矢量控制的无刷交流电动机调速系统仿真

本文介绍交流无刷电动机调速系统的仿真方法,知仿真数学模型的建立,速度调节系统控制策略的确定及仿真ＳＩＭＵＬＩＮＫ实现等。本文也给出了一个基于仿真结果设计的实际调速系统。     

三维非结构网格的生成及其应用

采用阵面推进法生成了高质量的三维四面体非结构网格,该方法的特点是在生成单元的同时引入结点,与其他预布结点的方法相比,其好处是能更好地控制网格单元尺度在整个计算域的合理２并提高网格质量。用Ｄｅｌａｕｎａｙ方法连接存储有控制参数的结点生成了背景网格。网格生成过程中采用了合理的数据结构,有效地提高了程序运行效果,最后给出了Ｍ６机翼的数值算例。     

俯仰-滚转耦合两自由度大振幅非定常实验技术

主要介绍了一套用于３ｍ低速风洞的俯仰－滚转两自由度大振幅非定常实验系统。该系统由三大部分组成：俯仰－滚转两自由度的模型动态支撑机构;俯仰－滚转两自由度电控液压系统;数据采集与处理软件系统。该系统可以在风洞中真实模拟飞行器姿态变化,并测量其相应的六分量非定常气动力变化。为飞行器的飞行力学动态性能分析或飞行模拟器提供非定常气动力数据。另外,用三角翼在３ｍ风洞进行了多种运动状态的非定常气动力特性测量,结果真实地反映了大迎角与大滚转角时三角翼的非定常气动特性     

自由飞行下基于集成学习的概率型冲突探测算法

空中交通流量的持续增加对中、短期飞行冲突探测的精度与处理大量目标的能力的要求更高,提出基于集成学习(ensemble learning)的冲突探测算法。首先,对飞机冲突过程建模,收集飞行样本;其次,提取飞机当前位置、速度矢量、向前看时间、待转弯时刻和转角为特征量,训练基本分类器,获得元数据集;然后,以支持向量机为二级分类器,元数据集为新的特征量,训练Stacking元分类器(meta classifier),分类阶段通过Sigmoid函数概率映射法输出冲突概率;最后进行仿真分析。结果表明:基于集成学习的冲突探测算法对冲突探测具有较高的准确率,使得虚警概率大幅下降,且适用于转弯飞行。     

基于多模态滑模的快速非奇异终端滑模控制

根据多模态滑模概念,提出了一种快速非奇异终端滑模控制方法(FNTSM,Fast Nonsingular Terminal Sliding Mode),实现了非奇异终端滑模控制的全局快速收敛.多模态滑模通过设计分段切换函数,实现多个滑动模态.FNTSM的切换函数由线性滑模的切换函数和非奇异终端滑模的切换函数连接而成.当系统状态远离平衡点时,系统运行于线性滑动模态;当系统状态靠近平衡点时,系统运行于非奇异终端滑动模态.设计了切换型控制律,保证了系统的到达时间和滑动时间都是有限的.数值仿真表明:FNTSM控制与非奇异终端滑模控制、线性滑模控制相比具有快速性优点.      

Temperature effects in the ATIC BGO calorimeter

The Advanced Thin Ionization Calorimeter (ATIC) Balloon Experiment had a successful test flight and a science flight in 2000–01 and 2002–03 and an unsuccessful launch in 2005–06 from McMurdo, Antarctica, returning 16 and 19 days of flight data. ATIC is designed to measure the spectra of cosmic rays (protons to iron). The instrument is composed of a Silicon matrix detector followed by a carbon target interleaved with scintillator tracking layers and a segmented BGO calorimeter composed of 320 individual crystals totaling 18 radiation lengths to determine the particle energy. BGO (Bismuth Germanate) is an inorganic scintillation crystal and its light output depends not only on the energy deposited by particles but also on the temperature of the crystal. The temperature of balloon instruments during flight is not constant due to sun angle variations as well as differences in albedo from the ground. The change in output for a given energy deposit in the crystals in response to temperature variations was determined.     

面齿轮滚刀基本蜗杆的设计方法

面齿轮传动由于其独特的传动优点,成为航空传动的主要研究方向.根据面齿轮传动原理,建立面齿轮加工坐标系,得到了面齿轮齿面方程,分析了面齿轮齿顶变尖和齿根根切的限制条件,同时根据实际算例讨论了面齿轮内外半径随压力角变化的规律,所获得的结论对面齿轮的设计具有参考价值.最后分析面齿轮的滚切原理,根据齿轮啮合原理,建立面齿轮滚刀型面方程,采用数值计算方法,得到滚刀型面离散三维坐标值,借助三维造型软件得到面齿轮滚刀基本蜗杆三维模型.     

基于褶皱的平流层浮空器升空结构形变模拟

平流层浮空器囊体材料具有非线性、黏弹性、各向异性和不能抗压等特点,起皱现象是在升空膨胀过程中必然会出现的形变状态,褶皱的扩展会影响整个囊体结构的受力状态,改变囊体变形和应力分布.同时,褶皱的存在还会影响囊体结构的动力学行为和空间环境下的热力学分布.通过主应力-主应变相结合准则对褶皱区域进行判别,采用修正褶皱单元的本构矩阵方程的方法对褶皱区域进行处理,地面充氦气试验证明了新方法的模拟结果更加接近测试值.从而为平流层浮空器设计提供了一种有效的分析方法.     

交会对接寻的段机动故障对策分析与仿真

根据寻的段的机动故障类型及其约束条件,首先给出了该段的故障控制策略规划模型,然后给出了相应的故障对策,最后基于高精度轨道模型仿真分析了各种故障工况。仿真结果表明,所提出的对策能较好的应对寻的段各类机动故障。     

Vertical wavenumber spectra of atmospheric ozone measured from ozonesonde observations

Vertical profiles of ozone have been measured at balloon altitudes. Our purpose is to examine the character of vertical wavenumber spectra of ozone fluctuations, to assess the possible roles of gravity wave field in ozone fluctuations, and to determine dominant vertical wavelengths of ozone spectra. Vertical wavenumber spectra of 12 ozone fluctuations obtained during June–August 2003 are presented. Results indicate that mean spectral slopes in the wavenumber range from 4.69 × 10⁻⁴ to 2.50 × 10⁻³ cyc/m are about −2.91 in the troposphere and −2.87 in the lower stratosphere, which is close to the slope of −3 predicted by current gravity wave saturation models. The consistency of the observed spectral slopes with the value of −3 predicted by current gravity wave saturation models suggests that the observed ozone fluctuations are due primarily to atmospheric gravity waves. At m = 1/(1000 m) the mean spectral amplitude is over 30 times larger in the lower stratosphere than in the troposphere. Mean vertical wavenumber spectra in area-preserving form reveal dominant vertical wavelengths of ∼2.6 km in the troposphere and ∼2.7 km in the lower stratosphere, which is consistent with the values varying between 1.5 and 3.0 km estimated from the velocity field and temperature field at these heights.