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1.
黄雨  郝亮 《工程地质学报》2008,16(2):184-188
地震诱发的地基液化对桩基础的破坏极大,液化地基中桩的破坏机理是岩土地震工程中的一个重要研究课题。目前地基液化时桩土结构系统的地震性态尚没有认识充分,已有的研究内容较多局限于桩身材料的强度破坏方面,难以考虑液化土体侧向流动、基桩屈曲失稳、以及土与结构动力相互作用等复杂因素的影响。本文重点加强以下3个方面的深入探讨和研究:(1)液化地基中桩的屈曲失稳;(2)液化地基中桩基破坏的数值模拟新方法;(3)液化地基中桩-土-结构的动力相互作用分析。  相似文献   

2.
为研究液化场地中群桩在强震作用下的动力响应特征及桩侧土抗力-桩土相对位移(p-y)曲线规律,依托海文大桥实体工程,基于振动台模型试验,开展了0.15g~0.35g地震动作用饱和粉细砂土层不同埋置深度下的砂土孔压比、桩身弯矩及p-y曲线动力响应研究。结果表明:地震动强度达到0.25g时,不同埋置深度下的饱和粉细砂土层孔压比均大于0.8,产生液化现象,且随埋置深度增加,孔压比增长时刻明显滞后;不同埋置深度下,桩身弯矩最大值均位于液化土层和非液化土层分界面处;同一埋置深度时,随地震动强度的增大,p-y曲线所包围的面积逐渐增大,其整体斜率逐渐变小,说明桩-土相互作用动力耗能逐渐增大,桩周土体刚度逐渐减小;随埋置深度增加,p-y曲线所包围的面积逐渐减小,其整体斜率逐渐增大,说明桩-土相互作用动力耗能逐渐减小,桩周土体刚度逐渐增大。因此,液化场地桥梁群桩抗震设计时,应综合考虑液化土层与桩基础的相互位置关系,确保桩基础在液化土层与非液化土层分界处的抗弯承载能力。  相似文献   

3.
One of the major causes of earthquake damage is liquefaction. However, it doesn't result in severe harm unless it leads to ground surface damage or ground failure. Therefore, prediction of potential for ground surface damage due to liquefaction is one of the important issues in microzonation studies for liquefaction-induced damage in areas with high seismicity. In 1985, based on a database compiled from Chinese and Japanese earthquakes, Ishihara considered the influence of the non-liquefied cap soil on the occurrence or non-occurrence of ground failure (mainly sand boiling), and proposed an empirical approach to predict the potential for ground surface damage at sites susceptible to liquefaction. However, some investigators indicated that this approach is not generally valid for sites susceptible to lateral spread or ground oscillation. In this study, a contribution to improve the approach by Ishihara is made. For the purpose, an index called liquefaction severity index (LSI) and data from two devastating earthquakes, which occurred in Turkey and Taiwan in 1999, were employed. The data from liquefied and non-liquefied sites were grouped and then analysed. Based on the observations reported by reconnaissance teams who visited both earthquake sites and the results of the liquefaction potential analyses using the filed-performance data, a chart to assess the potential for ground surface disruption at liquefaction-prone areas was produced. The analyses suggest that the procedure proposed by Ishihara is quite effective particularly for the occurrence of sand boils, while the bounds suggested in this method generally may not be valid for the prediction of liquefaction-induced ground surface disruption at sites susceptible to lateral spreading. The chart proposed in this study shows an improvement over the Ishihara's approach for predicting the liquefaction-induced ground surface damage. The microzonation maps comparing the liquefaction sites observed along the southern shore of Izmit Bay and in Yuanlin, and the surface damage and non-damage zones predicted from the proposed chart can identify accurately the liquefaction (sand boiling and lateral spreading) and no-liquefaction sites.  相似文献   

