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991.
《Wave Motion》2017
A higher-order dispersive equation is introduced as a candidate for the governing equation of a field theory. A new class of solutions of the three-dimensional field equation are considered, which are not localized functions in the sense of the integrability of the square of the profile over an infinite domain. For this new class of solutions, the gradient and/or the Hessian/Laplacian are square integrable. In the linear limiting case, an analytical expression for the pseudolocalized solution is found and the method of variational approximation is applied to find the dynamics of the centers of the quasi-particles (QPs) corresponding to these solutions. A discrete Lagrangian can be derived due to the localization of the gradient and the Laplacian of the profile. The equations of motion of the QPs are derived from the discrete Lagrangian. The pseudomass (“wave mass”) of a QP is defined as well as the potential of interaction. The most important trait of the new QPs is that, at large distances, the force of attraction is proportional to the inverse square of the distance between the QPs. This can be considered analogous to the gravitational force in classical mechanics. 相似文献
992.
Sandwich beams under three-point bending containing cracks in the core material very close to the upper skin interface are investigated. The cracks considered parallel or with an imperceptible inclination to the longitudinal beam axis and at different distances from the upper skin interface, are analyzed with static non-linear elastic two and three dimensional finite element analyses. From the proposed analyses stress intensity factors are calculated using linear elastic fracture mechanics. It is demonstrated that the crack propagation on the compression side of the core is mainly subjected in shear. The strain energy density criterion is used in order to determine the angle of kinking of the crack into the core. 相似文献
993.
994.
The evolution of a propagating kink in a Sine-Gordon lattice is studied asymptotically using an averaged Lagrangian formulation appropriately coupled to the effect of the radiation. We find that unlike the continuum case the interaction with the Goldstone mode is important to explain the acceleration of the kink as it hops along the lattice. We develop a discrete WKB type solution to study the interaction of the kink and the radiation. In particular using this solution we show how to calculate the effect of the Peyrard and Kruskal resonant radiation in the energy loss of the kink. We obtain a set of modulation equation which explains qualitatively the evolution of the kink with remarkable quantitative agreement. 相似文献
995.
可侵蚀地表上方含尘大气运动的数值模型 总被引:2,自引:0,他引:2
在稀相气固两相流的双流体模型框架下,导出含尘大气运动的基本方程,其中的源项考虑相间双向耦合作用;通过对基本方程进行无量纲化,求得控制气相和弥散相动力学行为的相似准则,包括弗洛德数、罗斯贝数、颗粒雷诺数、颗粒惯性参数、颗粒剪切横移参数、颗粒旋转横移参数和沙尘质量载荷率等. 作为一个模型问题,研究可侵蚀地表上方充分发展湍流大气边界层流动对土壤颗粒的气动卷扬作用,其中计及气动阻力、萨弗曼升力和重力等因素的影响. 为了克服由于沙尘跃移运动轨迹交叉导致流动参数多值性所造成的困难,引进拉格朗日坐标下弥散相连续方程. 对两种不同风速和4种不同粒径条件下的沙尘运动进行数值模拟,给出相应情况中沙尘运动特性和密度分布剖面并讨论风速和粒径等参数的影响,还细致分析了含尘大气边界层中沙尘与气流之间的能量传递过程. 所得的方程、准则和方法可以为土壤风蚀和沙尘暴等自然灾害的预报提供理论基础. 相似文献
996.
利用欧拉-拉格朗日方法,提出了用于预测竖直管道内绝热层流泡状流中含气率分布的三维模型。该模型能够跟踪单独的气泡轨迹,从而获取更多的界面力信息;同时气泡尺寸可以作为参数之一引入模型,使含气率分布的计算更为方便。模型中分析了绝热层流泡状流中气泡的各项受力表达式,建立了两种描述方法下的气液两相间的耦合关系。利用现有实验数据对模型进行的检验表明,该模型能够预测一定尺寸范围内气泡的分布;气泡径向分布主要取决于气泡所受侧向提升力。对于更大尺寸的气泡,气泡变形和气泡尾迹与当地流场间相互作用将对侧向提升力产生很大影响。 相似文献
997.
