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Field investigation and analysis of ground sinking development in a metropolitan city, Seoul, Korea

机译:韩国首尔大都市地面沉降发展的实地调查与分析

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摘要

Either geological features or some artificial factors, like sewer pipe leakage or incomplete construction work, cause ground sinking in urban areas. This study reports on a recent ground sinking, which occurred on account of complex factors related to geology and artificial excavation work. A cylindrical displacement of 14 m long in the ground, with a sinking of 3 m deep on the surface, was studied. This occurrence was situated adjacent to the excavation site, which was 38 m deep, during the construction of the high-rise building. Fine-grained soils were spilled out with groundwater, leaking through the bottom of the cutoff wall and before the ground sinking occurred completely. A scrutinized field survey was conducted through several means, such as observation through pit excavation, standard penetration test (SPT), and ground penetrating radar (GPR) exploration. Numerical groundwater flow analysis was also performed to evaluate the influence of the flow behavior from the surrounding area toward the excavated site using Visual MODFLOW. The study revealed that the geology of the site was comprised of multiple alluvial layers formed by many floods from the Han-river in Seoul, and it was very vulnerable to the piping near the excavation wall. The results of SPT displayed some void spaces of 20-30 cm thick under the sinking area, and the changes of soil properties are recognized before the excavation and after the ground sinking. The sequential displacement mechanism for ground sinking in this site is suggested from the analyses of the numerical groundwater flow model and the data obtained from field investigation.
机译:地质特征或某些人为因素(例如下水道泄漏或不完整的施工工作)都会导致市区下沉。这项研究报告了最近发生的地面下陷,这是由于与地质和人工开挖工作有关的复杂因素所致。研究了地下14 m长的圆柱位移,地表下沉3 m。在高层建筑的建造过程中,此事件位于发掘现场附近,发掘深度为38 m。细粒土壤被地下水溅出,从防渗墙的底部渗漏,并且在地面完全下沉之前就已经渗出。通过多种方法进行了详细的现场调查,例如通过基坑开挖观察,标准穿透试验(SPT)和探地雷达(GPR)勘探。还使用Visual MODFLOW进行了数值地下水流分析,以评估从周围区域到开挖点的流动行为的影响。研究表明,该地点的地质是由汉城汉江多次洪水形成的多个冲积层组成的,非常容易受到开挖墙附近管道的伤害。 SPT的结果显示,在下沉区域下有一些20-30 cm厚的空隙,在开挖前和下沉后都可以识别土壤性质的变化。通过数值地下水流模型的分析和现场调查获得的数据,提出了该场地下沉的顺序位移机制。

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