4.
地震历史对砂土抗液化性能影响的试验研究   总被引:1,自引:0,他引:1  
苏栋  李相崧 《岩土力学》2006,27(10):1815-1818
为探讨地震历史对饱和砂土抗液化性能的影响,通过离心机动力模型试验,观测了遭受过不同强度地震的饱和砂土水平场地在再次地震荷载作用下的响应,包括超静孔隙水压力的发展和土体的变形。研究表明,小地震有利于增强砂土颗粒之间的咬合及结构的稳定性,极大地提高了其抗液化能力,而遭受强地震并且发生液化的砂土,由于在沉积过程中形成的不稳定结构,则可能在将来强度相对较小的地震中再次液化。试验结果说明了地震历史对砂土液化性能有重大影响及进一步开展砂土细观结构研究的重要性。  相似文献   

5.
砂土液化是地震主要次生地质灾害之一。在512汶川地震中,德阳等地发生较大面积砂土液化现象。为详细了解液化带工程地质基本特征,选择板桥学校液化带进行详细液化震害调查、钻探和现场试验。结果表明:(1)液化震害典型,主要包括喷水冒砂、地表裂缝、侧移和基础下沉等;(2)砾石层是唯一的无粘性土层,砾石层分为性质不同的全新世沉积和更新世沉积两部分,未见砂层分布;(3)液化土层是全新统砾石层,该砾石的颗粒大小分布特征表现为级配不良,并有粒组缺失现象;(4)非液化盖层对喷出物有过滤作用,砂粒等细颗粒容易沿裂缝喷出地表,卵砾石等粗颗粒受阻留在土层中,导致喷出物为砂土。  相似文献   

6.
A numerical model of a centrifuge experiment on tunnel located in sand is being presented. The experiment was carried out under seismic loading using a dynamic actuator. The responses of the tunnel and of the sand were measured. The numerical model is based on a hypoplastic constitutive model with intergranular strains implemented in the FE-code TOCHNOG. The calculated accelerations in the sand match the measured results, while the surface settlement and the bending moments in the tunnel lining are only qualitatively reproduced by the numerical model.  相似文献   

7.
Despite advances in the numerical analysis of saturated sand behavior under earthquake loading, accurate prediction of liquefaction-related phenomena by numerical simulation remains a challenge. Variation of the coefficient of permeability is a key issue which has not obtained due attention in most previous modeling. In this study, a revised form of a recently proposed variable permeability function was implemented in a fully coupled dynamic model adopting modern two-surface plasticity constitutive law to evaluate the effects of permeability variations on the results of numerical modeling. The variable permeability model is comprised of a simple function relating the permeability coefficient of soil mass to the excess pore water ratio. In this study, the constants of the variable permeability function were attained based mainly on theoretical evidence and experimental observation. Well-documented centrifuge experiments were examined to evaluate how well the proposed model captures the main features of soil response to earthquake loading. The results indicate that the proposed function greatly enhanced the capability of numerical modeling to predict the behavior of saturated sand under cyclic loading. Particularly, the variable permeability model with proposed constants significantly improved the amount of liquefaction-induced settlement predicted by numerical modeling.  相似文献   

8.
侯娟  张孟喜  张陶陶  戴治恒 《岩土力学》2015,36(Z2):702-708
建立了横-竖立体加筋(H-V筋)地基的有限元模型,通过分析地基中的竖向应力分布、水平向位移分布以及筋-土界面相互作用,发现横-竖立体加筋地基中的竖向应力在筋材下方出现扩散和重分布,并逐渐向土体下部传递,使得土体中整体的应力分布更加均匀;同时,横-竖筋材中的竖筋类似于一个侧壁,其提供的垂直侧向力约束了介于竖筋间的土体,限制了土体的侧向水平位移,使得地基中筋材上部土体的侧向水平位移变小。基于有限元模拟对横-竖立体加筋地基加固机制的认识,将横-竖立体筋视为作用在地基上的一维弹性地基梁,通过弹性地基梁理论,根据弗拉曼解推导求解了横-竖立体加筋地基中任意一点竖向附加应力的计算表达式。将模型计算结果与有限元模拟所得结果进行对比发现两者吻合良好。  相似文献   

