跨越V形峡谷的桥梁抗震分析:多水平成层非均匀介质V形场地多点地震动模拟
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  • 英文篇名:Analysis of Seismic Response for Bridges Located on a V-shaped Canyon:Simulation of Multi-support Seismic Motions in a V-shaped Canyon with Inhomogeneous Multi-layer Topography
  • 作者:柳国环 ; 冯啸
  • 英文作者:LIU Guo-huan;FENG Xiao;School of Civil Engineering,Tianjin University;
  • 关键词:桥梁工程 ; V形峡谷 ; 地震动模拟 ; 波函数 ; 多点地震动 ; 非均匀介质
  • 英文关键词:bridge engineering;;V-shaped canyon;;seismic motion simulation;;wave function;;multi-support seismic motion;;inhomogeneous medium
  • 中文刊名:ZGGL
  • 英文刊名:China Journal of Highway and Transport
  • 机构:天津大学建筑工程学院;
  • 出版日期:2017-12-15
  • 出版单位:中国公路学报
  • 年:2017
  • 期:v.30;No.172
  • 基金:国家自然科学基金项目(51408409,51778414);; 天津市应用基础与前沿技术研究计划(15JCQNJC07400);; 华南理工大学亚热带建筑科学国家重点实验室开放基金项目(2017ZB21)
  • 语种:中文;
  • 页:ZGGL201712017
  • 页数:9
  • CN:12
  • ISSN:61-1313/U
  • 分类号:154-162
摘要
为了解峡谷地形对地震波场分布的特殊影响,重点发展和实现了V形非均匀多层介质峡谷的多点地震动场模拟,其理论依据是在长期假设均匀介质峡谷场地的基础上引入分层效应模型,其优点在于考虑了地下层分布不均匀对地震动的影响。具体理论包括:稳态波场被分为封闭区和开放区,同时引入波函数展开法和大圆弧法,经推导得到了V形峡谷在SH波入射激励下稳态波场的分布频域解析解,进而得到分布于V形峡谷表面的频域谱;然后,简述导出的基于V形峡谷地形的"平-凹"相干函数模型;进而,利用两步骤传递函数法(水平自由表面→V形峡谷表面→峡谷地下)推导得到地下频域谱;由此,形成并阐明了非均匀多层介质V形峡谷表面和地下的多点地震动具体模拟方法;最后,开发了依据上述途径的V形场地多点地震动模拟程序并实现其可视化,验证了计算结果的合理性和可靠性。分析结果表明:波场幅值在峡谷两侧水平场地与峡谷底部具有明显差异,峡谷效应的多点相干性因各层分界面与峡谷边界稳态波场中的散射成分存在而被降低。
        In order to investigate the specific effect of canyon topography on the seismic wave field,a simulation approach of multi-support seismic motions was proposed and developed based on the theory of spatial variable seismic motions in a multi-layered V-shaped canyon with inhomogeneous media.The homogeneous-media canyon model was improved by introducing the layer model,and the effects of inhomogeneous media were taken into account.Firstly,the steady-state wave field was separated into two regions,namely,the open region and the enclosed region.The wave function expansion method and big-arc boundary method were adopted to obtain the analytical solution of seismic wave field in the V-shaped canyon by a train of plane SH waves.A flat-sunken coherence function model of a V-shape canyon was illuminated.Moreover,the underground power spectral density functions were deduced by a two-step transfer function method(horizontal free surface→V-shaped canyon surface→underground canyon).Then thesimulation approach of spatially variable seismic motions in a multi-layer V-shaped canyon was illuminated.Finally,a visual program of multi-support seismic motions in a V-shaped canyon was developed for the simulation,whilst the rationality of calculation results was verified.The results show that there are great differences of the wave displacement amplitudes between flat terrain and canyon bottom.Influenced by the scattering wave components in the steady-state wave field of the layer interface boundary and the canyon surface boundary,the coherence of canyon effect decreases correspondingly.
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