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.     

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.      

涡扇发动机轴对称引射收敛喷管红外辐射特性

数值研究了涡扇发动机轴对称引射收敛喷管的红外辐射特性.排气系统的流场计算采用商用数值模拟软件,红外辐射特性计算采用自主开发的软件NUAA-IR,计算分析了轴对称收敛喷管和引射收敛喷管在3~5μm波段红外辐射特性以及喷管内不同固体壁面在探测方向上的红外辐射贡献.结果表明:引射收敛喷管的红外抑制作用主要在于引射加强了尾喷流与环境大气的掺混,减小了尾喷流的长度,降低了燃气流的红外辐射;引射收敛喷管对喷管内固体壁面的遮挡以及降温作用很小,只在方位角为20°方向上对内涵壁面、外涵内壁等中低温壁面有效;引射收敛喷管的总积分辐射强度在方位角为0°~15°范围内与收敛喷管几乎相等,在其他方位角范围内均小于收敛喷管,且在方位角为40°方向上降低幅度达到最大,约为34%.      

民用飞机燃油箱点燃防护设计研究

通过研究燃油箱点燃防护适航要求的发展历程,基于对最新适航条款要求的分析和理解及燃油箱点燃防护机理分析,归纳总结了适用于民用飞机燃油箱点燃防护的设计措施,包括点火源防护、减少燃油蒸气和加装惰化系统,为民用飞机燃油箱点燃防护设计和适航验证提供借鉴和参考。     

球面收敛二元矢量喷管气动及红外特性研究:模拟地面状态

采用数值模拟方法对涡扇发动机排气系统球面收敛二元矢量喷管的气动和红外辐射特性进行了研究,研究仅针对地面状态和俯仰偏转.结果表明:俯仰偏转角在小于20°范围内,俯仰偏转对排气系统推力系数和总压恢复系数的影响微弱,气动推力矢量角与俯仰偏转角几乎相等;由于气体的容积性热辐射特征,喷管俯仰偏转角的变化引起高温喷流红外辐射的方向性变化明显,喷管俯仰偏转时的热喷流在3~5μm波段红外辐射呈现一定幅度的增加;排气系统在3~5μm波段的红外辐射峰值随俯仰偏转角的增加而趋于减小,其出现位置小于俯仰偏转角;在大的俯仰偏转角下,排气系统在垂直探测平面上方的红外辐射较无矢量偏转情形有所降低,但在探测面下方却有明显的增强,导致另一个峰值的出现.