9.
The increasing importance of performance-based earthquake engineering analysis points out the necessity to assess quantitatively the risk of liquefaction of embankment-type structures. In this extreme scenario of soil liquefaction, devastating consequences are observed, e.g., excessive settlements, lateral spreading and slope instability. The present work discusses the global dynamic response and interaction of an earth structure-foundation system, so as to determine quantitatively the collapse mechanism due to foundation’s soil liquefaction. A levee-foundation system is simulated, and the influence of characteristics of input ground motion, as well as of the position of liquefied layer on the liquefaction-induced failure, is evaluated. For the current levee model, its induced damage level (i.e., induced crest settlements) is strongly related to both liquefaction apparition and dissipation of excess pore water pressure on the foundation. The respective role of input ground motion characteristics is a key component for soil liquefaction apparition, as long duration of mainshock can lead to important nonlinearity and extended soil liquefaction. A circular collapse surface is generated inside the liquefied region and extends toward the crest in both sides of the levee. Even so, when the liquefied layer is situated in depth, no significant effect on the levee response is found. This research work provides a reference case study for seismic assessment of embankment-type structures subjected to earthquake and proposes a high-performance computational framework accessible to engineers.  相似文献   

10.
汶川8.0级地震液化震害及特征   总被引:3,自引:1,他引:2  
通过现场详细地调查,归纳总结了汶川地震液化导致的工程震害的现象、分布、规律和特征。结果表明,此次地震液化震害现象显著,位于德阳地区的3个液化区域震害严重,都江堰地区、绵阳游仙区以及江油市区的3个液化区域震害中等,其他地区轻微,液化震害分布与液化分布有一定关系,但二者有所不同;液化场地上房屋均不同程度受损,其中结构性差的房屋会直接倒塌,设有圈梁、构造柱的房屋,液化也会导致其整体倾斜、下沉、开裂;学校液化震害具有典型性,部分校区大面积液化,地裂缝纵横,地基不均匀沉降严重,主体结构开裂、倾斜,功能丧失。这次液化震害具有3个显著特征:(1)只要液化出现的地方,震害均比周围重,没有减震现象;(2)Ⅵ度区不仅有液化现象,而且有明显的液化震害;(3)液化伴随地裂缝,是构成此次地震液化震害的主因。  相似文献   

11.
The results of centrifuge modeling of surface footings on a sand layer underlain by a rigid base are presented. The primary objective was to investigate the effect of sand layer thickness on the ultimate bearing capacity. The relative density of the sand layer and shapes of the model footings were also varied in the test program. The data indicate that prototype size footings are likely to experience local shear failure rather than general shear type failure. The observed values of the bearing capacity are compared with the predictions based on the Mandel and Salencon (1972) theory. It is concluded that theoretical predictions are conservative in relation to the experimental bearing capacity values, if appropriate values of mobilized angles of friction are used. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献   

12.
王家全  张亮亮  刘政权  周圆兀 《岩土力学》2018,39(10):3539-3547
为了研究土工格栅加筋砂土地基在动力荷载作用下的受力变形特性,利用自行设计的300 cm×160 cm×200 cm(长×宽×高)大比例地基模型试验装置,分别针对纯砂地基、土工格栅加筋地基进行了静动荷载破坏试验。分析地基承载力及基础沉降、地基土压力、动力加速度响应、土工格栅应变等参数变化规律,揭示了动力荷载作用下加筋砂土地基的承载力和变形特征,并对比分析静、动荷载对加筋地基承载性能的影响。试验结果表明,与纯砂地基相比,格栅单层加筋地基的承载力提高1.12倍,地基基础中轴线处沉降量减少24%,加筋土体的抗变形能力得到很大提高;加筋作用改变了地基的破坏模式,动载作用下纯砂地基为冲剪破坏而加筋地基为整体剪切破坏;筋材的存在对地基土压力及加速度峰值分别有明显的扩散作用和衰减作用,可有效降低在动力载荷下筋土的瞬态变形。  相似文献   

