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首页> 外文期刊>Acta Geotechnica: An International journal for Geoengineering >Observations of the ground and structural behaviours induced by a deep excavation in loose sands
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Observations of the ground and structural behaviours induced by a deep excavation in loose sands

机译:松散沙滩深度挖掘诱导的地面和结构行为的观察

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摘要

Large-scale deep basement excavations are commonly used in metropolitan areas; however, previous studies focused primarily on excavations in impermeable clay instead of permeable sand with high groundwater levels. In this study, a unique opportunity provides a complete picture of the ground and structural behaviours induced by deep excavations in loose to medium sand, which have been rarely studied in the past. With a maximum excavation depth of 16.8 m, the pit was retained by a 0.9-m-thick and 32-m-deep reinforcement concrete diaphragm wall with 4-level struts. The maximum wall displacement (delta(vh)) reached 56 mm at the end of excavation, and the ratio of delta(vh) to the excavation depth was 0.32%. In contrast, the ratio of the maximum surface settlement to the excavation depth was lower, i.e. only 0.2%. Pumping inside the excavation site did not appear to induce a significant impact outside the excavation site due to the retaining wall embedded in a layer of impermeable clay at a depth of 28.5-30.5 m. The plain strain ratio from the observed settlement is interpreted; the ratio indicates a difference of 2-39%. This difference may be connected to the soil anisotropy, or the maximum surface settlement at each monitoring section may not be detected. The wide range of the variance might also be connected with the small measured surface settlements and the difficulty of detecting such small displacements on the ground level in field surveys.
机译:大型深层地下室挖掘通常用于大都市区;然而,之前的研究主要集中在不透水粘土中的挖掘上,而不是具有高地下水位的渗透砂。在这项研究中,一个独特的机会提供了通过对中间沙子的深度挖掘引起的地面和结构行为的完整画面,这已经很少在过去研究。最大挖掘深度为16.8米,坑由0.9米厚和32米深加固混凝土隔膜壁保持,具有4级支柱。在挖掘结束时最大壁位移(Delta(VH))达到56毫米,Δ(VH)与挖掘深度的比例为0.32%。相反,最大表面沉降与挖掘深度的比率较低,即仅0.2%。由于嵌入在不透水粘土层中的挡土墙下,挖掘部位内部的挖掘部位内未诱导挖掘部位外部的显着影响。观察到的结算的普通应变比被解释为;该比率表示2-39%的差异。该差异可以连接到土壤各向异性,或者可能无法检测到每个监测部分的最大表面沉降。宽范围的方差也可以与小测量表面沉降和难以检测在现场调查中的地面上的这种小位移的难度。

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