结冰风洞中过冷大水滴云雾演化特性数值研究

为明晰结冰风洞中过冷大水滴（SLD）云雾演化特性,发展了基于欧拉法的SLD液滴运动、传热和传质耦合计算方法,针对3 m×2 m结冰风洞主试验段水平收缩构型,分析了SLD云雾沉降收缩特性、动量平衡特性和热平衡特性,探索了液滴变形破碎的影响,评估了构型出口处SLD液滴动量平衡和热平衡状态。研究结果表明：直径超过250 μm的SLD液滴在构型内会发生显著形变,液滴尺寸越大则变形程度越强,尤其在160 m/s工况下,当液滴直径超过750 μm后,SLD液滴甚至会发生破碎;液滴变形破碎效应会增大液滴加速度和液滴温度下降率,促使SLD液滴趋近动量平衡和热平衡状态;SLD云雾（最大液滴直径小于1 000 μm）在构型出口处会出现显著的粒径浓度分层、动量分层和热分层现象,其中直径小于100 μm的小尺寸液滴速度快、温度低且不断凝结,趋于平衡态,但直径超过500 μm的大尺寸SLD液滴速度慢、温度高且不断蒸发,则显著偏离平衡态;增大试验段气流速度尽管会减弱SLD云雾粒径浓度分层程度,但会增强动量分层和热分层程度,尤其在160 m/s工况下,SLD云雾会均匀分布在构型出口中心区域内（-0.75 m < Y < 0.75 m且-0.5 m < Z < 0.5 m）,与其平衡态间的最大速度差和温度差将分别超过18 m/s和20℃。     

A constitutive model coupling damage and material anisotropy for wide stress triaxiality

A constitutive model that can describe the damage evolution of anisotropic metal sheets during the complex forming processes which experience wide stress triaxiality history is essential to accurately predict the deformation and rupture behaviors of the processes. In this study, a modified Lemaitre damage criterion which couples with the anisotropic Barlat 89 yield function is established. The effects of stress triaxiality, Lode parameter and shear stress on damage accumulation are considered in the constitutive model. The model is numerically implemented and applied to fracture prediction in tensile tests with different stress triaxialities and a complex deformation process with wide stress triaxiality history. The good consistency of predictions and experiments indicates that the modified Lemaitre damage model has excellent fracture prediction ability. Finally, the accuracy of the model is analyzed and discussed.     

结合损伤力学与有限元方法预估铆接结构疲劳寿命

利用飞机铆接试验件疲劳试验数据,结合损伤力学与有限元方法,通过MATLAB调用ABAQUS进行损伤演化方程参数的遗传优化反演。将反演得到的损伤演化方程用于飞机结构疲劳寿命预估中,对机翼蒙皮锪窝形式的铆接结构进行了寿命计算和分析,并与试验数据作对比,证明了方法的可行性。     

化学镀镍钨磷合金过程中的析氢行为和沉积机理

本文研究了化学镀镍钨磷合金过程中的析氢行为，发现总析氢量大于金属沉积的量，即产生氢气的法拉第电流大于金属沉积的法拉第电流。认为镍钨磷合金化学沉积的机理是镍、钨、磷、氢的竞争放电，且除金属沉积时伴随着等量的析氢外，氢也能单独析出。温度、pH值和亚磷酸根浓度对合金沉积速度和合金成分的影响表明，该体系能在很宽的工艺范围内获得光亮、均匀、结合力良好的镀层。用塔菲尔斜率分析法测量的合金沉积速度与重量法测得的相一致，说明电化学方法可以用于确定化学度的沉积速度。     

正交铺设陶瓷基复合材料基体裂纹演化研究(英文)

采用能量平衡法对正交铺设陶瓷基复合材料在单轴拉伸载荷作用下的基体裂纹演化进行了研究。在拉伸载荷的作用下,正交铺设陶瓷基复合材料有5种开裂模式。开裂模式3包括横向开裂、基体开裂和纤维/基体界面脱粘;开裂模式5只包括基体开裂和纤维/基体界面脱粘。本文得到了两条横向裂纹之间出现开裂模式3和5的初始基体开裂应力;并得到了开裂模式3多裂纹演化的初始基体开裂应力。讨论了铺层厚度、纤维体积含量、纤维/基体界面剪应力和界面脱粘能对基体开裂应力和基体裂纹演化的影响。结果表明,对于SiC/CAS材料而言,两条横向裂纹之间首先出现开裂模式3。     

