北京城市深基坑地表沉降特征

S. Li, Wei Lu
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引用次数: 0

摘要

作为一种了解相关变形的可行手段,以往的研究在世界范围内开展了深基坑的性能研究,自20世纪60年代以来,人们提出了不同地点之间地表沉降特征的情景。目的是研究北京地区开挖过程中的特征,填补该情景的空白。选取30个施工质量较好的开挖实例和现场观测数据,量化沉降与开挖的关系,分析地表变形行为。描述了最大地表沉降的震级和位置($\delta vm$)、明显影响范围、发展过程和模式。研究表明:(1)最终地表沉降呈凹槽型,有轻微的隆起,$\delta vm$位于距墙体约0.5H ~ 0.75H处。(2)地表沉降($\delta v$)的空间差异较大,各墙后出现较大的沉降,两侧中跨最大的沉降发生在1 ~ 2支杆移动最少的地方,尤其是长侧,移动$\Delta \delta v$为$2.8 \pm 0.75$ mm,而转角的移动最小。(3)最终沉降一般在5mm ~ -20mm范围内,小于$\delta vm$。影响区距离基坑外约2.5H ~ 3.1H。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Characteristics of ground surface settlement associated with deep excavation in Beijing city
As a viable means to understand the associated deformation, performance study of deep excavations has been conducted worldwide in previous studies, a scenario of ground surface settlement characteristics among different sites has been proposed since 1960s. The objective is to study the characteristics during excavation in Beijing and fill in the blank on the scenario. Thirty excavation cases with good-quality construction and field observation data are selected to quantify the relationship between settlement and excavation, and to analyze the ground surface deformation behavior. The magnitude and location of maximum ground surface settlement ($\delta vm$), the apparent influence range, development process and pattern are depicted. This study demonstrates that: (1) Concave trough pattern of final ground surface settlement is detected, slight heave was observed and $\delta vm$ located at distances about 0.5H to 0.75H from the wall. (2) Spatial difference of ground surface settlement ($\delta v$) varies greatly, great depression appeared behind each wall and maximum settlements at midspans of both sides occurs with the lowest 1-2 struts removal, especially the long side with a $\Delta \delta v$ of $2.8 \pm 0.75$ mm. Movement was least of all by the corners. (3) Final settlement generally ranges from 5mm to -20mm, less than $\delta vm$. Influence zones reach to a distance about 2.5H to 3.1H outside the excavation.
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