热暴露对IMI834近α高温钛合金组织和拉伸性能的影响

测试了ＩＭＩ８３４高温钛合金在６００～７５０℃的空气中热暴露１００小时后拉伸性能，利用透射电镜和扫描电镜观察了合金暴露前后的组织变化及拉伸断口，认为表面氧化是造成合金热暴露后塑性下降的主要原因，但基体组织内有序α２相和硅化物的析出变化也在不同程度上造居了合金热暴露后的强度和塑性的下降。     

液氢液氧发动机喷管化学反应流数值模拟

用时间相关的半隐格式求解液氢液氧发动机喷管中的化学反应流动，考虑了６种燃烧产物，８个基元反应，得到了流动参数和产物的质量分数在流场中的分布，为发动机化学动力学损失计算和喷管热结构设计提供了必要数据。计算结果表明，采用半隐格式解决组分连续方程刚性引起的数值不稳定是有效的。     

机载小惯量探针研制及在飞机武器发射中的应用

介绍了一种用于飞机武器发射时测量发动机进口动态温升时序的机载小惯量探针,以其独特的研制方法,较好地解决了机载小惯量测温装置、频响与可靠性兼顾这一测试难题,并在武器发射时,成功地用来评价发动机工作稳定性的影响。     

超机动性技术及其战术优势探讨

随着对新型战机机动性要求的提高及飞机在大迎角下过失速状态的深入研究,提出了新型战机的超机动性技术。首先对超机动性的技术内涵、判断准则做简要介绍,然后对现代近距空战中,战机采用超机动性技术可能取得的战术优势及可能存在的一些问题进行了分析探讨。     

滑流区中三角翼大攻角气动力特性的实验研究

一种以后掠75.7°薄三角翼为主要特征的典型航空航天飞行器模型,在激波管风洞马赫数为11.9和15.4两种条件下,攻角范围20°～50°,用模型自由飞方法测量了它们的轴向力系数、法向力系数和俯仰力矩特性。相应的实验雷诺数分别为3.19×10~4和1.64×10~4,这两种流动条件均属于稀薄气流的滑流区。 实验结果表明在M_∞=11.9和15.4两种条件下,两种剖面外形模型的升力系数和阻力系数均随攻角加大而递增,其变化规律有很好的一致性,且对马赫数并不敏感;但从体轴系来看,不仅两种模型的轴向力系数不同,而且因粘性干扰的缘故,同一模型A在M_∞=15.4时比M_∞=11.9时有相对较大的轴向力系数,但两者随攻角变化的规律一致,且当α>45°时接近牛顿值。此外,实验表明两种模型的压心系数随攻角均没有明显变化。     

钝锥有攻角分离流动的数值模拟及其分析

本文定性分析了开式分离的性状,并对钝锥有攻角超声速绕流的开式分离作了数值模拟。分析指出,开式分离可能存在两种形态,第一种分离线的起点为正常点,第二种分离线的起始为鞍、结点(包括螺旋点)的组合。对于第一种形态,分离线的起点是横向分离的起始点,除分离线外,分离面上的流线不是从分离线的起点发出的。对文中计算的情况,流动属第一种开式分离。计算证实了定性分析的结论。计算和分析均指出,对第一种开式分离,在分离的起始区域,分离流面尚未卷曲,但在下游,则变成卷曲面。文中还研究了围绕物体的流管在分离诱导下的变形情况。     

一种模拟喷管二维流场的新方法

采用ＳＩＭＰＬＥ方法对固体火箭发动机喷管进行了纯气相流场的数值模拟。推导了建立在同位网格之上利用协变物理速度分量为计算变量的离散方程，采用协变物理速度分量推导压力修正方程，对密度采用一阶迎风格式插值，将ＳＩＭＰＬＥ方法扩大到计算可压流动。计算结果表明：本方法计算精度高，收敛速度快，程序编写简单。     

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.     

求解可压缩N－S方程的无粘－粘性分数步法

用按物理过程作时间分裂的无粘－粘性分数步法求解可压缩Ｎ－Ｓ方程，无粘步用高效欧拉算法解欧拉方程，粘性步用全隐格式解抛物方程；并采取了有效措施消除由分步法产生的时间和空间不相容性，文中给出了轴对称喷管内外流场的数值模拟结果。     

大瑞利数下二维Benard对流演化过程的DSMC仿真研究

利用DSMC（Direct Simulation Monte Carlo）方法研究了大Rayleigh（瑞利）数条件下稀薄气体的二维Benard对流的特性。考察了流动的非定常演化过程及若干流动特征量随时间的变化特征，得到了与实验较为一致的结论。计算结果表明，当流动控制参数不断增大时，二维Berard对流从热传导状态过渡到热对流状态表现出明显的非定常演化特征。最后当瑞利数增大到一定程度后，注动显示出混沌的特性。