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国外对隔震结构竖向地震反应的观测结果和对隔震结构竖向地震作用计算的规定,都与我国抗震规范有较大差别。本文通过反应谱和时程分析,讨论了多层隔震结构的竖向地震作用取值及竖向地震作用效应,对我国抗震规范的有关规定作了探讨,认为除位于近断层附近的隔震建筑外,其它隔震结构的竖向地震作用可取与不隔震结构相同;对于多层隔震建筑,多遇地震下可不考虑竖向地震作用,在罕遇地震下,应对所有隔震结构验算支座是否受拉或失稳,并且组合时应计入竖向地震作用效应。 相似文献
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《地震工程与工程振动》2021,41(4)
以典型的四层、六层和八层LRB(铅芯橡胶隔震支座)基础隔震结构为研究对象,通过大量的弹塑性时程分析,对极罕遇地震作用下的地震响应特点进行了分析;采用参数化方法,研究了隔震系统的力学性能参数和上部结构屈服强度比的变化对LRB基础隔震结构抗震性能的影响。结果表明:在极罕遇地震作用下,LRB基础隔震结构上部结构首层的层间位移角和延性系数明显增大;延长LRB隔震系统的隔震周期或选择最优的特征屈服强度比,均可显著降低上部结构的塑性变形程度,但LRB屈服位移的变化对隔震结构的响应几乎无影响;LRB隔震系统参数确定后,隔震结构上部结构的损伤状态主要与上部结构力学性能参数中的屈服强度比相关,增大上部结构的屈服强度比,可以显著降低上部结构的层间位移角和延性系数,但是隔震支座的平均最大剪应变会增大,可以选用橡胶剪切模量大或者直径大、第二形状系数小的LRB隔震支座。 相似文献
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组合基础隔震结构双向地震反应分析 总被引:2,自引:0,他引:2
本文采用双向耦合恢复力模型模拟组合隔震系统中隔震支座的双向耦合效应,对组合基础隔震结构进行了单向和双向地震反应对比分析,分析表明在水平双向地震作用下结构各层的加速度反应较小,隔震层的层间位移较大,而上部结构的层间位移较小,并且在水平双向地震作用下,支座的最大位移明显大于单向地震作用时支座的最大位移,因而应考虑水平双向地震作用对组合基础隔震结构地震反应和隔震支座性能的影响。 相似文献
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为研究罕遇地震下复合隔震村镇建筑的地震响应特征及设计参数,采用ABAQUS有限元软件建立了复合隔震结构、滑移隔震结构、砂垫层隔震结构以及传统的砌体结构四种模型,通过对比4种模型在不同滑移层摩擦系数及不同地震烈度下的加速度、位移及底部剪力等动力响应差异,得出复合隔震体系的地震响应特征及主要设计参数。结果表明:复合隔震体系具有最优的隔震效果,且滑移层摩擦系数越小,地震烈度越大,隔震效果越好。根据预设40%隔震率的要求,确定出不同抗震设防烈度区的滑移层摩擦系数取值范围。 相似文献
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《华南地震》2018,(4)
基础隔震结构在罕遇地震作用下可以大幅降低上部结构的地震响应,达到保护结构的目的;但在超过罕遇地震的强震作用下,隔震层位移可能超过预留的隔震沟宽度,隔震结构与周边挡土墙碰撞。建立考虑上部结构非线性的隔震结构模型,设防烈度为8度,进行了超过罕遇地震的强震下地震响应分析,结果表明,隔震结构与挡土墙碰撞减小了隔震层位移,但导致上部结构加速度、位移及层剪力明显放大,放大程度随碰撞刚度及地震动强度的增大而增大,随隔震沟宽度的增大而减小;碰撞刚度增大到一定程度后,层间位移的增大对碰撞刚度的增大不再敏感,加速度及上部结构基底剪力系数则未表现出这一趋势;碰撞还导致支座最大面压的增大及最小面压的减小。 相似文献
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层间隔震结构作为一种新型的隔震形式,不仅可以降低上部结构的动力响应,还可以弥补基础隔震结构的不足.现有研究多集中在远场地震作用下的规则层间隔震结构.本文利用通用结构分析与设计软件SAP2000分别模拟了一幢8层带裙房钢筋混凝土框架层间隔震结构、基础隔震结构和抗震结构,分析并对比了三种结构在近场地震作用下动力响应特征.结果表明在近场条件下三种结构顶层均出现不同程度的鞭梢效应;相比抗震结构两种隔震结构具有很好的减震效果,而且基础隔震结构的减震效果好于层间隔震结构;由于结构刚度突变的部位剪力较大,所以应对其裙楼顶部予以加强. 相似文献
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M. N. French R. L. Bras W. F. Krajewski 《Stochastic Environmental Research and Risk Assessment (SERRA)》1992,6(1):27-45
A procedure for short-term rainfall forecasting in real-time is developed and a study of the role of sampling on forecast ability is conducted. Ground level rainfall fields are forecasted using a stochastic space-time rainfall model in state-space form. Updating of the rainfall field in real-time is accomplished using a distributed parameter Kalman filter to optimally combine measurement information and forecast model estimates. The influence of sampling density on forecast accuracy is evaluated using a series of a simulated rainfall events generated with the same stochastic rainfall model. Sampling was conducted at five different network spatial densities. The results quantify the influence of sampling network density on real-time rainfall field forecasting. Statistical analyses of the rainfall field residuals illustrate improvement in one hour lead time forecasts at higher measurement densities. 相似文献
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《中国科学:地球科学(英文版)》2014,(3)
正SCIENCE CHINA Earth Sciences,an academic journal cosponsored by the Chinese Academy of Sciences and the National Natural Science Foundation of China,and published by Science China Press and Springer,is committed to publishing high-quality,original results in both basic and applied research. 相似文献
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《国际泥沙研究》2014,(4)
正Director:Shangfu Kuang,China Vice-directors:Chunhong Hu,China Duihu Ning,China Guangquan Liu,China The International Research and Training Center on Erosion and Sedimentation(IRTCES)was jointly set up by the Government of China and UNESCO on July 21,1984.It aims at the promotion of international exchange of knowledge and cooperation in the studies of erosion and 相似文献
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Richard D. Hey 《地球表面变化过程与地形》1979,4(1):59-72
Feedback mechanisms, which operate upstream through drawdown and backwater effects and downstream through sediment discharge are responsible for channel evolution. By combining these mechanisms with channel processes it euables a dynamic process-response model to be developed to simulate the initial evolution of straight gravel-bed channels. When erosion commences on a land surface, sediment entrained in the headwater reach by hydraulic action is selectively transported, deposited and reworked. This produces a damped oscillation between degradation and aggradation as the channel and valley respond to spatial and temporal variations in sediment calibre and hydraulic conditions. The initial cut and fill phases are responsible for valley incision and floodplain development while secondary and subsequent activity can produce river terraces. Eventually sediment entrainment in the headwaters declines as slopes are reduced. Subsequent channel evolution is relatively insignificant because it is dependent on local weathering activity producing material that can be transported on declining slopes. Therefore landforms produced during the initial phase of development, when local weathering was non-limiting, dominate the landscape. 相似文献