质子辐射带辐射中心区域模型

利用AP-8和CRRESPRO质子辐射带模式数据库, 比较了二者在磁赤道面上计算结果 的差异并给出其差异原因. 利用AP-8模式数据库数据, 建立起质子辐射带函数形式的辐射中心区域模式, 包括各能道全向微分通量峰值所对应的L值(L_c) 随能量E的变化模式以及各能道全向微分通量峰值J_max随能量E的变化模式. 利用RBSP A卫星REPT望远镜在磁赤道面上的高能质子观测数据, 分别与 AP-8模式、CRRESPRO模式及本文所得辐射中心区域模式计算结果进行比较, 发现在78.9, 102.6和208MeV三个能道上, RBSP A卫星观测所得各能道全向微分 通量明显偏大, 而L_c与AP-8或本文辐射中心模式所得结果基本一致; RBSP A卫星也观测到CRRESPRO Quiet模式所得的隐性第二质子辐射带结构.     

Results from the ESA SREM monitors and comparison with existing radiation belt models

The Standard Radiation Environment Monitor (SREM) is a simple particle detector developed for wide application on ESA satellites. It measures high-energy protons and electrons of the space environment with a 20° angular resolution and limited spectral information. Of the ten SREMs that have been manufactured, four have so far flown. The first model on STRV-1c functioned well until an early spacecraft failure. The other three are on-board, the ESA spacecraft INTEGRAL, ROSETTA and PROBA-1. Another model is flying on GIOVE-B, launched in April 2008 with three L-2 science missions to follow: both Herschel and Planck in 2008, and GAIA in 2011). The diverse orbits of these spacecraft and the common calibration of the monitors provides a unique dataset covering a wide range of B-L* space, providing a direct comparison of the radiation levels in the belts at different locations, and the effects of geomagnetic shielding. Data from the PROBA/SREM and INTEGRAL/IREM are compared with existing radiation belt models.     

基于NOAA卫星数据的辐射带质子投掷角分布研究

利用NOAA-12卫星数据对空间环境平静时期太阳同步轨道处辐射带质子投掷角分布进行了研究. 根据投掷角分布的经验公式,计算出90°投掷角的质子方向强度和各向异性指数n. 质子投掷角分布按n的取值范围可分为三类,即90°峰值分布、平顶分布和蝴蝶形分布. 观测证实,对于辐射带质子,三种分布类型均存在并且具有明显的空间区域特征. 在内辐射带边缘地区90°峰值分布占主要优势;在外辐射带高L值区域,90°峰值分布明显减少,平顶分布和蝴蝶形分布逐渐增多. 针对90°峰值分布,研究了质子强度各向异性的区域分布特征,对于内辐射带区域,n值随L值的增大而增大,对于外辐射带,n值表现为逐渐下降的趋势. 为了研究质子投掷角分布对磁地方时的依赖关系,分析了能量为250～800keV的质子在两个不同磁地方时范围的投掷角分布规律. 结果显示,在内辐射带,质子强度的投掷角分布相对稳定,随磁地方时的变化并不显著;而在外辐射带的高L值区域,质子强度的投掷角分布随磁地方时变化明显,与磁地方时之间有明显的依赖关系.     

High energy charged particle experiment – A payload proposal to KuaFu-B mission

High Energy Charged Particle Experiment (HECPE) is to measure the fluxes of MeV electrons and tens of MeV protons. The two satellites of KuaFu-B are in the same polar orbit with apogee 7.0R_E, perigee 1.8R_E. They can sweep large L values and pass through the inner and outer radiation belts. The high energy electrons and protons in the radiation belts are principal sources for failures of satellites and spacecrafts in the Earth orbits. The enhancements of the high energy electrons and protons, so-called energetic particle events, are important phenomena of the Space Weather. The energy ranges monitored by HECPE are 0.3–0.5 MeV, 0.5–1.0 MeV, 1.0–2.0 MeV, and E > 2.0 MeV for electrons, 5–10 MeV, 10–20 MeV, 20–40 MeV, and 40–80 MeV for protons.     

