大气湍流光学长曝光像的数值计算

在介绍大气湍流光学长曝光像的两个模型——高斯模型(空间域模型)和统计平均光学传递函数模型(空间频率域模型)的基础上，推导两模型之间的关系与差别，并应用两模型数值计算了扩展目标通过大气的长曝光成像结果。此外，还应用高斯模型给出了自适应光学系统校正后的远场光斑。     

高能CO2激光腔镜高反介质薄膜的传输特性

为了获得适用于高能CO2激光器的高抗破坏阈值高反薄膜,以10.6μm高反膜ZnSe/YbF3,PbTe/BaF2膜系为例,数值模拟了激光在高反介质膜中的传输的场特性;给出了激光在多层介质膜中的场强分布、温度场分布及热应力分布。结果表明硅镜基体上的PbTe/BaF2膜系所需膜层厚度小、膜层数少,反射率可高达99.98%。     

神舟2号大气密度探测器的探测结果(Ⅰ)日照和阴影区域热层大气密度变化

选用了神舟2号（SZ-2）大气密度探测器在2001年2—4月间的探测数据,进行日照和阴影区域热层大气密度变化的探讨.结果表明:在高度410km附近,日照和阴影区域大气密度变幅为2—3倍,变幅的大小与地磁活动程度呈负相关关系.日照面大气密度峰区位于星下点地方时1400—1500LT的纬度处,峰值大小与太阳活动程度呈正相关关系.阴影面大气密度谷区位于星下点地方时0400-0500的纬度处,同时在±10°纬度区域中还出现了阴影面峰区.     

参量型空气折射率传感系统

本系统分别利用传感器测出空气的温度、气压和湿度三个参量,把测量值用一个通用于不同机型的接口电路连接到微机进行数据处理并计算出空气折射率值。文中叙述了传感器及其检测电路的设计原理,给出了检测和接口电路框图、计算公式和程序流程图。整个系统已通过联机调试和初步的对比试验。     

Atmospheric reentry hemisphere prediction for prograde orbits using logical disjunction

A unique logic-based algorithm for atmospheric reentry hemisphere prediction is presented for spacecraft in low-eccentricity, prograde low Earth orbits at altitudes of 300 km and lower. Using two-line element (TLE) data for initial orbit conditions, coupled with coarse estimates for spacecraft aerodynamic characteristics, the algorithm relies on logical disjunction operations based on a dual analysis of histogram and two-weighted Gaussian probability density function (PDF) fits of predicted reentry latitude data. The algorithm requires the execution of a series of parametric simulations to determine the reentry hemisphere for variations in spacecraft aerodynamic coefficients and drag reference area. When implemented, the algorithm yields accurate hemisphere predictions on average 15 days from reentry as demonstrated by historical reentry cases from 1979 to 2018. All reentry cases were selected to demonstrate the algorithm’s ability to deliver accurate reentry hemisphere predictions for spacecraft with varying physical size and mass, and reentering during different periods of solar cycle activity.     

0.3 m低温风洞液氮供给系统研制

基于系统级的一维热流体模拟分析,建立了适用于研究分析0.3 m低温风洞液氮供给系统的数学模型,并开展了系统漏热、两相流及缓冲罐中液氮容积等流体动力学分析;在系统现有控制策略及试验数据的基础上,基于该数学模型开展了系统压力动态响应分析,获得了在阀门动态调节过程中管网压力的瞬态响应,计算结果与试验值的总体误差控制在10%以内。喷射压力一致化改造避免了阀间干扰,添加的回流管道消除了供给末端的两相流现象,使喷射压力控制精度达到1.1%,调节时间减少到23 s,实现了风洞总温快速安全调节和精确控制。     

吸气模式激光推进空气等离子体光谱

利用实验室自行研制的紫外预电离CO2激光器进行了激光等离子体实验,实验采用底面直径均为60mm,焦距分别为5 mm和10 mm的两种抛物面光船。介绍了激光等离子体光谱和明显的特征谱线,以及激光等离子体温度估计模型;分析了两种光船对激光等离子体的影响。实验表明:相同底面直径10 mm焦距光船产生的等离子体信号峰值和持续时间均略大于5 mm焦距光船;10 mm焦距光船产生的等离子体温度明显高于5 mm的,最大温度产生时间比5 mm光船要晚一些。     

