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Surface settlements at a soft soil site due to bedrock dewatering

机译:基岩脱水导致软土场地表层沉降

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Construction of a 16-m deep, 55-m wide, almost square, underground structure through 8-m of soft soils and 8-m of sandstone and siltstone led to the development of widespread settlements. The affected area extended to distances of over 200 m from the perimeter of the structure. The floor slab of the underground structure was not designed for water pressure. Thus, operation of the structure requires continuous pumping of seepage water collected at a sump located at the lowermost elevation within the structure. Subsurface investigation and monitoring data obtained over 5.75-year period following the construction of the structure indicated that the settlement resulted from consolidation of soft soils due to depressurization of an aquifer within the underlying bedrock caused by continuous dewatering needed for the operation of the structure. An analytical study was undertaken to project the long term settlement. A simple analytical model could be used to simulate the complex hydrogeological problem reasonably. The details of hydrogeologic setting, subsurface investigation and monitoring activities, and the analytical model for projecting long-term settlements are presented in this paper.
机译:通过8 m的软土以及8 m的砂岩和粉砂岩建造16 m深,55 m宽,几乎为正方形的地下结构,导致了广泛定居点的发展。受影响的区域延伸到距结构外围200 m以上的距离。地下结构的楼板不是为承受水压而设计的。因此,结构的操作需要连续泵送收集在位于结构内最低高度的集水槽处的渗漏水。在结构建造之后的5.75年中获得的地下调查和监测数据表明,沉降是由于软土的固结所致,这是由于结构运行所需的连续脱水导致下伏基岩层中的含水层减压所致。进行了一项分析研究以预测长期解决方案。一个简单的分析模型可以用来合理地模拟复杂的水文地质问题。本文介绍了水文地质环境,地下调查和监测活动的详细信息,以及预测长期沉降的分析模型。

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