13.
王志云  王忠涛  栾茂田  王栋 《岩土力学》2008,29(6):1545-1550
作为新型的深水海洋基础型式,吸力式沉箱基础被广泛地用于系泊深水海洋设施中,从而承受巨大的倾斜上拔荷载。在上拔荷载水平分量与竖向分量的共同作用下,吸力式沉箱的承载特性及其工作性能评价是海洋工程设计与建设中的关键技术问题之一。然而现有的理论分析与试验研究并不能满足工程实践的需要,因此,对吸力式沉箱基础的极限承载力分析建立了有限元数值计算方法。当沉箱基础在快速拔出过程中,正常固结黏土处于完全不排水状态,沉箱基础发生整体破坏时表现出反向地基承载力失稳模式,此时沉箱基础所发挥的极限承载能力往往最大。为此,在数值计算中直接假定沉箱基础及其周围土体处于完全不排水状态,针对不同的沉箱长径比,分别确定了在竖向上拔荷载和水平拉拔的单独作用下沉箱基础极限承载力。对比发现:竖向上拔极限承载力有限元解能够较好地与理论计算结果相符合,而水平极限承载力解与理论计算结果存在一定的差异。  相似文献   

14.
断层、滑坡、液化等地质灾害引起的场地大变形对埋地管道结构安全产生严重的威胁。开展了中密砂中埋地管道−砂土水平横向相互作用的系列三维数值模拟,根据数值模拟的结果探讨了不同深径比下管−砂土横向相互作用时土体的破坏模式,研究了深径比对砂土极限承载力的影响。基于管周土体的破坏模式建立了简化计算模型,根据极限平衡理论推导了管道水平横向运动时砂土极限承载力计算公式。研究结果表明:极限状态下,浅埋管道周围土体形成延伸到地表的破裂面,轮廓线近似对数螺线;砂土的极限承载力随着深径比增加,最终在临界深径比处达到稳定;随着深径比的增加,土体发生剪切滑动破坏所需的管道位移也逐渐增大;由于横向承载力系数取值依据不同,国内外规范计算所得土体极限承载力差异较大;得到的解析解能够较好地预测中密砂土中浅埋管道水平横向运动时土体的极限承载力。  相似文献   

15.
Rock masses are commonly used as the underlying layer of important structures such as bridges, dams and transportation constructions. The success of a foundation design for such structures mainly depends on the accuracy of estimating the bearing capacity of rock beneath them. Several traditional numerical approaches are proposed for the estimation of the bearing capacity of foundations resting on rock masses to avoid performing elaborate and expensive experimental studies. Despite this fact, there still exists a serious need to develop more robust predictive models. This paper proposes new nonlinear prediction models for the ultimate bearing capacity of shallow foundations resting on non-fractured rock masses using a novel evolutionary computational approach, called linear genetic programming. A comprehensive set of rock socket, centrifuge rock socket, plate load and large-scaled footing load test results is used to develop the models. In order to verify the validity of the models, the sensitivity analysis is conducted and discussed. The results indicate that the proposed models accurately characterize the bearing capacity of shallow foundations. The correlation coefficients between the experimental and predicted bearing capacity values are equal to 0.95 and 0.96 for the best LGP models. Moreover, the derived models reach a notably better prediction performance than the traditional equations.  相似文献   

16.
周恩全  朱晓冬  陆建飞  王炳辉 《岩土力学》2018,39(12):4698-4706
为研究液化砂土的流动变形特征,开展了液化砂土的流体特性试验研究。基于边界层理论研发一套液化砂土表观黏度测试装置,主要由调速电机、电机调速器、圆柱转子、扭矩传感器等部分组成,该装置能有效测试液化砂土的表观黏度;开展了不同孔压比、转速下饱和砂土表观黏度及圆柱转子所受摩擦力矩特性研究,着重分析了液化后砂土的表观黏度特性。结果表明,液化前孔压发展及液化后孔压消散阶段摩擦力矩均受到孔压比及转速的影响;液化后砂土孔压逐渐消散,强度恢复,流动能力衰减,表观黏度升高,表观黏度与孔压比呈现出一定的线性相关性;表观黏度随着剪应变率的增大而降低,且两者呈现出幂函数关系,表明液化后砂土具有典型幂律型剪切稀化非牛顿流体特征。  相似文献   

