圆钢管高强混凝土轴压短柱承载力有限元分析

应用Open SEES有限元软件计算圆钢管混凝土短柱的轴压承载力-应变关系曲线。由于钢管和混凝土之间相互作用的机理,分别采用Mander混凝土本构模型和根据套箍系数修正Mander混凝土本构模型,计算结果与实验结果吻合较好。应用此材料本构模拟圆钢管高强混凝土短柱并讨论不同参数的影响。结果表明:基于试验的Open SEES建模方式与模型参数选取合理;圆钢管高强混凝土与普通混凝土的力学性能差异大;增大核心混凝土的强度、钢材的套箍系数和屈服强度都可以提高构件的极限承载力。     

非均质软基上桶形基础承载性能有限元分析

作为海洋平台的基础部分,桶形基础不仅承受海洋平台结构及自身重量等竖向荷载的长期作用,而且往往还遭受波浪等所产生的水平荷载及力矩等其它荷载分量的作用。因此,确定软基上桶形基础在竖向荷载（V）、水平荷载（H）和力矩（M）等共同作用下的承载特性,建立其在复合加载模式下的破坏包络面,并进而依此评价海洋平台基础及地基的稳定性,是桶形基础设计与施工中的关键问题。在大型通用有限元分析软件ABAQUS平台上,采用基于Mises屈服准则的完全弹塑性本构模型,对横观各向异性软基上桶形基础的承载性能进行了三维弹塑性数值分析,探讨了软黏土不排水抗剪强度的各向异性对单个荷载和复合加载作用下桶形基础承载性能的影响。     

应用OpenSEES模拟方钢管混凝土柱的抗震性能

应用OpenSEES有限元软件计算方钢管混凝土柱的水平力-位移滞回曲线。考虑到钢管与混凝土相互作用的机理,采用Mander混凝土本构模型,计算结果与试验结果吻合较好。在此基础上对方钢管混凝土柱进行了参数分析,讨论了纤维模型数量、单元划分数量和材料本构等因素的影响。结果表明:基于OpenSEES建模方式与模型参数选取合理;增大钢材屈服强度,可以提高方钢管混凝土柱水平承载力,混凝土强度对方钢管混凝土柱的水平承载力影响则不大。     

上海软土地震响应的振动台模型试验及其三维数值拟合分析

对上海典型软土地铁车站结构振动台模型中的自由场振动台模型试验建立了三维计算模型,包括计算范围的确定,材料本构模型的选取,动力边界条件的选用以及地震波的输入等4个方面.用该模型对自由场振动台模型试验进行了三维的拟合分析,并将计算结果与实测结果以及二维拟合分析结果进行了比较分析,表明三者吻合较好.说明该计算模型可用来模拟模型土的动力特性,可为建立上海软土三维地震响应的计算方法提供基础.     

防屈曲支撑的有限元模拟及滞回性能分析

结合防屈曲支撑拟静力实验的研究成果,本文采用有限元软件ABAQU S对其进行了数值模拟分析。在模拟过程中,应用金属Com b ine本构模型设置内芯钢板材料属性。该模型是对传统双线性本构模型的改进,模拟结果很好地符合了实验结果,同时验证了防屈曲支撑具有良好的减震耗能性能,其在轴向加载达到7倍屈服位移时,依然能保持良好的滞回特性。通过对模型中橡胶无粘结层的合理设置,研究了内芯钢板在失稳变形中无摩擦滑移与能量缓冲转化的形变特点。分析表明,当外包约束强度和刚度足够时,内芯钢板在受轴向压力时只发生多波微幅弯曲失稳;随着内芯钢材与外包有效约束间隙的增大,支撑的失稳波幅也随之增大,支撑承载力与耗能能力显著降低。     

