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1.
《地震工程与工程振动》2016,(3)
地震作用下的桩基动力响应问题一直是土动力学和岩土工程抗震领域研究的热点。本文主要基于液化砂土中3×3群桩振动台试验,采用目前常用的大型有限差分软件FLAC~(3D)进行数值模拟研究,将模拟结果与试验分析结果进行对比研究。工况包括:不同峰值加速度的正弦波和El Centro波分别输入下的群桩在干砂和饱和砂土中的侧向动力响应特性,主要对基底台面、桩头承台的加速度与位移时程关系曲线进行对比分析。研究结果表明:随着正弦波峰值加速度输入的增加,群桩横向动力响应明显,尤其是当加速度为0.15 g时砂土发生液化,反应达到最大,数值模拟结果与试验吻合较好。地震波输入工况下也可以得到类似的结论,其中干砂与液化砂土的承台加速度、位移相对台面的均有所放大,但放大倍数不同。 相似文献
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均匀土-桩基-结构相互作用体系的计算分析 总被引：14，自引：4，他引：14
本文以结构－地基动力相互作用振动台模型试验为基础，结合通用有限元软件ANSYS，对均匀土－桩基－结构动力相互作用体系进行了三维有限元分析。计算中土体采用等效线性模型，利用面－面接触单元考虑土体与结构交界面的状态非线性，计算与试验得出的规律基本一致。桩基与土体间发生了脱开再闭合和滑移现象。桩身应变幅值分布呈桩顶大、桩尖小的倒三角分布，角桩的应变幅值较大，边排中桩和中桩的应变幅值较小。桩土接触压力幅值呈桩顶小、桩尖大的三角形分布。在沿振动方向的三排桩中，边排桩的滑移比中排桩的滑移量大。通过计算分析与试验的对照研究，验证了采用的计算模型与分析方法的合理性，为结构－地基相互作用的进一步研究奠定了基础。 相似文献
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桩-土-上部结构体系的动力相互作用是一个复杂的过程,尤其是在倾斜液化侧向扩展流动（侧扩流）场地中,由于地震过程中场地产生地面永久大变形,桩土间有可能产生错动滑移与开裂等非线性反应,因此桩-土相互作用模拟至关重要。为了探究桩-土非线性接触对倾斜液化场地-群桩基础-上部结构体系动力响应的影响,本文基于OpenSees分别建立了考虑桩-土相互作用弹簧和桩土结点之间直接绑定的有限元数值模型。结果表明：考虑桩-土相互作用Pyliq弹簧时,土体加速度幅值略微降低,桩基对土体的约束明显变弱,土体残余位移增大。同时,具有Pyliq弹簧的模型能较好地模拟桩的曲率响应,而采用桩土结点直接绑定的模型高估了桩顶曲率,进而无法准确估计桩基抗弯最不利位置。桩-土相互作用弹簧对上部结构动力响应的影响较小。 相似文献
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液化土体中桩基侧向动力响应一直是目前岩土工程界和地震工程领域关注的热点研究问题之一.本文基于振动台实验,首次将光纤布拉格光栅(FBG)技术应用到液化土体桩基侧向动力响应分析方法中.实验结果表明:采用FBG传感系统可以测得桩身侧向动力响应,与传统电阻式应变片法相比简洁方便;FBG测量土体位移同样有效可行,可代替以往加速度积分求解土体位移;后处理得到的桩基侧向动力p-y滞回曲线能更好地反映桩土之间真实的动力本构关系,并与干砂动力p-y曲线相比,探讨两种不同场地条件下桩基侧向动力响应机制与p-y曲线的发展变化模式,为以后液化土中桩基侧向动力响应问题的研究奠定了理论基础. 相似文献
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桩基础是松软深厚地基上高层建筑的主要基础形式,其长度直接影响高层建筑的抗震性能。尽管桩基础有较广的应用范围,但桩长与结构整体抗震性能的相关性研究还颇为少见。根据上海某高层建筑地基基础结构数据建立软土地基上桩基础高层建筑平面动力有限元计算模型,以横观各向同性材料模拟软土地基,弹性阻尼人工边界模拟地基半无限体,薄膜单元模拟桩土间接触滑移性能,并考虑桩-土-结构共同作用,采用上海地铁某车站地震监测数据作为地震波输入,在其他条件不变的情况下选择各种桩长进行计算,根据计算结果分析讨论在该模型条件下桩长选择对上部结构以及桩基础整体抗震性能的影响,提出优化方案。 相似文献