17.
砂土液化导致的地基侧向大变形是地震中许多重要的工程设施和建筑物破坏的主要原因之一。简要介绍了可进行液化大变形分析的散粒体材料本构模型--应变空间多机构CG模型,基于FLIP ROSE程序平台,建立了预测和研究倾斜地基砂土液化导致侧向大变形的二维有限元数值分析方法。采用该模型对相同工况的土工动态离心模型试验进行了模拟,通过对比超孔隙水压力、剪切波水平加速度以及地基侧向位移发现,数值预测与试验结果吻合良好,从而验证了该有限元数值分析模型的可靠性。最后利用该数值分析模型预测了倾斜率不同的地基受到相同剪切波作用时,倾斜地基不同深度产生的侧向位移。预测结果显示,随着地基深度的减小,倾斜率对于地震液化导致倾斜地基侧向大变形的影响越来越显著。  相似文献   

18.
石佳颖  郝雅萍 《江苏地质》2023,47(2):225-230
确保地震荷载作用下海床场地的动力稳定性是海洋工程全寿命周期安全运行的重要保证,然而对复杂海域环境下饱和粉细砂的液化特性研究尚属少见。基于海域场地动应力计算方法,确定各试验工况的场地循环应力比CSR,并对试样施加与之对应的不排水循环荷载。试验结果表明:可液化的海洋粉细砂在考虑其场地动应力条件的循环荷载作用下出现不同的液化可能性;粉细砂呈循环破坏模式,将双幅轴向应变>5%作为循环破坏标准;海洋粉细砂的液化可能性与土体的埋深及动应力均不呈单一相关性,而是随着干密度的增大,液化振次逐渐增大,当干密度>1.72 g/cm3时土体不再液化。该结果可为杭州湾区抗震区划及海洋工程结构抗震设计提供参考。  相似文献   

19.
In this paper, liquefied and laterally spreading soils triggered by seismic shaking are modeled as viscoplastic Bingham media characterized by two rheological parameters: the undrained residual shear strength and the Bingham viscosity coefficient. Since the precise evaluation of these two characteristics directly by appropriate in situ or laboratory experimental tests remains a very difficult task, an identification procedure is developed to assign numerically realistic values to both rheological characteristics from back-calculation of liquefaction-induced lateral spreading using centrifuge experiments. The proposed numerical procedure is applied successfully to two series of reported centrifuge tests where lateral displacements data during shaking were available.  相似文献   

20.
As a part of the seismic safety evaluation of several bridges and other hydraulic structures located on Kasai River bed in India, the liquefaction potential of Kasai River sand is studied in 1-g shake table in laboratory and numerically using a commercial software FLAC 2D. The surface settlement, lateral spreading, predominant frequency, amplification of the ground motion and pore water pressure development in Kasai River sand in dry and liquefied states have been studied when subjected to sinusoidal motions of amplitude 0.35 g at a frequency of 2 Hz. The nonlinear curves used to represent shear strain dependency of stiffness and damping ratio of Kasai River sand are obtained from cyclic triaxial tests. Reasonably good agreement between the experimental and the numerical results is observed. It is found that the settlement and lateral spreading for the liquefied sand is 2.60 and 2.50 times than those of the sand in the dry state. The volumetric strain of the liquefied sand is found to be around 4%, which is significantly higher than 1.53% observed in the dry sand. It is observed that the amplification of the peak ground acceleration for the saturated sand is 1.08 and 1.32 times higher than that for the dry sand from theoretical and experimental results, respectively. The shear strain developed in the liquefied sand is 1.17 times more than that for dry sand. The fundamental and higher modal frequencies of dry sand are found to be 1.13, 1.117 and 1.119 times more than those for the saturated sand, respectively.  相似文献   

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