岩石塑性变形条件下的Mohr-Coulomb屈服准则

传统的Mohr-Coulomb强度准则仅描述了峰值强度状态下正应力和剪应力之间的关系,作为岩石破坏的判据.本文拓展概念,提出Mohr-Coulomb屈服准则表述岩石发生塑性变形后不同应力状态下屈服面的应力应变关系.在总结实验研究的基础上建立了使用三轴压缩试验数据确定塑性参数c和φ随内变量κ变化的实验技术方法,给出了评价各向同性模型精度的参量表达以及某些测试结果.采用具有各向同性强(软)化规律的Mohr-Coulomb屈服准则,利用岩石的初始屈服、峰值屈服和残余屈服三组参数可以将全过程应力应变曲线简化表征为四直线模型,它比三线性模型有更广泛的适用性.本文的结果为工程地质数值模拟提供了理论和实验基础,具有指导意义.     

横观各向同性岩土材料的应变局部化分析

为分析横观各向同性岩土材料的应变局部化行为,推导对应于Lade横观各向同性屈服准则向前欧拉算法的迭代格式及本构矩阵,通过有限元软件ABAQUS的UMAT接口实现相应的程序代码。数值算例调查分析材料主方向对横观各向同性岩土结构的极限承载力和变形局部化模式的影响。结果表明该模型能较好地模拟横观各向同性岩土结构的应变局部化行为。     

钢筋混凝土筒体的非线性有限元分析模型

本文提出了一种反复荷载下混凝土材料的本构模型，该模型采用平面应力状态下的弥散正交裂缝假设，钢筋采用弥散假设，并考虑了屈服、应变硬化、循环卸载与再加载规则等因素。该本构模型与其他模型相比，具有简便有效的优点。在此基础上，本文采用八结点平面应力单元建立了钢筋混凝土核心筒体非线性有限元分析模型，并对试验模型进行了非线性分析，计算结果与试验结果吻合较好。     

砂土液化大变形本构模型及在ABAQUS软件上的实现

基于Yang和E lgam al等人提出的砂土液化大变形本构模型,对该模型的建立过程进行了详细的推导,基于新的嵌套屈服面硬化规则,对原有模型的硬化规则的不连续性做了改进,把该本构模型扩展应用到三维液化大变形的数值分析中,实现了基于ABAQUS大型商用软件计算平台上砂土液化大变形的计算子程序的开发,基于该计算平台和开发的本构模型,对动三轴试验体系中砂土试样的液化过程进行了数值试验分析,给出了试验过程中试样的竖向动位移、整体竖向应力应变关系滞回曲线和动孔压时程曲线的数值计算结果。文中初步验证了该模型在ABAQUS上开发的子程序的可靠性和数值计算模型的可行性,模型的可靠性及其子程序的稳定性还需通过试验结果和数值计算结果的对比分析与进一步验证。     

钢筋混凝土框架结构震后可存活概率预测方法研究

针对当前钢筋混凝土震后存活预测相关方法存在预测值与实际值拟合度低的问题,提出基于有限元的钢筋混凝土框架结构震后可存活概率预测方法。利用混凝土本构模型关联数值和钢筋本构模型数值计算,实现钢筋混凝土框架材料本构模型关联数值分析。结合建筑和结构施工图实现钢筋混凝土有限元模拟,将钢筋混凝土框架有限元模型的最大竖向荷载作为结构整体构造竖向极限承载力,并引入随机Pushdown方法及随机竖向IDA法得到钢筋混凝土框架震后可存活概率。经实验证明,将有限元应用至钢筋混凝土框架结构震后可存活概率预测中切实可行;预测值与实际值拟合度高于目前常用方法。所提方法的性能完善,可为该领域发展提供可借鉴的信息。     

SEDIMENT YIELD MODELING FOR SINGLE STORM EVENTS BASED ON HEAVY-DISCHARGE STAGE CHARACTERIZED BY STABLE SEDIMENT CONCENTRATION

