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1.
沉积河谷对地震动具有显著的放大效应,而软夹层的存在对其放大程度具有较大影响。采用一种高精度有限元-间接边界积分方程耦合方法,对P、SV和Rayleigh波入射下含软夹层层状沉积谷地地震响应进行计算分析。分析表明,软夹层的影响规律依赖于入射波的波型、频率和角度、软夹层的厚度和埋深等因素。整体上看,对于地表位移,较低频率地震波入射下,软夹层的放大效应比较明显,且较厚夹层在浅埋情况下的放大作用更为显著;对高频波入射则主要表现为减震效应。对于地表加速度,软夹层主要表现出降幅作用,降低幅度可达30%。另外,总体上软夹层对于P波的影响要大于对SV波的影响。  相似文献   

2.
刘中宪  尚策  王小燕  王冬 《地震学报》2017,39(1):111-131
基于一种高精度间接边界元法(IBEM), 实现了沉积盆地三维地震响应的频域、 时域精细求解, 并以半空间中椭球形沉积盆地对平面P波和SV波的散射为例, 着重探讨了入射角度、 入射波型、 入射频率、 盆地长宽比和深宽比对沉积盆地地震动放大效应的影响规律. 结果表明: 盆地形状对地震波的放大效应和空间分布状态具有显著影响, 且具体规律受控于入射波频段. ① 随着盆地深度增大, 盆地边缘面波发育更为充分, 在较宽频段内均会出现显著的地震动放大效应, 且深盆地的放大区域集中于盆地中部. ② 圆形盆地对地震波的汇聚效应最为显著, 而狭长盆地对地震波的汇聚作用相对较弱, 高频情况下可在盆地内部形成多个聚焦区域. ③ 不同波型入射下, 盆地对地震动放大效应的机制有所差异: P波入射下, 竖向位移放大主要是由于盆地边缘面波由四周向中部汇聚所致; SV波入射下, 边缘面波汇聚效应相对较弱, 而当盆地较深时, 底部透射体波和边缘面波易形成同相干涉从而显著放大地震动. 按盆地内外介质波速比为1/2, P波和SV波垂直入射下频域最大放大倍数分别为25和15, 时域放大倍数约为4.0和3.7(雷克子波). ④ 低频波入射下, 位移从盆地中部向边缘逐渐减小, 且浅层沉积盆地对地表位移幅值的放大作用不明显. ⑤ P波和SV波的入射角度对盆地地震动放大幅值及空间分布特征也具有显著影响.   相似文献   

3.
圆弧状沉积盆地与软土单覆盖层出平面地表运动对比   总被引:2,自引:0,他引:2  
采用解析方法,通过圆弧状沉积盆地与同样参数的软土均匀单覆盖层的对比,研究沉积盆地对平面SH波二维散射效应和其出平面地表运动。数值对比结果表明:(1)波垂直入射时盆地中央地表位移幅值反应,其随频率变化形式与软土单覆盖层的地表运动有较强的对应性,且此时单覆盖层地表位移幅值为其下降;(2)盆地的二维散射效应特点显著波的汇聚作用使盆地中的地表运动显著放大,总体上较软土单覆盖层的地表位移幅值要大,其频域内的最大反应则明显大于单覆盖层情况,但最大反应在盆地表面出现的位置依赖于入射波角度、盆地深宽比和盆地的软硬程度;(3)沉积盆地中地表位移运动有强烈扭转效应,且随盆地变软和入射波频率增高而增强。  相似文献   

4.
地下综合管廊由于埋深较浅,Rayleigh波能量对综合管廊的地震反应具有重要影响。建立非线性有限元三维动力数值模型,通过边界脉冲荷载生成Rayleigh波,研究Rayleigh波平行入射条件下综合管廊结构的加速度、位移和内力等响应特性,然后分别研究管廊断面尺寸、覆土厚度、Rayleigh波入射角和土体本构等因素对管廊结构动力响应特征的影响。研究结果表明:Rayleigh波平行入射作用下,综合管廊结构顶板受力表现为时而受拉以及时而受压,Rayleigh波传递过程对管廊结构受力产生不利影响;当Rayleigh波入射方向与管廊结构轴向夹角越接近90°,引起的动力响应相对越大;土体采用摩尔-库伦模型(MC模型)时,由于不能考虑材料滞回环属性对能量的耗散,相对于小应变硬化模型(HSS模型)模拟出的管廊结构内力和位移响应要大;管廊埋深越浅,结构位移响应幅值和内力响应幅度变化越大;不同截面管廊结构的纵向位移差别不大,竖向位移则随截面增大而减小,表明随着截面刚度的提高,抗变形能力增强;管廊结构内力峰值变化量随截面增大而减小,单仓结构在Rayleigh波作用下的内力响应最为显著。  相似文献   

