深厚富水砂土地铁深基坑变形性状及频发地连墙渗漏灾害分析

    Analyses of deformation behaviors of subway excavations and frequent through-wall leaking hazards in water-rich sandy strata

    • 摘要: 为探究深厚富水砂土地铁深基坑变形性状以及频发地连墙渗漏灾害特征,首先,建立了深基坑变形和渗漏事例数据库以开展全面统计分析,得到了围护结构和坑外地表变形规律并识别出关键影响因素。其次,提出了富水砂土深基坑挡墙渗漏灾害的新型分类方法,进而揭示了灾害主要诱因并总结了有效应对措施。统计分析表明:①墙体最大侧移 \delta _\texthm 范围为(0.03%~0.48%)HH为开挖深度), \delta _\texthm 大小受到角部效应、降水模式、墙趾埋置条件以及墙体暴露长度等因素影响;②地表沉降剖面为典型凹槽形,最大沉降 \delta _\textvm 为0.26% H_\texte ( H_\texte 为最终开挖深度)并距墙体约0.5 H_\texte ;③地连墙渗漏会导致 \delta _\texthm 突增,这主要归因于动水力引起的墙背水土合力增加以及注浆压力不当;④渗漏引起的大部分地表沉降增量 \Delta \delta _\textv1 均小于0.5% H_1 且主要影响区可扩展至坑外约2 H_1 范围,其中 H_1 为墙体渗漏深度,坑外地层扰动区呈“倒圆锥形”分布;⑤挡墙渗漏灾害可划分为3种类型:轻微渗水无土体流失、严重渗漏水轻微土体流失以及大量漏水漏砂;⑥采用“灾前预防和灾后应急处置”思路能有效控制地连墙渗漏灾害。

       

      Abstract: To explore the deformation behaviors of subway excavations in thick water-rich sandy strata and the characteristics of frequent through-wall leaking hazards, the databases of excavation deformation and through-wall leaking events are first built to carry out comprehensive statistical analyses; hence, the deformation laws of retaining walls and ground surface behind the walls are obtained, and the key influencing factors are identified. Then, a novel method for classifying through-wall leakages during deep excavation in water-rich sand is proposed; afterwards, their primary triggering factors are revealed, and the effective measures are also summarized. The statistical analyses show that: (1) The maximum lateral wall deflection, \delta _\texthm , varies from 0.03% H (H, excavation depth) to 0.48% H; the magnitudes of \delta _\texthm are affected by the spatial-corner effect, dewatering mode, burial condition of wall toes, and wall exposure length. (2) The profile of ground settlements is a typical concave shape, and the maximum settlement, \delta _\textvm , is 0.26% H_\texte ( H_\texte , final excavation depth), which occurs at about 0.5 H_\texte behind the walls. (3) Through-wall leaking causes sudden increments of \delta _\texthm , mainly attributed to the rapid increment of total lateral earth pressure induced by seepage force and/or the inappropriate grouting pressure. (4) Most of the leakage-induced settlement increments, \Delta \delta _\textv1 , are less than 0.5% H_1 , and the primary influence zone could be extended to about 2 H_1 outside the pit, in which H_1 denoted the burial depth of leaky spots on the wall; besides, the shape of strata disturbed behind the walls shows a distribution of "inverted cone". (5) Leaking hazards can be classified into three levels: minor seepage without soil loss, massive leakage with slight soil loss, and massive inrush of water and soils. (6) Through-wall leakages can be effectively controlled from the perspective of "disaster prevention before accidents and emergency response after accidents".

       

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