Characterization of the near Earth radiation environment by Liulin type spectrometers

Comprehensive study of the dose, flux and deposited energy spectra shape data obtained by Liulin type spectrometers on spacecraft (five different experiments) and aircraft since 2001 is performed with the aim of understanding how well these parameters can characterize the type of predominant particles and their energy in the near Earth radiation environment. Three different methods for characterisation of the incoming radiation from Liulin spectrometers are described. The results revealed that the most informative one is by the shape of the deposited energy spectra. Spectra generated by Galactic Cosmic Rays (GCR) protons and their secondaries are with linear falling shape in the coordinates deposited energy/deposited per channel dose rate. The position of the maximum of the deposited energy spectra inside the South Atlantic Anomaly (SAA) region depends on the incident energy of the incoming protons. Spectra generated by relativistic electrons in the outer radiation belt have a maximum in the first channels. For higher energy depositions these spectra are similar to the GCR spectra. Mixed radiation by protons and electrons and/or bremsstrahlung is characterized by spectra with 2 maxima. All type of spectra has a knee close to 6.2 MeV deposited energy, which correspond to the stopping energy of protons in the detector. Dose to flux ratio known also as specific dose is another high information parameter, which is given by experimentally obtained formulae [Heffner, J. Nuclear radiation and safety in space. M. Atomizdat. 115, 1971 (in Russian)] connecting the dose to flux ratio and the incident energy of the particles.     

辐射带AP9模式在南大西洋异常区的系统性量化评估

针对目前辐射带AP9模式量化评估不够系统的问题,基于F_10.7指数确定高、中、低太阳活动水平,以三种太阳活动水平条件下NOAA-15观测的140~500MeV的全向质子通量为参考数据,以南大西洋异常区为对比区域,定义边界吻合度和大小量级差为评估指标,将辐射带AP9模式分别与AP8模式和参考数据进行对比,对AP9模式进行系统性量化评估.结果表明,AP8和AP9模式均能重构出南大西洋异常区,但AP8模式重构的南大西洋异常区轮廓与观测结果更为吻合.平均而言,AP8和AP9模拟结果均比观测值高,AP8比AP9更接近观测值.太阳活动水平越低,AP9与观测之间的差距越小.     

Relativistic electron fluxes and dose rate variations during April–May 2010 geomagnetic disturbances in the R3DR data on ISS

Space radiation has been monitored successfully using the Radiation Risks Radiometer-Dosimeter (R3D) installed at the ESA EXPOSE-R (R3DR) facility outside of the Russian Zvezda module of the International Space Station (ISS) between March 2009 and January 2011. R3DR is a Liulin type spectrometer–dosimeter with a single Si PIN detector 2 cm² of area and 0.3 mm thick. The R3DR instrument accumulated about 2 million measurements of the absorbed dose rate and flux of 10 s resolution. The total external and internal shielding before the detector of R3DR device is 0.41 g cm⁻². The calculated stopping energy of normally incident particles to the detector is 0.78 MeV for electrons and 15.8 MeV for protons. After the Coronal Mass Ejection (CME) at 09:54 UTC on 3 April 2010, a shock was observed at the ACE spacecraft at 0756 UTC on 5 April, which led to a sudden impulse on Earth at 08:26 UTC. Nevertheless, while the magnetic substorms on 5 and 6 of April were moderate; the second largest in history of GOES fluence of electrons with energy >2 MeV was measured. The R3DR data show a relatively small amount of relativistic electrons on 5 April. The maximum dose rate of 2323 μGy day⁻¹ was reached on 7 April; by 9 April, a dose of 6600 μGy was accumulated. By the end of the period on 7 May 2010 a total dose of 11,587 μGy was absorbed. Our data were compared with AE-8 MIN, CRESS and ESA-SEE1 models using SPENVIS and with similar observations on American, Japanese and Russian satellites.     

地球磁层中合声波的频率与传播角分布特征

合声波的频率和传播角是影响其与电子相互作用的关键参数. 2013年1月1日至2015年12月31日期间范艾伦卫星数据的统计分析结果表明, 在传播角θ≈35°处, 较强的合声波(>7×10^–4 mV²·m^–2·Hz^–1)更倾向于出现在更窄的频率范围(0.3～0.4 f_ce). 随着磁壳数L的增大, θ≈35°处的合声波频谱变窄趋势逐渐明显. 从夜侧到晨侧(21:00 MLT－09:00 MLT), 较强的合声波能够在0.1～0.8 f_ce的频率范围内被观测到, 但夜侧θ≈35°处的合声波频谱宽度比晨侧更窄. 从上午到昏侧(09:00 MLT－21:00 MLT), 合声波电场功率谱密度明显降低, 且主要以斜传播(θ>60°)的下带合声波为主. 随着磁纬度λ_MLAT的增大, 上带合声波迅速减弱. 同时, θ≈35°处的下带合声波电场功率谱密度也逐渐下降. 本文揭示了不同区域内合声波强度的频率和传播角分布特征, 为构建更加精确的合声波–电子相互作用全球模型提供了重要信息.     