The relation between runoff volume and sediment yield for individual events in a given watershed receives little attention compared to the relation between water discharge and sediment yield, though it may underlie the event-based sediment-yield model for large-size watershed. The data observed at 12 experimental subwatersheds in the Dalihe river watershed in hilly areas of Loess Plateau, North China, was selected to develop and validate the relation. The peak flow is often considered as an important factor affecting event sediment yield. However, in the study areas, sediment concentration remains relatively constant when water discharge exceeds a certain critical value, implying that the heavier flow is not accompanied with the higher sediment transport capacity. Hence, only the runoff volume factor was considered in the sediment-yield model. As both the total sediment and runoff discharge were largely produced during the heavy-discharge stage, and the sediment concentration was negligibly variable during this stage, a proportional function can be used to model the relation between event runoff volume and sediment yield for a given subwatershed. The applicability of this model at larger spatial scales was also discussed, and it was found that for the Yaoxinzhuang station at the Puhe River basin, which controls a drainage area of 2264km2, a directly proportional relation between event runoff volume and sediment yield may also exist.     

A Simple Relation to Constrain Groundwater Models Using Surface Deformation

A simple relation between pore pressure change and one-dimensional surface deformation is presented. The relation is for pore pressure change in a confined aquifer that causes surface deformation. It can be applied to groundwater models of any discretization and is computationally efficient. The estimated surface deformation from model results can be compared to observed surface deformation through geodetic techniques such as Differential Interferometric Synthetic Aperture Radar. Model parameters then are constrained using the observed surface deformation. The validity of this relation is shown through constraint of model parameters for surface uplift due to pore pressure increase caused by wastewater disposal injection.     

地震强度分布不均匀性的摩擦时间依从CA模型

设计一个摩擦时间依从的地震活动性细胞自动机模型（CA），研究产生地震累积频度-震级关系曲线中，出现拐点的地震强度分布不均匀现象的物理原因。外界通过应力加载向模型输入能量，模型的细胞之间存在非线性的相互作用。对比分析规定单个细胞破裂与模型地震之间不同的决定规则时产生的地震序列的累积频度-震级关系，研究结果表明，地震的级联破裂方式是引起累积频度-震级关系在震级较低范围和震级较高范围之间不连续的因素之一。     

基于分数阶时间导数常Q黏弹本构关系的含黏滞流体双相VTI介质中波场数值模拟

分数阶微分算子具有描述历史依赖性和全域相关性的特质,本文利用这种特质描述双相介质固体骨架的黏弹性特征.基于Kjartansson常Q理论将含有分数阶时间导数的黏弹固体骨架各向异性本构关系与双相介质理论有机地结合起来,并引入流变学本构关系描述孔隙流体的黏滞性力学行为,提出一种新的基于分数阶时间导数常Q黏弹本构关系的含黏滞流体双相VTI模型.推导了相应的时间域波传播方程,然后对该方程进行了数值模拟.对整数阶导数采用高阶交错网格有限差分算法,对分数阶时间导数采用短时记忆中心差分算法,进行了不同相界、不同品质因子组及双层地质结构情况下该类介质中波场的数值模拟与特征分析.模拟结果表明：将含有分数阶时间导数的常Q黏弹固体骨架各向异性本构关系及孔隙流体的黏滞性本构关系引入双相介质理论是可行的,二者的结合能更好地反映地下介质的黏弹性特征,对于进一步认识波在黏弹各向异性孔隙介质中的传播机理具有重要意义,为反演和重构地下油气储层和结构奠定正演理论基础.     

Estimating suspended sediment concentrations in areas with limited hydrological data using a mixed‐effects model

Sediment rating curves are commonly used to estimate the suspended sediment load in rivers and streams under the assumption of a constant relation between discharge (Q) and suspended sediment concentrations (SSC) over time. However, temporal variation in the sediment supply of a watershed results in shifts in this relation by increasing variability and by introducing nonlinearities in the form of hysteresis or a path‐dependent relation. In this study, we used a mixed‐effects linear model to estimate an average SSC–Q relation for different periods of time within the hydrologic cycle while accounting for seasonality and hysteresis. We tested the performance of the mixed‐effects model against the standard rating curve, represented by a generalized least squares regression, by comparing observed and predicted sediment loads for a test case on the Chilliwack River, British Columbia, Canada. In our analyses, the mixed‐effects model reflected more accurate patterns of interpolated SSC from Q data than the rating curve, especially for the low‐flow summer months when the SSC–Q relation is less clear. Akaike information criterion scores were lower for the mixed‐effects model than for the standard model, and the mixed‐effects model explained nearly twice as much variance as the standard model (52% vs 27%). The improved performance was achieved by accounting for variability in the SSC–Q relation within each month and across years for the same month using fixed and random effects, respectively, a characteristic disregarded in the sediment rating curve. Copyright © 2012 John Wiley & Sons, Ltd.     

