航空制件超声检测中的声场特性分析

 针对航空制件超声检测中影响缺陷定量准确性的声场问题进行了深入讨论, 研究了脉冲波声场的计算方法, 设计了相应的计算软件并绘制出实用换能器声轴线上的声压分布曲线, 分析了不同材料和厚度的采样回波对频谱的影响, 比较了连续波声场和脉冲波声场的分布特性及异同点。研究结果为提高超声检测中缺陷定量的准确性和科学性提供了依据。     

薄膜材料和纤维材料的热扩散率测量

介绍了激光热波技术用于测量薄膜材料和纤维材料热扩散率的测试系统，测试温度范围为２０－５００℃。讨论了测量中的各种试验条件、基本公式和误差分析。在理论上此系统可以应用于任何厚度样品面向热扩散率的测量。     

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.     

正弦波模型化测量方法及应用

本文对应用较多的几种正弦波模型化测量方法进行了综述，它们是曲线拟合法、直方图统计分析法、FFT法和拍频法。较详细地介绍了这几种测量方法的典型用途以及特点，通过比较几种方法的优缺点，讨论了它们应用中的局限性。     

圆管内表面周向三维裂纹应力强度因子的新解法

对圆管内表面周向三维裂纹应力强度因子的求解,发展了传统的能量差率方法,同时研究了新兴的双重边界元理论,并运用这两种新解法,分别获得了关于裂纹张开位移的伯努利方程的半数值半工程封闭解和基于非连续裂尖奇异单元离散的应力强度因子数值解。并讨论了应力强度因子与裂纹形状a/c及裂纹深度a的关系,两者比较分析发现,其计算结果规律是一致的,且能量差率方法更保守,也更安全。     

旋转爆轰流场的数值模拟

基于带化学反应的二维Euler方程,采用氢气-空气的9组分19步基元反应简化模型,对充有当量比的氢气-空气预混气和空气的环形旋转爆轰流场,从点火燃烧到发展成旋转爆轰的过程进行了数值模拟。根据数值结果分析了波后流场中爆轰产物受激波、高温和离心力等作用而挤向外壁,形成有利于充入燃料,实现持续稳定旋转爆轰的流场特征。还讨论流场中爆轰波、激波与间断面和内外壁面反射或折射,从而形成多个激波相交的波系特征。为认识和理解旋转爆轰流场,开展旋转爆轰的实验研究等具有现实的指导意义。     

钛合金表面镍包石墨喷涂层的耐磨性能

为了提高钛合金的表面耐磨性,利用氧乙炔热喷涂枪,在TC4合金表面上制备出镍包石墨涂层。采用MXP-2000型销盘式摩擦磨损实验机,进行钛合金及其镍包石墨涂层的干摩擦磨损实验,并利用扫描电镜对磨损表面进行观察和分析。实验结果发现,镍包石墨涂层的摩擦系数只有钛合金的一半左右,前者磨损量为后者的1/6,说明镍包石墨涂层可以大大提高钛合金的表面耐磨性能。TC4合金的磨损机制以黏着磨损为主,喷涂层的磨损机制以磨粒磨损为主,喷涂层中的石墨润滑相是其耐磨性高的主要原因。     

分布式防火墙在网络安全中的技术应用

分布式防火墙为网络安全提供了技术支持,可为企事业单位提供多层次、多协议的全方位安全体系。采用主机驻留的方式保护网络中的关键结点服务器、数据和工作站免受非法入侵的破坏,采用多层过滤,入侵检测,日志记录等手段为不同服务器和主机实施安全策略。较好地解决了企业内网与外网以及内部子网之间的非法攻击问题。     

基元化学反应一维爆轰波的数值模拟

应用基元化学反应模型对一维氢氧混合气体爆轰波进行数值模拟。采用一端高温高压点火起爆的方式,模拟爆轰波的传播。对一维爆轰波的结构、传播特征以及各个化学组分的变化趋势进行了研究。通过将模拟的结果同国内外的研究结果进行对比,发现了一些规律,为多维爆轰波的数值模拟和脉冲爆轰发动机的研究奠定一定的基础。     

高速列车进入带缓冲结构隧道的压力变化研究（I）

给出了列车穿越带有缓冲结构的隧道压力变化的三维粘性流场数值模拟过程，控制方程为三维粘性、可压缩、非定常流的N．S方程，空间离散采用了中心有限体积法格式，时间采用预处理二阶精度多步后差分格式进行离散，对列车与隧道之间的相对运动采用移动网格技术处理。对不同的缓冲结构缓解隧道内瞬变压力及压力梯度的作用进行了研究。研究结果表明，缓冲结构的设置能够有效地降低隧道内的压力和压力梯度的最大值，其原因在于缓冲结构延长了压缩波压力上升的时间，降低列车突入隧道时所形成的最大压力梯度；另一方面由于压缩波在缓冲结构和列车、隧道之间多次的反射，也降低了压力峰值。