基于范艾伦卫星观测数据的地球辐射带电子能谱分布的统计分析

利用范艾伦卫星2014年至2018年观测的高精度电子能谱数据, 统计分析了不同辐射带高能电子能谱类型的时空分布特征. 结果表明, 辐射带电子能谱主要被分为三类: 指数分布能谱、幂律分布能谱和反转能谱. 指数分布能谱通常在等离子体层以外占主导地位. 幂律分布能谱通常在磁暴的主相出现在高L处, 并逐渐转移到低L处. 在地磁活动平静时期, 幂律分布能谱在高L处存在时间更长, 占比更多. 反转能谱在等离子体层内L>2.5处占主导地位, 随着等离子体层层顶升高, 反转能谱增加, 指数分布能谱减少. 在长时间的地磁活动平静年份, 辐射带电子反转能谱局地峰值(约2 MeV)附近的电子通量明显较低, 反转能谱占比较少. 辐射带电子能谱类型对等离子体层层顶和地磁活动依赖性的统计分析表明, 反转能谱发生率的峰值位置约位于L=(L_pp–2)(L_pp为等离子体层层顶位置), 指数分布能谱发生率的峰值约位于L=(L_pp+1.5), 幂律分布能谱的出现与电子的注入密切相关. 磁暴越剧烈, 反转能谱被指数分布能谱取代的L范围越广泛. 在平静时期, 由于等离子体嘶声的散射作用, 等离子体层层顶内的指数分布能谱被反转能谱取代. 本文给出了辐射带电子能谱类型长期的时空分布特征, 可以为辐射带动态建模和高能电子通量预报提供理论参考.     

外辐射带动态演化的粒子模拟研究

运用计算机实验方法即三维电磁粒子模拟方法初步研究了暴时扰动情况下外辐射带粒子环境的动态演化特性。模拟计算了暴时辐射带粒子环境的演化情况。模拟计算结果显示，高能质子、电子注入午辐射滞后，两者一方面沿磁力线做弹跳运动，向高纬扩展，部分注入质子和电子沉降于南北两极区域；另一方面，注入质子和电子还经历顺时针和逆时针方向的漂移运动，粒子能量越大，漂移速度越快。暴时多次注入引起整个辐射带粒子能量的大幅增强；粒子注入颗次和强度越大，辐射带粒子通量增幅越大。本项研究为开发研制完整的辐射带动态模式积累了有益的经验。     

载人航天器舱内辐射剂量及其预估

本文依据国内外95例空间飞行氟化锂热释光剂量计测量的舱内宇宙辐射剂量及轨道参数,建立了近地轨道载人航天器舱内剂量预先评估的数学模型。模型表明,影响舱内剂量水平的主要因素是轨道高度,呈二次曲线形式;其次是太阳活动因素。轨道倾角对舱内剂量的影响并不显著。依据模型作出了辐射安全飞行的时限曲线并就辐射的安全防护问题进行了分析讨论。     

低高度空间高能质子通量分布计算

介绍了AP-8模式、CRRESPRO模式和PSB97模式,并用这3种模式分别计算低高度空间300-1100km范围内的高能质子通量分布,由IDL软件绘出通量等值线图.AP-8模式通量主要受银河宇宙线调制,即受太阳活动直接影响,与太阳活动高年相比,太阳活动低年的质子通量较大;CRRESPRO模式中,因活动期和平静期的数据采集时间前后相差很短,从而使同一高度上两种环境条件下的通量分布相似.模式之间的比较结果表明,AP-8模式通量较小,CRRESPRO模式通量较大,PSB97模式通量介于二者之间,并与实测通量接近.PSB97是为低高度(1000km以下)定制的模式,在低高度上优于AP-8模式和CRRESPRO模式,能较好地计算当前条件下的低高度高能质子通量.     

Application of a modified generalized sail model on a solar sail with wrinkles

In this paper, we present an analysis of effect of wrinkles on the solar sail performance. We describe different analytical, semi-analytical and numerical approaches to the calculation of general large-scale curvature of a solar sail as well as parameters of so-called wrinkled domains, and introduce the impact of such wrinkles on the thrust and torque of the solar sail. Finally, we present a model of an optically-orthotropic surface for such non-ideal sail, providing a connection with the Generalized Sail Model, and other solar sail thrust models.     

三波长辐射温度计

采用辐射法测量物体表面真实温度的最大困难是被测材料表面的发射率难测。三波长辐射温度计能消除发射率对测温的影响,尤其是对抛光表面的测温。本文基于推导多波长辐射温度计的理论,推出了一种三波长辐射测温法的新关系式,并建立了三波长辐射温度计的数学模型。