导弹机动飞行的弹道参数估算

为简化计算,根据导弹的质心运动方程,通过近似处理导出了导弹机动飞行中助推段、跨越段和机动段弹道参数的估算公式。仿真计算表明,该估算公式的计算结果与理论公式的偏差较小,且方法简便,可用于导弹机动飞行的弹道设计。     

基于统计参数分析和RBF网络的动调陀螺故障诊断方法

针对动调陀螺故障振动信号的特点,提出了一种基于振动统计参数分析和神经网络的动调陀螺故障诊断方法.该方法通过计算原始振动信号的一组统计参数作为表征故障的特征信息,以此作为RBF神经网络的输入参数来学习并识别陀螺故障.实验结果表明,采用对统计参数的计算能够简单、有效地提取陀螺故障特征信息;运用神经网络进行故障诊断建模,使诊断具有自适应、自学习的能力,诊断结果更加可靠.     

CPL蒸发器传热和蒸发流动过程的分布参数模型

针对ＣＰＬ蒸发器，建立了可据以分析其传热过程和蒸发流动过程的分布参数模型，并就一个模拟算例进行了考察，得出了有意义的结论。该模型较之传统集中参数模型的优点在于，其计算结果反映出了蒸发器内沿轴向流动过程中各肋壁温度及肋壁与流动工质之间换热系数大小的变化情况以及蒸发器内局部蒸汽（或液体）的热力状况，因而为从细节上揭示ＣＰＬ蒸发器的传热性能及其工程模型的试验研究、优化设计等打下了一定的基础     

离散系统仿真输出数据的统计分析

概括了分析仿真产生的数据的方法，讨论了离散系统仿真输出分析的目的以及应用统计方法的要求，对单变量情形，给出了有关估计来自终态仿真和和稳态仿真参数的技术。对多变量情形，以终态仿真为例，给出了用于分析离散系统的仿真输出的某些多变量统计技术，并提出均值向量的估计方法。     

一个新的蠕变寿命估算公式的推出

本文从一些经典公式出发,推导出新的寿命公式。另外,通过引入蠕变损伤特征参量的概念还导出类似的另一个蠕变寿命估算公式。所推导出两个公式在16MnR材料中得到较为成功的应用。     

海冰热力模式抛物型分布参数系统区域辨识模型及性质

根据北极海冰的热力学性质,建立了北极海冰热力模式时变区域抛物型分布参数系统及关于雪层与冰层的厚度辨识模型(即最优控制模型),论述了该系统解的存在唯一性及最优控制的必要性条件。     

控制增稳系统参数对飞机纵向飞行品质的影响

本文以纵向控制增稳系统为例,通过计算分析控制增稳系统的几个主要参数对飞机飞行品质的影响与作用,进一步讨论控制增稳系统的参数选择问题。     

大传动比摆线针轮减速机的改进齿形

本文提出采用适当参数的短幅外摆线的等距线替代产生自交的短幅外摆线的等距线或复合齿形作为摆线轮的齿形,以便于既能够保持复合齿形提高效率的目的,又能够简化工艺,提高工效,同时满足摆线齿的修形要求,增大齿顶强度,使啮合传动平稳。文中还给出了一种机型的计算结果和放大的图样。     

二元外压式进气道斜板和唇口参数选择的风洞试验研究

在几何不可调的二元外压式斜板进气道的设计中，选择合理的斜板和唇口几何能数是最重要的问题之一。本文对一个设计马赫数为１．８的这类进气道的斜板和唇口参数进行了风洞试验研究。用缩尺模型风洞试验，对比分析了不同斜板角和不同外侧唇口内唇角，唇缘半径对进气道内流特性的影响，结果表明，对确定的进气道布局，斜板角小的变化对进气道超音速内流总压恢复系数，稳态出口流场周向畸变指数及喘振裕度的影响很大，唇口参数小的改变     

