高超声速小钝锥尾流转捩规律与光电特性

显式有限差分方法用于求解小钝锥高超声速化学非平衡尾流的轴对称边界层方程。该方法既适用于层流也适用于湍流。应用 Goldburg 转捩准则确定转捩初始位置。详细地计算了小钝锥尺寸、飞行速度、高度对尾流转捩和光电特性的影响。从计算中得到转捩和光电特性变化的一些有用规律。对湍流亚密部分的雷达散射截面进行了规律性分析。计算结果具有实用参考价值。     

一种微波等离子体原子氧模拟装置

介绍了一种新颖的原子氧模拟试验装置。该装置采用了微波电子回旋共振（ｅｌｅｃｔｒｏｎｃｙｃｌｏｔｒｏｎｒｅｓｏｎａｎｃｅ简称“ＥＣＲ”）的先进技术。最佳调试状态下，可获得１０（１５）／（ｃｍ２·ｓ）的束流。在该试验装置上，对航天器上常用的Ｋａｐｔｏｎ和石墨环氧材料进行了原子氧效应试验，首次在国内成功的获得了原子氧束流模拟试验的样品结果。对样品的表面形貌分析证明：试验结果完全与国外同类设备的试验结论一致，这标志着中国在原子氧地面模拟技术领域的研究已取得重要进展。     

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.     

MONITORING OF ENERGETIC PARTICLE ENVIRONMENT INSIDE THE CHINA-BRAZIL EARTH RESOURCE SATELLITE

On 14 October 1999, the Chinese-Brazil earth resource satellite (CBERS-1) was launched in China. On board of the satellite there was an instrument designed at Peking University to detect the energetic particle radiation inside the satellite so the radiation fluxes of energetic particles in the cabin can be monitored continuously. Inside a satellite cabin, radiation environment consists of ether penetrated energetic particles or secondary radiation from satellite materials due to the interactions with primary cosmic rays.Purpose of the detectors are twofold, to monitor the particle radiation in the cabin and also to study the space radiation environment The data can be used to study the radiation environment and their effects on the electronics inside the satelhte cabin. On the other hand, the data are useful in study of geo-space energetic particle events such as solar proton events, particle precipitation and variations of the radiation belt since there should be some correlation between the radiation situation inside and outside the satellite.The instrument consists of two semi-conductor detectors for protons and electrons respectively. Each detector has two channels of energy ranges. They are 0.5-2MeV and ≥2MeV for electrons and 5-30MeV and 30-60MeV for protons. Counting rate for all channels are up to 104/(cm2@s)and power consumption is about 2.5 W. There are also the additional functions of CMOS TID (total integrated dose) effect and direct SEU monitoring. The data of CBMC was first sent back on Oct. 17 1999 and it's almost three years from then on. The detector has been working normally and the quality of data is good.The preliminary results of data analysis of CBMC not only reveal the effects of polar particle precipitation and radiation belt on radiation environment inside a satellite, but also show some important features of the geo-space energetic particle radiation.As one of the most important parameters of space weather, the energetic charged particles have great influences on space activities and ground tech nology. CBMC is perhaps the first long-term on-board special equipment to monitor the energetic particle radiation environment inside the satellite and the data it accnmulated are very useful in both satellite designing and space research.     

利用MF雷达对耀斑期间电离层D区电子密度的观测研究

利用MF雷达观测资料对X级别耀斑爆发期间在66-80km高度之间的电子密度进行了研究，观测到了耀斑爆发期间电子密度的突然增加，在较低高度上的电子密度的时间变化趋势与耀斑的软X射线辐射通量相关．电子密度的变化强度依赖于具体的耀斑参数，有些耀斑引起的电子密度增加高达400cm^-3，有些仅为100cm^-3左右．但耀斑期间在这一高度区间增加的总电子含量增量仅占耀斑辐射引起的整个电离层总电子含量增量的千分之一左右．最后，利用恢复阶段电子密度的时间变化过程估算了1997年11月4日耀斑期间部分高度上的有效复合系数．     

