共查询到20条相似文献，搜索用时 156 毫秒
1.
采用ABAQUS建立12层剪力墙结构的有限元模型，利用该结构1/5缩尺模型振动台试验时预留试块的材性试验结果及相似关系，确定相应原型结构材料的性能参数，将试验参数和我国混凝土结构设计规范给出的混凝土单轴受拉/压应力-应变关系曲线相结合，确定ABAQUS模型中混凝土损伤塑性模型所需的应力-应变参数；将试验参数和张劲公式法相结合，确定ABAQUS模型中混凝土损伤塑性模型所需的损伤因子参数。对比有限元分析结果和振动台试验结果，验证参数设置的有效性。ABAQUS有限元分析和振动台试验所得原型结构前三阶振型和自振周期相差很小，说明ABAQUS模型和参数设置能够反映并用于计算实际结构的弹性响应。ABAQUS有限元分析得到的结构损伤情况与试验模型的损伤情况基本一致；结构的顶点加速度曲线和滞回曲线等响应的有限元分析结果与试验结果在多遇地震作用下基本吻合，但由于振动台试验累积损伤的影响，两者的差异随着地震波幅值的增大而逐渐增大；ABAQUS有限元分析得到的位移包络曲线与剪力墙结构弯曲变形的特点相符。以上弹塑性分析结果进一步表明了ABAQUS模型和参数设置能够很好地模拟结构在地震作用下的响应。 相似文献
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波浪荷载能引起海床土体的主应力轴连续旋转。不同于地震、交通等循环荷载,在周期性波浪荷载作用的土体应力路径方式下,软黏土的软化效用更为明显。本文分别对天然和扰动的海床土体在波浪荷载作用下的应力响应进行模拟,并分析应力路径的特点;为描述软化后的应力-应变关系,将软化效用和累积塑性应变的参数引入到能够反应土体动力非线性的Hardin-Drnevich模型中,建立修正模型,使之能够反应软黏土体软化与塑性应变累计特性;通过与模拟波浪荷载下土体应力特征的循环耦合试验结果进行对比分析,验证该修正模型的可靠性。 相似文献
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抗震性能是建筑设计中的一项重要指标,需要对地震作用下的建筑结构动力弹塑性损伤情况进行分析。提出一种中强地震下建筑结构动力弹塑性损伤模型研究方法。从有效应力与Cauchy应力张量\,建筑材料损伤演化方程等方面对弹塑性损伤模型基本原理进行分析,以此为理论基础,分析建筑材料应变率与建筑结构损伤能释放率的相关关系,通过Bonora损伤模型获取失效建筑材料损伤指数,并计算整体建筑结构构件损伤指数,以建筑材料损伤指数和建筑结构构件损伤指数为依据,完成中强地震下的建筑结构动力弹塑性损伤模型构建。利用实例进行分析,地震加速度值为0.3g的情况下,该模型的建筑结构相对位移时程曲线与实际位移曲线拟合度较高,且具有较好的建筑结构动力弹塑性损伤模拟精度,表明该模型具有一定的可行性。 相似文献
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动力本构模型UE模型具有可以描述非对称循环荷载、记忆量小、模型参数物理意义明确、表达式简单等优点。但其描述等幅循环荷载作用下的土体滞回圈时,存在非对称性,并且无法较好地拟合土体动阻尼比随应变产生的变化规律。通过在UE模型的骨架曲线中引入两个瞬变参数,利用“massing二倍法”构造滞回曲线,使模型同时满足各个应变下的剪切模量及阻尼比,确定瞬变参数的表达式,将瞬变参数表达式带入滞回曲线方程中,即得到最终的滞回曲线表达式,并定义各个滞回圈顶点的连线为此修正模型的实际骨架曲线。分析结果表明,该修正模型能够克服UE模型存在的不足,且更符合实际。 相似文献
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基于可靠度的结构损伤性能设计 总被引：4，自引：0，他引：4
本文基于现行抗震规范设计方法，运用荷载抗力分项系数法对结构损伤可靠度进行了研究。选择了恰当的地震动随机过程模型。合理地确定了模型参数。利用现有的钢筋混凝土构件的损伤模型。应用响应面法拟合目标函数，提出了钢筋混弹簧土结构损伤可靠度的分项系数标定方法，根据试验经验公式并结合截面应力应变分析。确定了钢筋混凝土截面恢复力模型参数，应用MonteCarlo方法对结构的可靠度进行计算。编制了钢筋混凝土结构的损伤可靠度计算程序，采用重要抽样法计算结构的可靠度，提高了计算效率，计算了现行抗震规范的结构损伤可靠度，确定了分项系数和目标失效概率的关系。为现行规范向性能设计规范的过度提供了可靠度基础。 相似文献
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邓肯E-B模型无法描述软化土体的应力应变关系以及土体的剪胀效应；采用抛物线型体应变曲线的南水模型破坏时的剪胀率趋于定值，与实际土体不符。但南水模型适合描述应力应变峰值点前或最大剪胀率前土体的本构关系，邓肯模型适合描述的应变范围更小。因此，若要进行土工结构渐进破坏的分析计算，则需要建立一个适合于描述直至破坏的更大应变范围的土体本构关系。采用损伤扰动概念，将变形过程中的土体视为“相对完整”的未损伤土体和“完全调整”扰动土体的混合体，其应力应变关系可根据损伤扰动程度，由各自的应力应变关系组合确定。并根据试验提出了确定损伤扰动函数的计算公式。对体应变曲线，则采用抛物线加双曲线的形式加以描述。 相似文献
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基于振动台试验的RC框架模型修正及模拟损伤识别 总被引：1，自引：0，他引：1