Magnetosphere Imaging Instrument (MIMI) on the Cassini Mission to Saturn/Titan

The magnetospheric imaging instrument (MIMI) is a neutral and charged particle detection system on the Cassini orbiter spacecraft designed to perform both global imaging and in-situ measurements to study the overall configuration and dynamics of Saturn’s magnetosphere and its interactions with the solar wind, Saturn’s atmosphere, Titan, and the icy satellites. The processes responsible for Saturn’s aurora will be investigated; a search will be performed for substorms at Saturn; and the origins of magnetospheric hot plasmas will be determined. Further, the Jovian magnetosphere and Io torus will be imaged during Jupiter flyby. The investigative approach is twofold. (1) Perform remote sensing of the magnetospheric energetic (E > 7 keV) ion plasmas by detecting and imaging charge-exchange neutrals, created when magnetospheric ions capture electrons from ambient neutral gas. Such escaping neutrals were detected by the Voyager l spacecraft outside Saturn’s magnetosphere and can be used like photons to form images of the emitting regions, as has been demonstrated at Earth. (2) Determine through in-situ measurements the 3-D particle distribution functions including ion composition and charge states (E > 3 keV/e). The combination of in-situ measurements with global images, together with analysis and interpretation techniques that include direct “forward modeling’’ and deconvolution by tomography, is expected to yield a global assessment of magnetospheric structure and dynamics, including (a) magnetospheric ring currents and hot plasma populations, (b) magnetic field distortions, (c) electric field configuration, (d) particle injection boundaries associated with magnetic storms and substorms, and (e) the connection of the magnetosphere to ionospheric altitudes. Titan and its torus will stand out in energetic neutral images throughout the Cassini orbit, and thus serve as a continuous remote probe of ion flux variations near 20R _S (e.g., magnetopause crossings and substorm plasma injections). The Titan exosphere and its cometary interaction with magnetospheric plasmas will be imaged in detail on each flyby. The three principal sensors of MIMI consists of an ion and neutral camera (INCA), a charge–energy–mass-spectrometer (CHEMS) essentially identical to our instrument flown on the ISTP/Geotail spacecraft, and the low energy magnetospheric measurements system (LEMMS), an advanced design of one of our sensors flown on the Galileo spacecraft. The INCA head is a large geometry factor (G ∼ 2.4 cm² sr) foil time-of-flight (TOF) camera that separately registers the incident direction of either energetic neutral atoms (ENA) or ion species (≥5^∘ full width half maximum) over the range 7 keV/nuc < E < 3 MeV/nuc. CHEMS uses electrostatic deflection, TOF, and energy measurement to determine ion energy, charge state, mass, and 3-D anisotropy in the range 3 ≤ E ≤ 220 keV/e with good (∼0.05 cm² sr) sensitivity. LEMMS is a two-ended telescope that measures ions in the range 0.03 ≤ E ≤ 18 MeV and electrons 0.015 ≤ E≤ 0.884 MeV in the forward direction (G ∼ 0.02 cm² sr), while high energy electrons (0.1–5 MeV) and ions (1.6–160 MeV) are measured from the back direction (G ∼ 0.4 cm² sr). The latter are relevant to inner magnetosphere studies of diffusion processes and satellite microsignatures as well as cosmic ray albedo neutron decay (CRAND). Our analyses of Voyager energetic neutral particle and Lyman-α measurements show that INCA will provide statistically significant global magnetospheric images from a distance of ∼60 R _S every 2–3 h (every ∼10 min from ∼20 R _S). Moreover, during Titan flybys, INCA will provide images of the interaction of the Titan exosphere with the Saturn magnetosphere every 1.5 min. Time resolution for charged particle measurements can be < 0.1 s, which is more than adequate for microsignature studies. Data obtained during Venus-2 flyby and Earth swingby in June and August 1999, respectively, and Jupiter flyby in December 2000 to January 2001 show that the instrument is performing well, has made important and heretofore unobtainable measurements in interplanetary space at Jupiter, and will likely obtain high-quality data throughout each orbit of the Cassini mission at Saturn. Sample data from each of the three sensors during the August 18 Earth swingby are shown, including the first ENA image of part of the ring current obtained by an instrument specifically designed for this purpose. Similarily, measurements in cis-Jovian space include the first detailed charge state determination of Iogenic ions and several ENA images of that planet’s magnetosphere.This revised version was published online in July 2005 with a corrected cover date.