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Structural Movement and Damage to the Alaskan Way Viaduct Due to the Nisqually Earthquake

机译:大地震造成的结构运动和对阿拉斯加道路高架桥的破坏

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This paper addresses the effects of the February 28, 2001 Nisqually Earthquake on the Alaskan Way Viaduct located on the Seattle Waterfront, approximately 35 miles from the epicenter. Seismic ground motions at the Viaduct will be summarized from the seismic monitoring stations. Supplemental physical evidence from buildings and bridges in the vicinity provide a basis for characterizing the seismic ground motion. Preliminary findings indicate that the most significant ground movement was transverse to the bridge centerline, corresponding to seismic shear wave propagation from the epicenter, with a gravitational coefficient (g) of approximately 0.16. There is also some evidence of localized soil subsidence in the vicinity of the adjacent seawall attributable to the earthquake. Established elastic movement and permanent deformation of the Viaduct as a consequence of the seismic ground motions is discussed. Inspection findings document information establishing conclusions presented, with information gathered from historical bridge records. These inspection findings indicate that the bridge generally moved within elastic limits transverse to the roadway centerline, with some longitudinal movement in portions of the southern end. Inspection findings subsequent to the earthquake provide the basis for discussion of structural damage, and will include structural failure of the Pier 100 East column, and structural distress to Piers 94, 97, 121, 145, and 160 including adjacent crossbeams and longitudinal beams. Other bridge conditions not directly related to the earthquake will be addressed as they affect the seismically induced damage, including settlement of selected foundations A description of how the monitoring programs were developed and how they will be used in the future to determine structural movement is presented. Two methods for recording small structural movement have been implemented. One system is based on surveys with established control points and a second system utilizes "crack monitors" installed on the bridge over selected structurally significant cracks.
机译:本文探讨了2001年2月28日的尼斯奎利地震对位于西雅图水滨,距震中约35英里的阿拉斯加大道高架桥的影响。高架桥处的地震地面运动将通过地震监测站进行总结。附近建筑物和桥梁的补充物理证据为表征地震地震动提供了基础。初步发现表明,最显着的地面运动是横向于桥梁中心线,与地震震波从震中传播相对应,重力系数(g)约为0.16。还有一些证据表明,由于地震,相邻海堤附近存在局部土壤沉降。讨论了由于地震地面运动而导致的高架桥既定的弹性运动和永久变形。检查结果记录了建立结论的信息,以及从历史桥梁记录中收集的信息。这些检查结果表明,桥梁通常在横向于车道中心线的弹性限度内移动,并且在南端的部分区域内进行了一些纵向移动。地震后的检查结果为讨论结构破坏提供了基础,并将包括Pier 100 East柱的结构破坏以及94、97、121、145和160墩的结构遇险,包括相邻的横梁和纵梁。与地震没有直接关系的其他桥梁条件也将得到解决,因为它们会影响地震引起的破坏,包括选定地基的沉降。将介绍如何制定监控程序以及将来如何将其用于确定结构运动。已经实现了两种记录小结构运动的方法。一种系统是基于具有确定控制点的勘测,另一种系统是利用安装在桥梁上选定的具有重大结构裂缝的“裂缝监测器”。

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