锚固正交各向异性岩体的本构关系和破坏准则 总被引:8,自引:0,他引:8
从理论上对由系统锚杆加固的正交各向异性岩体,取出包含锚杆的表征单元.根据“等效材料”的概念,在原岩体的本构关系和破坏准则中计人锚杆刚度和强度的“贡献”,从而建立了相应锚固岩体的木构关系和破坏准则.然后列举算例,考察了表征单元的应力-应变关系和破坏强度随锚杆安置角度变化的各向异性表现.最后将计算与一个简单试验的结果作了对比,看到二者的吻合程度较好,因而初步地验证了所提力学模型的可靠性. 相似文献
998.
The effect of a thin isotropic coating on the edge effect zone in a representative element of a coated material is examined.
Isotropic and transversely isotropic materials are considered. The transversely isotropic material has the elastic properties
of unidirectional glass-fiber-reinforced plastic. The decay of the edge effect in the directions perpendicular to the coating
plane and to the plane of isotropy is studied. A boundary-value problem of elasticity for piecewise-homogeneouse orthotropic
bodies and a quantitative edge effect decay criterion for normal stresses are used as a design model. The problem is solved
using the finite-difference method and base schemes. The results of evaluation of the edge effect zone in homogeneous and
inhomogeneous materials are presented. It is shown that the presence of a thin isotropic coating blocks the edge effect, that
is, decreases the edge effect zone in both isotropic and transversely isotropic materials
__________
Translated from Prikladnaya Mekhanika, Vol. 43, No. 12, pp. 61–67, December 2007. 相似文献
999.
在连续介质力学基础上建立了一个广义双剪粘弹塑性海冰动力学本构模型。该模型在海冰屈服前采用Kelvin-Vogit粘弹性模型,考虑中间主应力和静水压力对海冰屈服的影响选用广义双剪应力屈服准则作为海冰屈服判据,屈服后采用相关联的正则流动法则。采用该本构模型对渤海海冰动力过程进行了48小时数值模拟,讨论了辽东湾海冰的厚度、密集度、冰速和主应力的分布规律,其中海冰厚度分布与卫星遥感资料符合良好,从而有效地验证了该广义双剪粘弹塑性本构模型在海冰动力学中的可靠性。 相似文献
1000.
G. Bertolino A. Constantinescu M. Ferjani P. Treiber 《Theoretical and Applied Fracture Mechanics》2007,48(2):140-151
The aim of this paper is to analyse the fatigue phenomena in the presence of stress gradients. It is well-known that most fatigue criteria fail to predict the lifetime of components in the presence of high stress concentrations or stress gradients, as it is the case in the neighbourhood of cracks, holes notches and encountered for example in riveted or threaded structures. Proposed is a numerical approach in the framework of the high cycle fatigue domain in order to give a qualitative answer. The work starts from the numerical computation of macroscopic loading corresponding to some fatigue experiments on specimens with an inclusion of metallic grains embedded in a macroscopic matrix. The computed fields are then analysed in terms of the HCF (high cycle fatigue) criterion [1], which is based on the estimation of the shakedown limit at the grain scale. The infinite lifetime prediction is based on the assumption that fatigue occurs if at least one grain fails, i.e. reaches plastic shakedown. The predictions at mesoscopic and macroscopic scales are close if the macroscopic stress distribution is homogeneous. However in the case of the stress gradient, lifetime predicted at the macroscopic scale is underestimated when compared to the predictions made at the mesoscopic scale. Another result is that the gap between microscopic and macroscopic predictions obtained from these numerical computations can roughly be estimated by a diminution of stress of the same order of magnitude as found in the experiments and phenomenological observations. 相似文献