含孔边裂纹各向异性有限板的二维问题

应用边界元法,并结合一种特殊的复变函数基本解,研究了含孔边裂纹的各向异性有限板的应力强度因子修正系数的计算。这种特解边界元法避免了在裂纹附近划分单元,可以获得较好的数值计算精度。通过算例分析,结果表明本方法精度高,运算量小,具有一定的工程应用价值。     

飞机失速/螺旋模型自由飞试验总体方案构想中几个问题的分析

本文对制定飞机失速/螺旋模型自由飞试验总体方案时必然会遇到的一些重要问题进行了分析,其内容涉及模型缩尺比例数 K 的最佳选取、确定飞机进入螺旋特征模拟高度 H_A 的依据、模型投放高度 H_m 的变化范围和试验模型质量 M_m 的控制问题。本文所作的各种分析和提出的原则对各种模型自由飞失速/螺旋试验研究具有普遍意义。     

锯齿扁管内沸腾换热试验

建立以等热流密度方式进行试验件加热的沸腾换热试验系统,分别对当量直径为1.28mm和1.59mm锯齿扁管内R134a工质的沸腾换热特性进行研究,试验参数范围:制冷剂质量流率为68.5~305.5kg/(m2·s),工作饱和压力为0.27~0.46 MPa,加热热流密度为9~42kW/m2。试验结果表明:相同结构的通道,当量直径小换热能力更强;热流密度和饱和压力对沸腾换热的影响与一个干度值有关。当干度小于此值时,沸腾换热系数会随着热流密度及饱和压力增大而增大;而当干度大于此值时,沸腾换热系数随着干度增大而急剧下降,热流密度和饱和压力对换热的影响较小;该干度值会随着热流密度或饱和压力增大而逐渐变小。质量流率对沸腾换热的影响与热流密度有关,随着热流密度增大,质量流率的影响趋向大干度区域。通过分析各参数对沸腾换热的影响,建立了一个预测试验工况下微小尺寸锯齿扁管的沸腾换热系数计算经验公式。     

基于旋转坐标系转轴振动信号的滚动轴承故障诊断方法

实验验证了基于旋转坐标系转轴振动信号的滚动轴承局部故障诊断方法.建立起滚动轴承故障实验台, 采用压电晶体加速度传感器测取转轴的振动.通过滚动轴承内环、外环、滚动体和保持架四种典型故障的实验分析结果, 证明了该方法的可行性, 并发现转轴振动信号的传递路径相对简单, 对轴承内环、滚动体和保持架早期微小故障的发现与诊断可能是有利的.      

大扫描视场飞行器共形光学系统设计

共形光学窗口外表面与飞行器轮廓相同,可以显著提升飞行器的整体性能,但在大扫描视场应用时,引入大量非对称动态像差,严重影响成像质量。针对大扫描视场的共形光学系统,提出了基于共形窗口内表面优化,以及分视场单元透镜阵列的动态像差校正方法,实现动态像差的静态化校正。在84°扫描视场范围内,对共形光学系统进行仿真验证,结果表明：该方法使共形光学系统在全扫描视场范围内的Zernike多项式系数绝对值从0~10.82λ减小到0~1λ（λ为波长）,同时各通道单元透镜阵列保持固定状态。与目前已有方法相比,本文显著提升了大扫描视场共形光学系统的成像质量和系统稳定性,有效简化了系统结构。本文的研究对实现大扫描视场、高成像质量和高稳定性的共形光学系统有重要意义。     

惯性导航系统各种传递对准方法讨论

 本文按对准基本原理将惯性导航系统各种传递对准方法分为两大类,一类可称为计算参数匹配法,它包括速度匹配和位置匹配;另一类可称为测量参数匹配法,它包括加速度匹配、姿态匹配和角速度匹配。文中详细讨论了这两类方法的性质,指出:计算参数匹配法类似静基座自对准和空间率对准,在载体无机动动作时对准时间较长。测量参数匹配法对准时间短,但受载体挠性变形的影响大。     

4F傅里叶变换透镜系统对粒子场全息记录的影响

 4F傅里叶变换透镜系统在空间滤波和光学信息处理中,被广泛用来处理二维透光物体。但在实际应用中,4F系统也被用于三维场的研究。例如三维粒子场的全息记录。由于全息记录的特点,要求了解经4F系统转换后的粒子物光场,以确定粒子场的空间分布。而目前4F系统在粒子场全息记录的应用基础均借助对二维物场的研究理论。本文讨论了经4F系统转换后的三维粒子物光场的特点以及对全息记录的影响。     

Solar Sources of Heliospheric Energetic Electron Events—Shocks or Flares?

Electrons with near-relativistic (E≳30 keV, NrR) and relativistic (E≳0.3 MeV) energies are often observed as discrete events in the inner heliosphere following solar transient activity. Several acceleration mechanisms have been proposed for the production of those electrons. One candidate is acceleration at MHD shocks driven by coronal mass ejections (CMEs) with speeds ≳1000 km s⁻¹. Many NrR electron events are temporally associated only with flares while others are associated with flares as well as with CMEs or with radio type II shock waves. Since CME onsets and associated flares are roughly simultaneous, distinguishing the sources of electron events is a serious challenge. On a phenomenological basis two classes of solar electron events were known several decades ago, but recent observations have presented a more complex picture. We review early and recent observational results to deduce different electron event classes and their viable acceleration mechanisms, defined broadly as shocks versus flares. The NrR and relativistic electrons are treated separately. Topics covered are: solar electron injection delays from flare impulsive phases; comparisons of electron intensities and spectra with flares, CMEs and accompanying solar energetic proton (SEP) events; multiple spacecraft observations; two-phase electron events; coronal flares; shock-associated (SA) events; electron spectral invariance; and solar electron intensity size distributions. This evidence suggests that CME-driven shocks are statistically the dominant acceleration mechanism of relativistic events, but most NrR electron events result from flares. Determining the solar origin of a given NrR or relativistic electron event remains a difficult proposition, and suggestions for future work are given.     

Elemental Abundances of the Bulk Solar Wind: Analyses from Genesis and ACE

Analysis of the Genesis samples is underway. Preliminary elemental abundances based on Genesis sample analyses are in good agreement with in situ-measured elemental abundances made by ACE/SWICS during the Genesis collection period. Comparison of these abundances with those of earlier solar cycles indicates that the solar wind composition is relatively stable between cycles for a given type of flow. ACE/SWICS measurements for the Genesis collection period also show a continuum in compositional variation as a function of velocity for the quasi-stationary flow that defies the simple binning of samples into their sources of coronal hole (CH) and interstream (IS).     

Fe/O Ratios in Interplanetary Shock Accelerated Particles

It is widely accepted that diffusive shock acceleration is an important process in the heliosphere, in particular in producing the energetic particles associated with interplanetary shocks driven by coronal mass ejections. In its simplest formulation shock acceleration is expected to accelerate ions with higher mass to charge ratios less efficiently than those with lower mass to charge. Thus it is anticipated that the Fe/O ratio in shock-accelerated ion populations will decrease with increasing energy above some energy. We examine the circumstances of five interplanetary shocks that have been reported to have associated populations in which Fe/O increases with increasing energy. In each event, the situation is complex, with particle contributions from other sources in addition to the shock. Furthermore, we show that the Fe/O ratio in shock-accelerated ions can decrease even when the shock is traveling through an Fe-rich ambient ion population. Thus, although shock acceleration of an Fe-rich suprathermal population has been proposed to explain large Fe-rich solar particle events, we find no support for this proposal in these observations.