太阳同步轨道真空紫外光电倍增管的高能粒子屏蔽方法研究

空间辐射环境是导致光电倍增管性能衰变甚至失效的主要原因, 由于空间辐射环境的复杂性以及飞行器在空间活动的轨道、设计寿命和光电倍增管的类型不同, 光电倍增管需要的抗辐射屏蔽要求不同. 以太阳同步轨道高能粒子辐射环境为例, 对真空紫外光电倍增管进行了辐射屏蔽的Monte-Carlo计算, 在此基础上提出了运行于该轨道上的真空紫外光电倍增管的高能粒子屏蔽优化组合. 模拟计算表明, 采用Al-W-Al三层结构的屏蔽组合形式, 其中Al层厚2mm, W厚 0.5mm,可将辐射剂量从原本的9.98× 106rad (Si)降低到 8.41× 102rad (Si), 能较好地满足实际使用要求.      

共硝化及TATN／DADN共硝化合成研究

介绍了共硝化法合成混合硝酸酯的特点及其应用价值,在此基础上较详细地研究了TA(一种三元醇)和DA(一种二元醇)共硝化合成TATN/DADN混合硝酸的工艺条件,分析讨论了各种影响因素对共硝化产率、纯度、TATN/DADN比值的作用,提出了氧化副反应和乳化现象发生的原因及抑制方法。     

国外高能量密度材料与目标化合物CL—20的进展

介绍了国外高能量密度材料(HEDM)发展的新动态。以多硝基/硝胺基多环化合物和主体笼形化合物等的开发研究作为契机,HEDM发展进入了一个新的阶段。CL-20即六硝基六氮杂异伍兹烷(HNIW)是一个很有前途的多环硝胺主体笼形化合物,本文着重评述它的结构、性能、应用及合成途径。认为通过它的六氮杂前驱物体系的基团转化而引入硝基的途径是可取的。     

基于嫦娥一号高能粒子数据的地球磁层屏蔽效应研究

月球绕地球运行轨道约有1/4位于地球磁层内,因此,地球磁层是否会为月球轨道附近高能粒子提供足够的磁场屏蔽对于探索月球活动具有重要影响.嫦娥一号是中国首颗绕月人造卫星,其绕月飞行的工作轨道距离月球表面200 km.通过对嫦娥一号高能粒子探测器(HPD)的探测数据进行分析,比较了当月球位于地球磁层内外6个不同能道(能量范围4～400 MeV)时质子通量的变化,发现当月球位于地球磁层内时,这些能道的质子通量并没有发生显著减少,结果表明地球磁层不能为月球轨道附近高能粒子提供显著的磁屏蔽.     

Nightside 135.6 nm emission enhancements of mid/low latitudes during geomagnetic storms as observed by the ionosphere PhotoMeter (IPM) on the Chinese meteorological satellite FY-3D

IPM has detected nightside 135.6 nm emission enhancements over a wide latitude range, from the sub-auroral latitudes to the equatorial regions during geomagnetic storms. Our work, presented in this paper, uses the data of IPM to understand these 135.6 nm emission enhancements during of geomagnetic storms and studies the variations of total electron content (TEC) and the F₂ layer peak electron density (NmF2) in the region of enhanced emissions. Middle and low latitude emission enhancements are presented during several medium storms in 2018. The variations of both the integrated electron content (IEC) derived from the nighttime OI 135.6 nm emission by IPM and TEC from the International GNSS Service (IGS) relative to the daily mean of magnetically quiet days of per each latitude bin (30°≦geographic latitude < 40°, 15°≦geographic latitude < 30°, 0°≦geographic latitude < 15°, ?15°≦geographic latitude < 0°, ?30°≦geographic latitude < -15°, ?40°≦geographic latitude < -30°) are investigated and show that on magnetically storm day, IEC by IPM always increases, while TEC from IGC may increase or decrease. Even if both increase, the increase of IEC is greater than that of TEC. From the comparison of IEC and TEC during magnetic storms, it can be seen that the enhancement of the nighttime 135.6 nm emissions is not entirely due to the ionospheric change. The time of IEC enhancements at each latitude bin is in good agreement, which mainly corresponds to the main phase time of the geomagnetic storm event and lasts until the recovery phase. The available ground-based ionosonde stations provide the values of NmF2 which match the 135.6 nm emissions measured by IPM in space and time. The variations of NmF2 squared can characterize the variations of the OI 135.6 nm emissions caused by O⁺ ions and electrons radiative recombination. The study results show that the OI 135.6 nm emission enhancements caused by O⁺ ions and electrons radiative recombination (where NmF2 squared increases) are obviously a contribution to the measured 135.6 nm emission enhancements by IPM. The contribution accounts for at least one of all contributions to the measured 135.6 nm emission enhancements by IPM. However, where the NmF2 squared provided by ionosonde decrease or change little (where the OI 135.6 nm emissions cause by O⁺ ions and electrons radiative recombination also decrease or change little), the emission enhancements measured by IPM at storm-time appear to come from the contributions of other mechanisms, such as energetic neutral atoms precipitation, or the mutual neutralization emission (O+ + O-→2O + h? (135.6 nm)) which also occupies a certain proportion in 135.6 nm airglow emission at night.