利用有限元模型修正技术综合利用理论建模和实验建模的优点,可以得到更加符合结构实际的基准模型,为结构动力分析、损伤诊断及健康监测提供更可靠的依据。基于一12层钢筋混凝土框架模型振动台试验测点加速度记录,采用特征系统实现算法对该模型结构进行模态参数识别,识别结果与有限元分析结果之间存在明显的差异。采用基于灵敏度分析的参数型有限元模型修正技术,选择识别精度较高的实测模态频率为修正基准,以构件的弹性模量和密度为修正参数,对该框架的初始有限元模型进行了修正,得到基准有限元模型。进一步以基准有限元模型为标准,以构件弹性模量的降低模拟结构的损伤,对两种假设工况下的损伤结构进行修正,得到构件弹性模量的变化值并与假设的降低值对比,验证了有限元模型修正技术在结构损伤识别中应用的可行性。 相似文献
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本文采用自主编写的光滑粒子流体动力学法程序,在平面应变单轴压缩条件下,开展了非均质岩石试样破坏过程中剪切带、声发射数及应变能释放量的演变规律研究,探讨了形状参数和Weibull分布函数的定位参数的影响,而过去的研究更多地关注形状参数的影响.仅粒子的黏聚力被认为服从Weibull分布.当粒子破坏后,粒子的黏聚力跌落至残余值,在此过程中,最大主应力(即第3主应力)保持不变.得到了下列结果.随着定位参数的增加,破坏粒子的分布由弥散向集中转变,岩样的纵向应力峰值增加.每20个时步数目的全局最大声发射数和全局最大应变能释放量均发生在峰后应力迅速跌落过程中,与二者有关的8个量随形状参数或定位参数的演变规律较为复杂,这应与岩样破坏形态的多样性有关. 相似文献
9.
浙北及邻近地区应力场数值模拟与地震危险区预测 总被引：4，自引：0，他引：4
根据构造地质学、地震地质学的考察和观测结果,结合构造单元、地震活动分区和研究区位置确定计算模型的范围,选定一个构造骨架,确定计算模型的边界形状和几何参数。然后参考地震震源机制解结果和新构造运动特征,选定模型边界条件,参考岩石力学实验结果,确定模型的物理参数,最后利用线弹性二维有限元程度计算了各节点位移、各单元应力应变及应变能增量。通过分析应用应场和应变能增量划分出２个地震危险区。 相似文献
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This paper reports an experimental study of the evolution of permeability during rock brittle failure and a theoretical analysis of rock critical stress level. It is assumed that the rock is a strain-softening medium whose strength can be described by Weibull’s distribution. Based on the two-dimensional renormalization group theory, it is found that the stress level λc (the ratio of the stress at the critical point to the peak stress) depends mainly on the homogeneity index or shape parameter m in the Weibull’s distribution for the rock. Experimental results show that the evolution of permeability is closely related to rock deformation stages: the permeability has a rapid increase with the growth of cracks and their surface areas (i.e., onset of fracture coalescence point), and reaches the maximum at rock failure. Both the experimental and analytical results show that this point of rapid increase in permeability on the permeability-pressure curve corresponds to the critical point on the stress-strain curve; for rock compression, the stress at this point is approximately 80% of the peak strength. Thus, monitoring the evolution of permeability may provide a new means of identifying the critical point of rock brittle fracture. 相似文献
12.
基于能量耗散理论建立非均质岩石的动态损伤破坏元胞自动机,分析单轴压缩试验中岩石破坏截面的损伤状态,得到该情况下的岩石裂隙微观动态发展过程、损伤演化关系以及全程应力应变曲线。研究发现：①加载过程中,均质度较低的岩样裂纹的萌生和扩展较为分散,损伤速率低;均质度较高的岩样裂纹的萌生和扩展非常集中,表现为脆性破坏。②损伤演化曲线呈3阶段S形发展。③随着岩石均质度参数的增加,岩石的峰值强度和峰值应变都有所提高,峰后曲线越来越陡。④给出的衡量岩石脆性破坏强弱程度的指标参数,能够较好地描述岩石破坏形式随着均值度参数m变化的规律。 相似文献
13.
