适当安排回灌井的起爆,可以有效地限制外部地下水的流入,从而减少地下水的下降和基坑外土体的沉降。其中,将防水帷幕的穿透深度从6 m增加到12 m,可使内部沉降减少6.7%,外部沉降减少77.9%,表明对外部的减缓效果更强。这些发现不仅扩展了现有的理论模型,明确地考虑了悬式防水帷幕和外部补给井的耦合效应与延迟的表层响应,而且支持和拓宽了先前的发现,证明了补给设计参数和启动时间如何关键地控制深基坑的下陷和土壤变形。
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来源期刊
Advances in Water Resources
Advances in Water Resources 环境科学-水资源
CiteScore
9.40
自引率
6.40%
发文量
171
审稿时长
36 days
期刊介绍: Advances in Water Resources provides a forum for the presentation of fundamental scientific advances in the understanding of water resources systems. The scope of Advances in Water Resources includes any combination of theoretical, computational, and experimental approaches used to advance fundamental understanding of surface or subsurface water resources systems or the interaction of these systems with the atmosphere, geosphere, biosphere, and human societies. Manuscripts involving case studies that do not attempt to reach broader conclusions, research on engineering design, applied hydraulics, or water quality and treatment, as well as applications of existing knowledge that do not advance fundamental understanding of hydrological processes, are not appropriate for Advances in Water Resources. Examples of appropriate topical areas that will be considered include the following: • Surface and subsurface hydrology • Hydrometeorology • Environmental fluid dynamics • Ecohydrology and ecohydrodynamics • Multiphase transport phenomena in porous media • Fluid flow and species transport and reaction processes
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