数据库开放对象的数学模型

本文根据系统论提出了开放对象的概念,认为客观世界是由开放对象构成的。它本身是一个递归定义的层次结构,同时具有目的性和适应环境、改造环境的能力即具有自我进化的能力。每个开放对象与其外界的通讯只能通过信息来完成,而且允许它们对同一个消息具有完全不同的理解。开放对象实质是面向对象+人工智能+数据库的一个模型。同时本文还给出它的形式定义。     

Diversity of Comets: Formation Zones and Dynamical Paths

The past dozen years have produced a new paradigm with regard to the source regions of comets in the early solar system. It is now widely recognized that the likely source of the Jupiter-family short-period comets (those with Tisserand parameters, T > 2 and periods, P, generally < 20 years) is the Kuiper belt in the ecliptic plane beyond Neptune. In contrast, the source of the Halley-type and long-period comets (those with T < 2 and P > 20 years) appears to be the Oort cloud. However, the comets in the Oort cloud almost certainly originated elsewhere, since accretion is very inefficient at such large heliocentric distances. New dynamical studies now suggest that the source of the Oort cloud comets is the entire giant planets region from Jupiter to Neptune, rather than primarily the Uranus-Neptune region, as previously thought. Some fraction of the Oort cloud population may even be asteroidal bodies formed inside the orbit of Jupiter. These comets and asteroids underwent a complex dynamical random walk among the giant planets before they were ejected to distant orbits in the Oort cloud, with possible interesting consequences for their thermal and collisional histories. Observational evidence for diversity in cometary compositions is limited, at best. This revised version was published online in June 2006 with corrections to the Cover Date.     

箱梁颤振过程中旋涡的演化规律及气动力的变化特性

利用粒子图像测速技术（PIV）观测了箱梁颤振过程中模型周围流场的旋涡特征,以模型扭转振动位移作为参考信号,采用相位平均的方法研究了旋涡规律性演化对模型周期性振动的驱动作用。风速较低时,箱梁振幅很小,其尾部风嘴附近上侧的旋涡尺度也很小,不易观测到,而下侧的旋涡尺度较大,其形状接近于圆形。当风速接近颤振临界风速时,箱梁振幅明显增大,并且模型尾部风嘴上侧的旋涡尺度也显著增大,达到与下侧旋涡尺度相匹配的程度,模型尾部风嘴上下侧旋涡的交替作用主导了结构振动直到模型振动发散。基于流固松耦合的计算策略,采用计算流体动力学（CFD）的数值方法模拟了箱梁颤振临界状态下的绕流特性,结合正交特征分解（POD）的方法研究了模型颤振时刻表面压力的空间分布特征,通过分析发现在颤振过程中箱梁表面波动压力的主控成分向迎风侧风嘴漂移。     

Dynamical evolution of high area-to-mass ratio debris released into GPS orbits

A large set of simulations, including all the relevant perturbations, was carried out to investigate the long-term dynamical evolution of fictitious high area-to-mass ratio (A/M) objects released, with a negligible velocity variation, in each of the six orbital planes used by Global Positioning System (GPS) satellites. As with similar objects discovered in near synchronous trajectories, long lifetime orbits, with mean motions of about 2 revolutions per day, were found possible for debris characterized by extremely high area-to-mass ratios. Often the lifetime exceeds 100 years up to A/M ∼ 45 m²/kg, decreasing rapidly to a few months above such a threshold. However, the details of the evolution, which are conditioned by the complex interplay of solar radiation pressure and geopotential plus luni-solar resonances, depend on the initial conditions. Different behaviors are thus possible. In any case, objects like those discovered in synchronous orbits, with A/M as high as 20–40 m²/kg, could also survive in this orbital regime, with semi-major axes close to the semi-synchronous values, with maximum eccentricities between 0.3 and 0.7, and with significant orbit pole precessions (faster and wider for increasing values of A/M), leading to inclinations between 30° and more than 90°.