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Characterization of Shallow Soils in the Central Business District of Christchurch, New Zealand

机译:新西兰基督城中央商务区的浅层土壤特征

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The strong shaking experienced during multiple events of the 2010-2011 Canterbury earthquake sequence caused extensive liquefaction throughout the central business district (CBD) of Christchurch, New Zealand. The performance of structures during these events was often related to liquefaction of foundation soils. Careful sampling and triaxial testing (monotonic and cyclic) were performed on soils from key building sites in the CBD of Christchurch. High-quality test specimens could be obtained using the Dames & Moore (DM) hydraulic fixed-piston thin-walled tube sampler for most of the predominantly silty and sandy soils in the CBD. Test results indicate, though, that loose clean sand specimens were densified significantly during sampling, and, thus, the DM sampler should not be used in this type of soil deposit. Important insights regarding the cyclic response of these soils were developed through the laboratory testing. These results when combined with existing information [e.g., cone penetration test (CPT) profiles and building damage observations] provide the basis for performing dynamic analyses through the calibration of advanced soil constitutive models.
机译:在2010-2011年坎特伯雷地震序列的多个事件中经历的强烈震动导致新西兰基督城的中央商务区(CBD)发生广泛的液化。这些事件中结构的性能通常与地基土的液化有关。对基督城中央商务区主要建筑工地的土壤进行了仔细的采样和三轴测试(单调和循环测试)。可以使用Dames&Moore(DM)液压固定活塞薄壁管采样器获得高质量的试样,用于CBD中大部分主要为粉质和沙质土壤。但是,测试结果表明,在采样过程中,松散的干净的沙子样本已被显着地致密化,因此,DM采样器不应用于此类土壤沉积物。通过实验室测试得出了有关这些土壤循环响应的重要见解。这些结果与现有信息(例如,锥孔试验(CPT)剖面图和建筑物损坏观察)结合在一起,为通过高级土壤本构模型的校准进行动力分析提供了基础。

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