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Effectiveness of inhibiting liquefaction triggering by shallow ground improvement methods: field shaking trials with T-Rex at one area in Christchurch, New Zealand

机译:浅层地面改善方法抑制液化触发的有效性:新西兰基督城一个地区与T-Rex的田间摇动试验

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Christchurch and the Canterbury region in New Zealand were devastated in 2010-2011 by a series of powerful earthquakes. The Christchurch area experienced widespread liquefaction that caused extensive damage. One critical problem facing the rebuilding effort is that the land remains at risk of liquefying in future earthquakes. Therefore, effective engineering solutions had to be developed to increase the resilience of homes and low-rise structures. To this end, a comprehensive series of full-scale field trials of multiple shallow ground improvement methods was performed. The field trials presented in this paper were conducted at one area in a severely damaged suburb of Christchurch and involved five test panels of different ground improvements. Each test panel and two additional test panels of unimproved natural soil were instrumented with embedded arrays of sensors and were characterized by crosshole seismic testing before shaking. A large mobile shaker, called T-Rex, was used to perform a staged-loading sequence of increasing sinusoidal horizontal loads at the surface of each test panel. The results of the staged-loading tests were successfully used to identify ground improvement methods that improved the ground performance versus those methods that contributed an insignificant improvement or even degraded the ground performance. The results of the pre-shaking crosshole tests were successfully used for two purposes. First, portions of the soils below the water table that were unsaturated were identified using compression wave velocities. Second, shear wave velocities were used: (1) to identify changes in the natural soil skeleton between improvements, and (2) to evaluate the effective shear stiffness of the combined improvement and surrounding natural soil. Further, the crosshole measurements led to development of a field verification method for use in evaluating changes created by shallow ground improvements.
机译:基督城和新西兰的坎特伯雷地区于2010 - 2011年被一系列强大的地震摧毁。基督城地区经历了广泛的液化造成了广泛的伤害。面临重建努力的一个关键问题是,该土地仍然有液化的危险。因此,必须开发有效的工程解决方案以增加房屋和低层结构的恢复力。为此,进行了一系列全面的多种浅层地面改进方法的全规模实地试验。本文提出的现场试验在基督城郊区严重受损的一个地区进行,并涉及五个不同地面改进的测试面板。每个测试板和两个额外的未化天然土壤测试面板用嵌入式传感器仪器仪表,其特征在于摇动前的横孔地震检测。用于T-REX的大型移动振动器用于在每个测试面板的表面上进行增加的正弦水平载荷的分阶段加载顺序。上演装载试验的结果成功用于识别地面改进方法,改善了地面性能与那些有助于改善或甚至降解地面性能的方法。预振荡斜孔试验的结果成功用于两个目的。首先,使用压缩波速度鉴定不饱和的水位下方的土壤部分。二,使用剪切波速度:(1)以识别改进之间的天然土壤骨架的变化,(2)评价组合改善和周围天然土壤的有效剪切刚度。此外,交叉孔测量导致开发用于评估浅层地改进产生的变化的现场验证方法。

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