钢筋混凝土柱考虑损伤累积的反复荷载-位移关系分析

为能在反复荷载作用下钢筋混凝土柱的荷载-位移关系分析中考虑柱低周疲劳性能,提出了一损伤模型,对柱中纵向受力钢筋和混凝土的损伤状态作评估与记录。将这一记录材料性能信息的损伤指标带入材料各自的恢复力模型以考虑产生损伤后材料的强度和刚度退化。基于多弹簧模型对不同变幅加载路径下及等幅低周疲劳加载下钢筋混凝土柱的空间反应进行了数值计算模拟。与已有试验结果比较表明,所提材料层次上的损伤累积模型以及考虑损伤累积效应的柱构件空间荷载-位移关系分析方法具有一定的精度,为钢筋混凝土柱的抗震性能分析提供了一个辅助工具。     

Power-laws and applications to earthquake populations

In this paper we study the rooted tree model applying the concepts of probability to obtain results of importance in understanding power-law distributions in pure populations and also in an ensemble of pure populations. The well-known Gutenberg-Richter relation, which is an empirical relation providing the number of earthquakes whose magnitude exceeds a given value, is shown to be an asymptotic form of survivor function of earthquake magnitudes. The implications of this model are briefly discussed in relation to other branches of sciences where power-law distributions are encountered.     

Study of main body element of crustal strain and its relationship with moderate-strong earthquakes

In this paper, progress in strain study of blocks and faults by GPS data are discussed, and the concept that active structures between blocks are the main body of crustal strain is clarified. By energy transfer principle of elastic mechanics, the relation between strain around faults and tectonic force on fault surfaces is set up and main body element model of crustal strain is constructed. Finally, the relation between mechanical evolution of model and seismogenic process of Kunlun earthquake （Ms=8.1） is discussed by continuous GPS data of datum stations. The result suggests that the relatively relaxed change under background of strong compressing and shearing may help to trigger moderate-strong earthquakes.     

应用全张量重力梯度数据优化密度和速度模型

重力梯度全张量数据具有高灵敏度反映探测目标局部微弱变化的特点,可以对单一地震数据在建立速度模型过程中的不确定性,尤其是各向异性速度模型建立过程中的精细结构进行补充修正.本文主要研究重震两类数据与各自所反映的物理模型关系以及密度模型与速度模型之间的相互联系和制约关系,从而建立重力全张量数据与地震速度模型间的信息互补关系和模型参数间的解析表达式.在此基础上,提出多参数加权正反演算法流程,逐层异常分离技术和约束条件下迭代反演模型修正方法,并实现模块编程和验证.实验数据和结果表明,重力全张量数据和地震数据多参数融合能够明显提高地震速度建模精度,减小模型解释的不确定性.     

Constraints imposed on crustal heat production by the linear heat flow relation

The class of three-dimensional radiogenic heat source functions, which satisfy a linear relation between heat flow and surface heat production, is constructed by expanding the source in terms of Fourier transforms in the horizontal directions and Laguerre functions in the vertical. The linear relation then becomes a set of linear equations among the expansion coefficients. In particular, it is shown that the preferred exponential decay model can only hold if heat flow is constant at the Earth's surface. Furthermore, if a heat source function has any lateral variation, then the linear relation cannot survive erosion of any uniformly thick slab. For a given heat flow data set, construction of a source solution, closest in the mean-square sense to the exponential decay model, is demonstrated. When applied to a heat flow data set from central England, the construction gives vertical profiles which locally show significant departures from the exponential model.