5.
沉积河谷对地震波的高频散射规律尚不明确。采用一种高精度间接边界元法(IBEM)用于沉积河谷对平面P、SV和Rayleigh波的二维散射宽频求解分析。数值结果表明:IBEM可高效精确地模拟地震波的宽频散射;中低频段(无量纲频率η5.0),河谷地形对地震波的放大效应显著;高频波段(η10.0),河谷放大效应减弱甚至出现缩幅效应。随河谷深度增加,位移放大频段的带宽逐渐减小,第一峰值频率降低,且在低频段频谱曲线振荡剧烈。阻尼比对沉积河谷地表位移幅值具有显著影响,尤其是在高频段衰减作用明显。实际沉积河谷场地地震反应分析,需充分考虑波型、入射波频率和角度、河谷深宽比等因素,以更科学地进行震害解释和地震安全性评价。  相似文献   

6.
于琴  刘中宪  何颖 《地震学报》2017,39(6):1-14
基于间接边界元法计算沉积河谷对平面P波和SV波的二维散射,着重考察沉积介质波速和材料阻尼的随机性对河谷地震动放大效应。利用蒙特卡罗方法随机模拟产生了波速样本和阻尼样本各30组,给出了不同入射角度和频率P波和SV波入射下河谷随机响应的单频和频谱结果。算例分析结果表明:(1)地表位移响应幅值的变异系数极值均显著大于波速比变异系数,且波速比的随机性对地表位移的影响在体系共振频率处最为明显,地表位移的最大标准差可达7.168;低频情况下,沉积中部地震反应变异性更显著,高频情况下则在沉积河谷边缘变异性最大;(2)入射波角度对地表位移响应变异系数极值的影响不大,但对变异系数空间变化的影响显著;(3)阻尼的随机性对地表位移的影响在低频情况下较小,在高频情况下则较明显,尤其是在沉积河谷的体系自振频率处,其影响最为显著。   相似文献   

7.
层状半空间中洞室对入射平面P波的放大作用   总被引:4,自引:0,他引:4  
文中利用间接边界元法,在频域内求解了层状弹性半空间中洞室对入射平面P波的放大作用问题。通过自由场反应分析,求得假想洞室边界上各单元的应力响应。在洞室边界各个单元上施加虚拟分布荷载,求得位移和应力的格林函数。根据应力边界条件确定虚拟分布荷载,将自由场位移响应和虚拟分布荷载产生的位移响应叠加起来,即得到问题的解答。比较了层状半空间和均匀半空间中洞室对入射平面P波的放大作用,结果表明,层状半空间情况有可能导致较大的地表位移幅值,尤其是对于较低频率入射波。  相似文献   

8.
本文采用波函数展开法给出弹性半空间中隧道-土-隧道轴向动力相互作用的一个解析解,并通过对地表位移残差的收敛性分析对解析解的精度进行了验证。研究了隧道埋深、隧道质量、隧道间距、波入射频率和入射角度等参数对隧道轴向动力响应的影响。研究表明,隧道埋深越小,隧道动力响应越大;隧道质量越大,隧道动力响应越大;隧道间距越小,隧道动力响应越大,但隧道间距的影响并不是单调变化,与波入射频率密切相关,两个隧道情况动力响应幅值可达单隧道情况的2.7倍。当隧道间距较小时,地下隧道的抗震设计需要考虑隧道之间的影响。  相似文献   

9.
黄磊  刘中宪  张雪  李程程 《地震学报》2020,42(6):657-668
结合单相介质动力格林函数和流体域格林函数,将间接边界元方法拓展到含流体层河谷对地震波散射的求解,并结合具体算例进行大量参数分析。研究结果表明,含流体层河谷地形对平面P波、SV波入射时的地震响应受控于入射波频率、入射波角度及流体深度等多种因素。总体来看:① 在低频域内,含流体河谷底部及附近地表的频谱特性与不含流体的河谷反应基本一致;② P波入射时在水层体系共振频率处,河谷底部位移缩小效应显著,而此频率处流体表面位移达到最大;③ 流体层具有吸收地震波能量的作用,流体深度越大,河谷表面及附近地表的地震动位移越小。研究成果可在一定程度上为河谷地形附近地震动效应的评估及防震减灾工作提供理论依据。   相似文献   