A constitutive model of rocks subjected to cyclic stress–temperature was proposed. Based on statistical damage theory, the damage constitutive model with Weibull distribution was extended. Influence of model parameters on the stress–strain curve for rock reloading after stress–temperature cycling was then discussed. The proposed model was initially validated by rock tests for cyclic stress–temperature and only cyclic stress. Finally, the total damage evolution induced by stress–temperature cycling and reloading after cycling was explored and discussed. The proposed constitutive model is reasonable and applicable, describing well the stress–strain relationship during stress–temperature cycles and providing a good fit to the test results. Elastic modulus in the reference state and the damage induced by cycling affect the shape of reloading stress–strain curve. Total damage induced by cycling and reloading after cycling exhibits three stages: initial slow increase, mid-term accelerated increase, and final slow increase. 相似文献
14.
岩石塑性变形条件下的Mohr-Coulomb屈服准则 总被引：4，自引：0，他引：4
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. 相似文献
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In order to investigate the dynamic mechanical properties of amphibolite and sericite-quartz schist under confi ning pressure, two rocks are subjected to impact loadings with different strain rates and confi ning pressures by using split Hopkinson pressure bar equipment with a confi ning pressure device. Based on the experimental results, the stress-strain curves are analyzed and the effects of confi ning pressure and strain rates on the dynamic compressive strength, peak strain and failure mode are summarized. The results show that:(1) The characteristics of two rocks in the ascent stage of the stressstrain curve are basically the same, but in the descent stage, the rocks gradually show plastic deformation characteristics as the confi ning pressure increases.(2) The dynamic compressive strength and peak strain of two rocks increase as the strain rate increases and the confi ning pressure effects are obvious.(3) Due to the effect of confi ning pressure, the normal stress on the damage surface of the rock increases correspondingly, the bearing capacity of the crack friction exceeds the material cohesion and the slippage of the fractured rock is controlled, which all lead to the compression and shear failure mode of rock. The theoretical analysis and experimental methods to study the dynamic failure mode and other related characteristics of rock are useful in developing standards for engineering practice. 相似文献
17.
This study presents a framework for numerical simulations based upon micromechanical parameters in modeling progressive failures
of heterogeneous rock specimens under compression. In our numerical simulations, a Weibull distribution of the strength and
elastic properties of the finite elements is assumed, and the associated Weibull parameters are estimated in terms of microstructural
properties, such as crack size distribution and grain size, through microscopic observations of microcracks. The main uncertainty
in this procedure lies on the fact that various ways can be used to formulate a ``microcrack size distribution' in relating
to the Weibull parameters. As one possible choice, the present study uses the number of counted cracks per unit scanned volume
per grain size to formulate the crack distributions. Finally, as a tool, the Rock Failure Process Analysis code (RFPA2D) is adopted for simulating the progressive failure and microseismicity of heterogeneous rocks by using an elastic-damage
finite-element approach. To verify our framework, compression tests on marble specimens are conducted, and the measured acoustic
emissions (AE) are compared with those predicted by the numerical simulations. The mode of failure, compressive strength and
AE pattern of our simulations basically agree with experimental observations. 相似文献
18.
基于断层面强度的非均匀性,将断层面的宏观破裂过程看作是断面局部微元的破裂累积过程,假设断层局部微元强度遵循Weibull概率分布,从统计力学角度推导出了宏观的断层载荷.变形的全过程本构关系.采用一维地震力学模型,以远场位移a为控制变量,用稳定性理论研究了地震不稳定性问题.研究表明,系统刚度比(围岩刚度与断层刚度之比)β是影响地震发生的重要参数,只有当β<1时才会出现地震失稳,且应力突跳发生在平衡路径曲线的位移转向点,并给出了地震过程的3个重要参数(地震后断层半错距、地震应力降和释放的弹性能)的表达式.当β≥1时,不会发生地震,仅是缓慢的断层滑动,属于无震滑动. 相似文献
19.
V. I. German 《Pure and Applied Geophysics》2006,163(10):2243-2258
A statistical model for describing the energy scaling of the distribution of inter-event times is described. By considering
the diverse region seismicity (natural and induced) on different scale (energy/magnitude) levels the self-similarity of the
distribution has been determined. A comparison between the distribution of inter-event times on different scale levels and
the most popular distributions of reliability theory has been carried out. The distribution of inter-event times for different
scale levels is well approximated by the Weibull distribution. The Weibull distribution, with parameters which obey the scaling
model and the Gutenberg-Richter law, has been tested. 相似文献
20.
A method to approach the stress-strain curve of frozen soil is presented based on the fact that the stressstrain curve of frozen soil has fractal property. First, a linear hyperbolic iterated function system (LHJB) in which the perpendicular contraction factors are regarded as parameters is established using fractal geometry theories. Secondly, a method to calculate the best point which makes the attractor of the LHIFS an optimal approximation of the stress-strain curve of frozen soil is presented. Then, a method for calculating the fractal dimension of the stress-strain curve of frozen soil is obtained. Finally, a simple example is provided. The method presented in this paper provides a new method for simulating the stress-strain curve and calculating its fractal dimension of geomaterials that have the fractal feature by using computer 相似文献