A Comparative Study of the Influence of the Active Young Sun on the Early Atmospheres of Earth, Venus, and Mars

Because the solar radiation and particle environment plays a major role in all atmospheric processes such as ionization, dissociation, heating of the upper atmospheres, and thermal and non-thermal atmospheric loss processes, the long-time evolution of planetary atmospheres and their water inventories can only be understood within the context of the evolving Sun. We compare the effect of solar induced X-ray and EUV (XUV) heating on the upper atmospheres of Earth, Venus and Mars since the time when the Sun arrived at the Zero-Age-Main-Sequence (ZAMS) about 4.6 Gyr ago. We apply a diffusive-gravitational equilibrium and thermal balance model for studying heating of the early thermospheres by photodissociation and ionization processes, due to exothermic chemical reactions and cooling by IR-radiating molecules like CO₂, NO, OH, etc. Our model simulations result in extended thermospheres for early Earth, Venus and Mars. The exospheric temperatures obtained for all the three planets during this time period lead to diffusion-limited hydrodynamic escape of atomic hydrogen and high Jeans’ escape rates for heavier species like H₂, He, C, N, O, etc. The duration of this blow-off phase for atomic hydrogen depends essentially on the mixing ratios of CO₂, N₂ and H₂O in the atmospheres and could last from ∼100 to several hundred million years. Furthermore, we study the efficiency of various non-thermal atmospheric loss processes on Venus and Mars and investigate the possible protecting effect of the early martian magnetosphere against solar wind induced ion pick up erosion. We find that the early martian magnetic field could decrease the ion-related non-thermal escape rates by a great amount. It is possible that non-magnetized early Mars could have lost its whole atmosphere due to the combined effect of its extended upper atmosphere and a dense solar wind plasma flow of the young Sun during about 200 Myr after the Sun arrived at the ZAMS. Depending on the solar wind parameters, our model simulations for early Venus show that ion pick up by strong solar wind from a non-magnetized planet could erode up to an equivalent amount of ∼250 bar of O⁺ ions during the first several hundred million years. This accumulated loss corresponds to an equivalent mass of ∼1 terrestrial ocean (TO (1 TO ∼1.39×10²⁴ g or expressed as partial pressure, about 265 bar, which corresponds to ∼2900 m average depth)). Finally, we discuss and compare our findings with the results of preceding studies.     

酒石酸钠体系中TC18钛合金阳极氧化膜的制备、表征与疲劳性能

在以酒石酸钠为成膜剂的新型无氟环保电解液体系中对TC18钛合金进行阳极氧化,制备出一种钛合金阳极氧化膜。通过扫描电子显微镜和拉曼光谱仪分析了阳极氧化膜的形貌和相结构。采用电化学方法研究了阳极氧化后TC18钛合金的耐腐蚀性能。采用万能高频疲劳试验机进行高频疲劳试验。结果表明：膜层具有沟壑与鼓包的表面形貌。膜层具有非晶态、锐钛矿型及金红石型TiO₂结构,可能有板钛矿TiO₂结构。阳极氧化后TC18钛合金的耐蚀性有显著的提高。阳极氧化后TC18钛合金的拉伸性能与疲劳性能基本不降低,相比于传统硫酸-磷酸型阳极氧化,拉伸性能和疲劳性能得到了一定的改善。     

钝体稳定射流火焰的火焰面模型数值研究

基于稳态火焰面(SLFM)和交互式非稳态欧拉颗粒火焰面(EPFM)模型对Sydney大学CH4/H2钝体稳定湍流扩散火焰行了数值研究,采用修正的雷诺应力模型(RSM),同时对两种不同规模的甲烷详细化学反应动力学机理进行研究,比较了燃烧模型和反应机理对湍流火焰结构、活性自由基以及氮氧化物预测精度的影响,与实验数据对比结果表明:两种反应机理得到的温度场和主要组分分布基本相同;SLFM模型能对速度场和标量场的分布进行较为准确预测,采用EPFM模型修正后,部分区域OH预测结果更加靠近实验结果;采用EPFM模型对SLFM模型耦合GRI-Mech 211的计算结果修正后,NO量级降低近2倍,预测精度明显改善,与实验结果实现较好的符合,验证了化学反应动力学机理以及非稳态效应对氮氧化物预测精度的影响。