10.
地震体波斜入射情形下台阶地形引起的波型转换   总被引:12,自引:0,他引:12  
本文首次对地震体波斜入射情形下竖直、倾斜台阶地形引起的波型转换进行了数值模拟,结果表明:地震波的斜入射会使台阶上角点引起更强的转换面波;转换Rayleigh面波最大振幅可达弹性半空间表面自由场位移的1.1倍左右。  相似文献   

11.
A two-dimensional soil-structure interaction analysis is carried out for transient Rayleigh surface waves that are incident on a structure. The structure is modelled by a three-degree of freedom rigid basemat to which is attached a flexible superstructure, modelled by a single mass-spring system. The structural responses to a given Rayleigh wave train are compared with those that would have been obtained if the free-field acceleration-time history had been applied as a normally incident body wave. The results clearly exhibit the [frequency filtering] effects of the rigid basemat on the incident Rayleigh waves. It is shown that, if seismic excitation of a structure is, in fact, due to Rayleigh surface waves, then an analysis assuming normally incident body waves can considerably over-estimate structural response, both at basemat level for horizontal and vertical motions and for vertical oscillations of the superstructure. However, in the examples considered here, relatively large rocking effects were induced by the Rayleigh waves, thus giving maximum horizontal accelerations in the superstructure that were of comparable magnitude for Rayleigh and normally incident body waves.  相似文献   

12.
The effect of topography and subsurface inhomogeneity on surface motion is investigated in the case of Rayleigh waves. In the previous paper, the same effect was investigated in the case of SV waves. Several types of topography, such as cliffs both with and without a soft layer at the foot of the slope, are considered. Computations are made using a new hybrid method combining a particle model with a finite element method. In cases of harmonic Rayleigh waves, surface motions with amplitudes as large as 1.5 to 5 times the horizontal surface displacement of the incident Rayleigh waves are produced near the slope and the sloping interface. When a Rayleigh wave propagating through a hard single-layered ground encounters a sloping interface where hard ground and soft ground make contact with each other, Rayleigh waves having two different, phase velocities are produced and they correspond to the fundamental mode, and the first mode determined by Haskell's method. In addition, the transient response when Rayleigh waves propagate through the cliff is also simulated. Assuming the vertical component of the Tokachi-oki Earthquake (1968) measured on the surface to be a Rayleigh wave, the incident Rayleigh wave can be obtained by a Fourier synthesis of eigenfunctions of Rayleigh waves.  相似文献   

13.
In this study, A time-domain seismic response analysis method and a calculation model of the underground structure that can realize the input of seismic P, SV and Rayleigh waves are established, based on the viscoelastic artificial boundary elements and the boundary substructure method for seismic wave input. After verifying the calculation accuracy, a comparative study on seismic response of a shallow-buried, double-deck, double-span subway station structure under incident P, SV and Rayleigh waves is conducted. The research results show that there are certain differences in the cross-sectional internal force distribution characteristics of underground structures under different types of seismic waves. The research results show that there are certain differences in the internal force distribution characteristics of underground structures under different types of seismic waves. At the bottom of the side wall, the top and bottom of the center pillar of the underground structure, the section bending moments of the underground structure under the incidences of SV wave and Rayleigh wave are relatively close, and are significantly larger than the calculation result under the incidence of P wave. At the center of the side wall and the top floor of the structure, the peak value of the cross-sectional internal force under the incident Rayleigh wave is larger than the calculation result under SV wave. In addition, the floor of the underground structure under Rayleigh waves vibrates in both the horizontal and vertical directions, and the magnification effect in the vertical direction is more significant. Considering that the current seismic research of underground structures mainly considers the effect of body waves such as the shear waves, sufficient attention should be paid to the incidence of Rayleigh waves in the future seismic design of shallow underground structures.  相似文献   

14.
The effect of topography and subsurface inhomogeneity on surface motion is investigated in the case of incident SV waves. Several types of topography, such as a cliff, a cliff with a soft layer and filled land, are considered. Computations are made using a new method combining a particle model with a finite element method. The accuracy of this method is discussed through comparisons with Wong's solutions, which are in good agreement. It is found that the surface displacement is very much influenced by surface irregularities when the incident wavelengths are comparable to the size of the topographic features. Rayleigh waves are strongly produced in the neighbourhoods of the slopes of a cliff and a cliff with a soft layer, the latter being a cliff adjacent to and covered at its foot by a soft layer. Thus, a zone of large amplification takes place near a slope, combining incident SV waves and Rayleigh waves. A large displacement also occurs at the upper corner of the slope. In filled land, vertical and horizontal displacements are produced, which are 3 times larger than those at a distance. The present results are considered to be significant from the viewpoint of engineering seismology.  相似文献   

