北京建筑大学学报
北京建築大學學報
북경건축대학학보
Journal of Beijing Institute of Civil Engineering and Architecture
2015年
1期
17-24
,共8页
孙健%陈昊祥%戚承志
孫健%陳昊祥%慼承誌
손건%진호상%척승지
液化场地%地下结构%地震%影响因素
液化場地%地下結構%地震%影響因素
액화장지%지하결구%지진%영향인소
liquefied soil%underground structure%earthquake%the effect factor
目前,我国在地下结构抗震分析与液化破坏研究中尚存在诸多问题,需要深入研究地下结构的动力响应分析的影响因素:对不同结构截面形式、水平-竖向波共同作用、不同地震波输入。在地震作用下处于可液化场地的拱形结构和矩形结构的受力形式和最不利受力位置;模型分别在竖向波以及横向波单独和共同作用下,孔压比幅值也不相同;不同地震波对结构的受力形式影响不大,却对结构加速度影响十分巨大。这些问题的研究分析对可液化场地下结构在地震作用下的动力响应规律与液化破坏形式具有重要的工程应用价值和意义。
目前,我國在地下結構抗震分析與液化破壞研究中尚存在諸多問題,需要深入研究地下結構的動力響應分析的影響因素:對不同結構截麵形式、水平-豎嚮波共同作用、不同地震波輸入。在地震作用下處于可液化場地的拱形結構和矩形結構的受力形式和最不利受力位置;模型分彆在豎嚮波以及橫嚮波單獨和共同作用下,孔壓比幅值也不相同;不同地震波對結構的受力形式影響不大,卻對結構加速度影響十分巨大。這些問題的研究分析對可液化場地下結構在地震作用下的動力響應規律與液化破壞形式具有重要的工程應用價值和意義。
목전,아국재지하결구항진분석여액화파배연구중상존재제다문제,수요심입연구지하결구적동력향응분석적영향인소:대불동결구절면형식、수평-수향파공동작용、불동지진파수입。재지진작용하처우가액화장지적공형결구화구형결구적수력형식화최불리수력위치;모형분별재수향파이급횡향파단독화공동작용하,공압비폭치야불상동;불동지진파대결구적수력형식영향불대,각대결구가속도영향십분거대。저사문제적연구분석대가액화장지하결구재지진작용하적동력향응규률여액화파배형식구유중요적공정응용개치화의의。
At present, there are many problems still existing in the seismic analysis of underground structure and research of liquefaction failure. They are needed to be investigated further. This paper emphasizes on three factors which effect analysis of dynamic response of the underground structure:different forms of structural section, combinational action of horizontal and vertical wave and inputtingdifferent seismic wave. The stress forms and the most adverse location of arch and rectangular structure in the liquefiable site under seismic activity are addressed. The model is under the attack of transverse waves and longitudinal waves respectively and collectively. And the amplitude of pore pressure ratio is various. Different seismic waves have little influence on the stress forms of structure. But the acceleration of structure varies with different seismic waves remarkably; The research and analysis on above problems have important engineering application value and significance of the dynamic response law and liquefaction failure form of underground structures in liquefiable soil when the earthquake strikes.