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结合典型工程实例，采用在土体侧向边界节点处用弹簧并联阻尼器来进行模拟，在平面应变单元和桩体梁单元连接处用约束方程的方法进行节点耦合、满足连续条件，选择桩、土、荷载参数，用整体有限元方法进行桩－土－结构相互作用体系的地震反应分析。重点讨论了三种不同的上部结构刚度对桩基地震内力的影响，得到了在水平地震荷载作用下上部结构刚度的增大将增大桩基的内力及水平位移，且桩顶及桩身处于第一个软硬土层交界面处的截面的内力尤为突出等结论。关键词：上部结构刚度改变；桩－土－结构相互作用；弹性－阻尼边界；地震反应分析 相似文献
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层状土介质中群桩及其上部结构体系对任意入射地震波的响应 总被引：2，自引：0，他引：2
本文舍弃桩基动力分析中的土介平面应变假定，采用薄层内位移纡性变化条件下的动力Ｇｒｅｅｎ函数形成桩－土－桩相互作用所需的土介质柔度矩阵，用梁单元模拟桩的运动，用振型分解方法来考虑上部结构与桩基承台间的动力相互作用，以任意地震波入射为初始运动输入，建立了层状土介质中群桩及其上部结构体系对放射地震波响应的半解析分析模型，研究了桩基及其上部结构体系对不同角度入射、ＳＨ、ＳＶ和Ｐ波的动力响应，结果表明，本文 相似文献
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桩贯入地基过程的动画仿真 总被引：1，自引：0，他引：1
本文通过三维显式有限元计算结果，对混凝土桩打基的过程进行了三堆动力反应分析，褡完成了此过程的动画仿真研究，研制成可携带的录相带工匠仿真动画，形象，生动，直观地再现了桩贯入地基过程中撞击波在桩体，地基中的传播，桩体与地基间的相对接触，滑移及桩锤与桩头部间的接触撞击过程。 相似文献
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基于OpenSees数值分析平台,建立了群桩-土-桥墩非线性数值分析模型。模型中桩-土水平向相互作用和桩-土竖向相互作用、桩底-土竖向相互作用分别通过p-y、t-z与q-z零长度弹簧单元模拟。模型中同时考虑了群桩效应与纵筋在墩底的应变渗透和粘结滑移的影响。结合群桩基础拟静力试验结果,对数值模型的准确性进行了验证,在此基础上对土体参数特性对桩基滞回性能的影响规律进行了分析。结果表明:所建立的数值分析模型可对群桩基础滞回曲线和骨架曲线进行较为准确的模拟分析,验证了模型的可靠性。反复荷载作用下,前桩处土体的反应明显大于中桩处;土体由软黏土变为硬黏土时,墩顶侧向承载力与刚度显著增加,但土体的非线性反应减弱。 相似文献
10.
分层液化土中桩基侧向动力反应机理的试验研究 总被引：2，自引：0，他引：2
饱和砂土中的桩基侧向动力响应研究一直是岩土工程界与地震工程领域关注的热点,尤其是群桩侧向动力响应机制是需要重点研究的课题之一。基于振动台试验,通过输入2种不同的波形,采用FBG光栅传感系统对饱和砂土中的单桩与群桩侧向动力响应特性和典型测试点的桩土动力p—y滞洄曲线进行研究。研究结果表明：振动初期,单桩和群桩试验孔压增长不大,随后单桩孔压迅速上升,振动后期逐渐下降至0.5,而群桩孔压则上升缓慢;单桩试验土表加速度在振动初期逐步升高后又迅速降低,且加速度放大值略大于台面加速度值,群桩试验土表加速度在振动初期逐渐升高时就达到了最大,且随着孔压比的升高,加速度没有继续放大,而是逐渐减小,直到后期与单桩试验土表加速度重合;饱和砂土液化对单桩承台加速度和位移的影响较大,群桩承台侧向动力响应对液化的敏感程度略低于单桩承台;在振动输入和承台输入相同的条件下,液化后的群桩基础比单桩基础能更好地抵抗侧向力的作用。 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
16.
