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A New Model of Pore Pressure Generation for Seabed Soils Under Typhoon Wave Loading

机译:台风作用下海床土壤孔隙压力生成的新模型

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With climate change in recent years caused the occurred frequencyrnincreasing of extremely waves. Due to sea level rise and the typhoonrndisasters, it could be caused the pore pressure of seabed may bernsustained a build-up state below the coastal structures, and occurringrnand increasing the risk of the seabed liquefaction.rnMost of the past related researches followed the earthquake relevantrntheory to evaluate the dynamic characteristic of cyclic wave loading,rnincluding wave induced the single external stress or internal stress,rnnumber of cycles in seabed, and pore pressure generation model forrnearthquake mechanism. Therefore, this study used experimentalrnmechanics and theoretical model to simulate liquefaction behaviorrnunder typhoon wave loading with case study of "Zone A" of KaohsiungrnHarbor Intercontinental Container Center at second stage project.rnFrom the related cyclic triaxial test results, this study proposed an porernpressure generation model for seabed under long-term wave loading byrnthe hyperbolic sine function, and suggest a testing parameter to predictrnthe curve of pore pressure under different test conditions as Tp=0.005,rn0.05 and 0.5. The model can be applied in assessment of typhoon waverninduced seabed liquefaction potential. The maximum possible liquefiedrndepth is about 6.6m when Tc =1200s in this study area, and provide thernwell marine geotechnical practical application for seabed stability.
机译:近年来随着气候变化而引起的极浪发生频率增加。由于海平面上升和台风灾害,可能导致海床的孔隙压力可能维持在沿海结构之下的堆积状态,并发生并增加了海床液化的风险.rn过去的大多数相关研究都遵循了地震相关理论为了评估循环波荷载的动力特性,包括波浪引起的单一外部应力或内部应力,海床的循环次数以及地震作用的孔隙压力产生模型。因此,本研究利用实验力学和理论模型来模拟台风波浪荷载作用下的液化行为,并以高雄港洲际集装箱中心二期工程“ A区”为例。rn从相关的循环三轴试验结果,本研究提出了一种孔隙压力产生模型。通过双曲正弦函数在长期波浪载荷作用下对海床进行了研究,并提出了一个测试参数来预测不同测试条件下的孔隙压力曲线,Tp = 0.005,r0.05和0.5。该模型可用于台风波诱发海床液化潜力的评估。当该区域Tc = 1200s时,最大可能液化深度约为6.6m,为海床稳定性的海洋地质工程实际应用提供了条件。

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