A time-frequency analysis of the thermal radiation background anomalies caused by large earthquakes: A case study of the Wenchuan 8.0 earthquake

Strong earthquakes have an impact on the regional thermal radiation background, which has been both observed and confirmed. This effect produces anomalies in the thermal radiation background (TRBA) and increases the difficulty of extracting a thermal radiation anomaly (TRA) that is associated with an earthquake occurring during the same time period. The extraction and identification of such anomalies has been ignored by previous studies. In this study, we investigate the time-frequency analysis (TFA) method, together with the wavelet filtering of the Daubechies method and the relative power spectrum analysis of the Fourier Welch method to extract and analyse the TRBA caused by the 2008 Wenchuan Ms 8.0 earthquake and the TRA of the 2013 Minxian-Zhangxian Ms 6.6 earthquake using data concerning the brightness temperature of a black body (TBB) from the Fengyun-2 series of geostationary meteorological satellites developed by China. The result showed that this method can effectively extract and analyse the TRBA caused by the Wenchuan earthquake and the TRA of the Minxian-Zhangxian earthquake form a complex background environment. Furthermore, we discussed the impact of the earthquake on the TRBA and segmented the process. The impact is mainly reflected by three aspects; the characteristic period of the TRBA changes, the TRBA occurs at the same time every year, which is identical to the time at which the earthquake anomaly occurred, and the impact process is in stages. We also summarized the correlation between the characteristic parameters of a TRA and the regional thermal radiation background, geography, and climatic factors.     

飞行器表面红外辐射的模型以及红外特征分析(英文)

隐身最重要的技术之一是评估飞行器被红外探测器接收到的红外辐射强度。本文针对飞行器表面红外辐射特征计算的问题提出一个方法。首先通过分析飞行器表面气动加热、发动机热部件等主要热源,建立了CFD计算模型并获得了飞行表面的温度场。并结合反向蒙特卡洛方法建立求解飞行器表面复杂几何外形的红外辐射模型。通过数值模拟,比较了飞行器主要部件在水平和侧向上红外辐射强度所占的比重;并针对飞行器主要部件冷却对红外辐射强度的影响效果进行了研究。计算结果表明:在水平方向降低飞行器头部、垂尾、机翼部件表面温度10K能降低红外辐射强度大于8%;而在侧方向降低飞行器头部、垂尾、机翼部件表面温度10K能降低红外辐射强度小于8%。计算结果可为隐身设计提供参考。     

再入体实验模型热化学非平衡绕流流场的数值分析

利用数值求解一个和多个振动温度热化学非平衡Navier-Stokes方程的CFD计算程序,对爆轰风洞球锥试验模型的热化学非平衡绕流流场进行了数值模拟,分析了分子组分振动温度在全流场(头身部流场和底部流场)中的分布规律.研究结果表明:(1)计算的压力、电子数密度以及流场的光辐射数据与试验数据符合较好;(2)在再入体身部,大多数分子的振动温度峰值大大高于平动温度的峰值;在再入体近尾出现振动温度冻结并大大高于平动温度的现象;CO2的两个振动态的振动温度分布非常接近平动温度分布.     

机载雷达罩热载荷仿真分析关键技术研究

研究了机载雷达罩热载荷仿真分析的3个关键技术,一是雷达罩及天线的CAD建模技术,并应用Fluent计算罩体外表面温度;二是建立雷达罩的多腔体热辐射模型,以得到雷达罩内表面的温度分布;三是温度插值技术,用以将流场计算得到的温度值插值到对应的热应力分析模型上。     

航空发动机燃烧室出口高温热电偶校准技术

在高温校准风洞上,对测量航空发动机燃烧室出口温度气冷式和非气冷式这两种形式的高温热电偶进行校准,确定了高温热电偶的辐射修正系数.校准实验结果表明:高温热电偶的辐射误差随气流速度和压力的增加而降低,而且气流温度与航空发动机机匣壁面温度的温差越大,辐射误差也越大.比较两种结构形式的高温热电偶,非冷却式高温热电偶的测量误差比气冷式高温热电偶的相对较小.