《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
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Based on relocating the Jiujiang-Ruichang earthquake sequence which occurred on November 26, 2005 in Jiangxi Province with the double-difference （DD） algorithm and master event technique, the paper discusses the focal mechanism of the main shock （MsS.7） and the probable seismo-tectonics. The precise relocation results indicate that the average horizontal error is 0.31kin in a EW direction and 0.40kin in a NS direction, and the average depth error is 0.48kin. The focal depths vary from 8kin to 14kin, with the predominant distribution at 10kin - 12kin. The epicenter of the main shock is relocated to be 29.69^oN, 115.74^oE and the focal depth is about 10.Skin. Combining the predominant distribution of the earthquake sequence, the focal mechanism of the main shock and the tectonic conditions of N-E- and NW-strike faults growth in the seismic region, we infer that the main shock of the earthquake sequence was caused by a NW striking buried fault in the Rnichang basin. The nature of seismic faults needs to be further explored. 相似文献
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《水文科学杂志》2013,58(6)
Abstract The western reservoirs represent the principal groundwater system in Morocco. Demographic, industrial and agricultural developments during the last decade have markedly altered groundwater quality. The Mamora coastal aquifer system is among the Atlantic systems which are most heavily threatened by pollution. Agricultural and industrial activities, and rapid urban growth contribute to the pollution of the groundwater. Contamination transport is facilitated by a high permeability of the aquifer formations. In order to assess the actual groundwater quality of the Mamora aquifer and to understand the influence of the factors generating the pollution, an extensive multidisciplinary research programme is in progress, with hydrochemistry and microbiology playing essential roles. The present paper concerns the spatial distribution of physico-chemical parameters in the groundwater, subjected to domestic, industrial and agricultural pollution. Fifty-seven samples were analysed for several parameters (Ca2+, Mg2+, Na+, K+, Cl?, SO4 2?, HCO3 ?, NO3 ?, pH, electrical conductivity and temperature). The microbiological analysis of 143 samples reveals the presence of four kinds of indicator bacteria in the groundwater resources: faecal Streptococci, faecal coliform, Escherichia coli and Clostridium. The physico-chemical results and bacteriological monitoring show that the nitrate and bacteria concentrations exceed the maximum admissible levels, notably around pumping stations in the sectors of Sidi Taibi, Sidi Ahmed Taleb and Aïn Sbaâ. Contamination is generated by uncontrolled anthropogenic activities and accentuated by the high intrinsic vulnerability of the aquifer system. Several parameters appeared to exceed admissibility standards. Measures are recommended to prevent groundwater pollution in the region. 相似文献
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K.-G. Malle 《洁净——土壤、空气、水》1992,20(4):196-204
Zinc in the Environment. In 1990 the world production of zinc ammounted to 7 Mio. metric tons. The main areas of application were: galvanization, alloys like brass and zinc metal. The content in the earth crust varies between 10–300 ppm zinc with a mean of 70 ppm. Uncontaminated surface waters contain less than 10 mg/m3 zinc. Apart from civilization air contains 1–10 ng zinc per m3. These background concentrations are exceeded by orders of magnitude in zinc deposit areas and where anthropogenic influences predominate. Accumulation can occur in sediments and sewage sludge. Molluscs and Algae also accumulate zinc. Zinc is essential for live. With normal food the zinc supply of man is just sufficient. Bioaccumulation of zinc towards man or chronic oversupply of man is not known. Zinc has no teratogenic or mutagenic effects, a suspicion on a carcinogenic effect proved wrong. In stockbreeding and plant cultivation a minimum supply of zinc is necessary. Plants are relatively less sensitive against higher soil contents of zinc. Considering the toxicological and ecotoxicological effects of zinc in the environment, the critical organismens are marine invertebratae like tubifex, daphnia, gammarus and algae. But normally only a minor part of the total zinc contest is biologically available, depending on salt content and pH of the waters. 相似文献