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首页> 外文期刊>Journal of JSCE >STUDIES ON SOIL LIQUEFACTION AND SETTLEMENT IN THE URAYASU DISTRICT USING EFFECTIVE STRESS ANALYSES FOR THE 2011 OFF THE PACIFIC COAST OF TOHOKU EARTHQUAKE
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STUDIES ON SOIL LIQUEFACTION AND SETTLEMENT IN THE URAYASU DISTRICT USING EFFECTIVE STRESS ANALYSES FOR THE 2011 OFF THE PACIFIC COAST OF TOHOKU EARTHQUAKE

机译:利用东北地区2011年太平洋沿岸有效应力分析对浦安地区土壤液化和沉降的研究

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The 2011 off the Pacific coast of Tohoku Earthquake caused soil liquefaction over a wide area. In particular, severe soil liquefaction was reported in the northern parts of the reclaimed lands around Tokyo Bay, even though the seismic intensity in this area was only about 5 on the JMA scale with low acceleration. The authors surveyed the residual settlement in the Urayasu district and then conducted effective stress analyses of sites affected and not affected by liquefaction. The analyses results were compared with the acceleration waves monitored with K-NET Urayasu or ground settlements surveyed. They were based on the acceleration observed on the seismic bedrocks in earthquake engineering in some other districts adjacent to Urayasu. Much of the settlement was due to the long duration of the earthquake, with further settlement resulting from the aftershocks. The study shows that the effects of aftershocks need to be monitored. The simplified liquefaction prediction methods using the factor of safety, F_(L), also need improvement.
机译:2011年东北地震太平洋沿岸地区造成了大范围的土壤液化。特别是,在东京湾附近的开垦土地的北部,据报道严重液化,尽管该地区的地震烈度在JMA规模上仅为5左右,且加速度较低。作者调查了浦安地区的残余沉降,然后对受液化影响和不受液化影响的地点进行了有效的应力分析。将分析结果与用K-NET Urayasu或调查的地面沉降监测的加速度波进行了比较。它们是基于邻近浦安其他地区地震工程中地震基岩上观测到的加速度得出的。大部分的沉降是由于地震的持续时间长,而余震导致了进一步的沉降。研究表明,余震的影响需要监测。使用安全系数F_(L)的简化液化预测方法也需要改进。

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