15.
The dynamic response of a finite number of flexible surface foundations subjected to harmonic incident Rayleigh or SH waves is presented. The foundations are assumed to be resting on an elastic half-space. The results show that the foundation stiffness has a marked effect on the vertical response, while there is only a minor effect on the horizontal displacements. In general, the dynamic response decreases with increasing foundation stiffness. In cases of Rayleigh wave incidence, the existence of an adjacent foundation generates a certain amount of horizontal response in the direction perpendicular to the incident wave and subsequently causes the system to undergo a torsional motion; while in cases of horizontally incident SH waves, a vertical response has been observed and its magnitude is comparable to the response in the direction of the incident wave.  相似文献   

16.
基于多自由度空间结构体系地震响应分析的基本理论,利用ANSYS建立空间有限元模型,采用动力时程分析法分析某大跨度连续钢桁架柔性拱桥在一致和非一致激励作用不同地震工况下的空间地震响应。研究结果表明:非一致激励作用下,拱肋轴力、主桁弯矩峰值出现在拱脚和边墩附近;地震波组合输入较其单向输入拱脚轴力和面内弯矩最大分别可达1.28和8.32倍;非一致输入较一致激励作用拱脚轴力和面内弯矩分别可达2.5和8.4倍;地震波横向输入较纵向输入横向位移峰值比可达2.4倍,纵向输入较横向输入纵向位移峰值比可达2.6倍;结构的支座形式对结构构件地震响应结果也有一定影响;建议大跨度钢桁拱桥抗震设计应充分考虑地震波的空间和时间效应。  相似文献   

17.
Rayleigh波在浅圆凹陷地形附近的散射:高频解答   总被引:4,自引:1,他引:4  
利用波函数展开法给出了Rayleigh波在浅圆凹陷地形附近散射的一个高频解析解,并分析了入射频率、凹陷地形宽度和深度等因素对波散射的影响。数值结果表明,由于Rayleigh波幅值随深度而衰减,凹陷地形表面位移幅值整体上较小,且随着凹陷地形深度的增加而减小;由于Rayleigh波幅值还随频率而衰减,随着入射频率的升高,凹陷地形表面位移幅值逐渐减小;由于凹陷地形的屏障作用,在人射波的近端,地表位移分布变得相对复杂,地表位移峰值出现在左角点附近,而在入射波远端,地表位移分布相对简单,地表位移峰值出现在距凹陷地形较远的地方。  相似文献   

18.
在远场地震作用下单桩横向地震响应研究的基础上,引入相互作用因子,研究了远场地震作用下成层地基中桩与桩的横向动力相互作用,得到了桩间距、桩土刚度比、桩顶约束条件、瑞利波入射角度、震动频率是影响群桩横向动力相互作用主要因素的结论,为进一步研究远场地震作用下群桩的横向地震响应打下了基础。  相似文献   

19.
Seismic ground motions of two neighboring mountains and the free surface between them are calculated under the SV seismic waves with three different incident angles. The results are then taken as the inputs of multi-point seismic excitations for the foundation of a long-span bridge built over the valley in the analysis considering the integrated influence of traveling wave and topography. On the basis of a dynamic analytical method, a finite element model is created for the seismic responses of a four-span rigid-frame bridge of 440 m. The pier-top displacement and the pier-bottom internal force of the bridge are calculated. Then the results are compared with those considering traveling-wave effect only. The conclusions can serve as a seismic design reference for the structures located on the complex mountain topography.  相似文献   

20.
When analysing the seismic response of pile groups, a vertically‐incident wavefield is usually employed even though it does not necessarily correspond to the worst case scenario. This work aims to study the influences of both the type of seismic body wave and its angle of incidence on the dynamic response of pile foundations. To this end, the formulation of SV, SH and P obliquely‐incident waves is presented and implemented in a frequency‐domain boundary element‐finite element code for the dynamic analysis of pile foundations and piled structures. Results are presented in terms of bending moments at cap level of single piles and 3 × 3 pile groups, both in frequency and in time domains. It is found that, in general, the vertical incidence is not the most unfavourable situation. In particular, obliquely‐incident SV waves with angles of incidence smaller than the critical one, a situation in which the mechanism of propagation of the waves in the soil changes and surface waves appear, yield bending moments much larger than those obtained for vertically‐incident wavefields. It is also shown that the influence of pile‐to‐pile interaction on the kinematic bending moments becomes significant for non‐vertical incidence, especially for P and SV waves. Copyright © 2013 John Wiley & Sons, Ltd.  相似文献   

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