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.     

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.     

中地球轨道高能电子辐射环境特性分析

采用中国中地球轨道卫星在太阳活动下降相到上升相的高能电子探测数据, 首次分析研究了该轨道高能电子环境的空间分布、通量强度、时序变化以及对地磁暴活动响应的特性. 结果表明, 中地球轨道高能电子的空间分布 范围稳定, 电子通量强度随能量升高而下降; 中地球轨道高能电子环境是 一个在不同时间尺度上剧烈变化的动态系统, 该系统可能间歇性地出现27天重 现性变化, 该系统变化受地磁暴事件调制, 但其对磁暴的响应呈现出非线性特征.     

On the practical exploitation of perturbative effects in low Earth orbit for space debris mitigation

This paper presents the results of a numerical evaluation of the natural lifetime reduction in low Earth orbit, due to dynamical perturbations. The study considers two values for the area-to-mass ratio, a nominal ratio which resembles a typical value of spacecraft in orbit today, and an enhanced ratio which covers the surface augmentation. The results were obtained with two orbit propagators, one of a semi-analytical nature and the second one using non-averaged equations of motion. The simulations for both propagators were set up similarly to allow comparison. They both use the solar radiation pressure and the secular terms of the geopotential ($J_2,J_4$ and $J_6$). The atmospheric drag was turned on and off in both propagators to alternatively study the eccentricity build up and the residual lifetime. The non-averaging case also covers a validation with the full 6?×?6 geopotential. The results confirm the findings in previous publications, that is, the possibility for de-orbiting from altitudes above the residual atmosphere if a solar sail is deployed at the end-of-life, due to the combined effect of solar radiation pressure and the oblateness of the Earth. At near polar inclinations, shadowing effects can be exploited to the same end. The results obtained with the full, non-averaging propagator revealed additional de-orbiting corridors associated with solar radiation pressure which were not found by previous work on space debris mitigation. The results of both tools are compared for specific initial conditions. For nominal values of area-to-mass ratio, instead, it is confirmed that this resonance effect is negligible.The paper then puts the findings in the perspective of the current satellite catalogue. It identifies space missions which are currently close to a resonance corridor and shows the orbit evolution within the resonances with a significantly shorter residual orbital lifetime. The paper finishes with a discussion on the exploitation of these effects with regards to the long-term simulation of the space debris environment and a flux and collision probability comparison.     

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.     

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.     

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.     

The effects of proton radiation on UHMWPE material properties for space flight and medical applications

Ultra High Molecular Weight Polyethylene (UHMWPE) is a polymer widely used as a radiation shielding material in space flight applications and as a bearing material in total joint replacements. As a long chain hydrocarbon based polymer, UHMWPE’s material properties are influenced by radiation exposure, and prior studies show that gamma irradiation is effective for both medical sterilization and increased wear resistance in total joint replacement applications. However, the effects of space flight radiation types and doses on UHMWPE material properties are poorly understood. In this study, three clinically relevant grades of UHMWPE (GUR 1020, GUR 1050, and GUR 1020 blended with Vitamin E) were proton irradiated and tested for differences in material properties. Each of the three types of UHMWPE was irradiated at nominal doses of 0 Gy (control), 5 Gy, 10 Gy, 20 Gy, and 35 Gy. Following irradiation, uniaxial tensile testing and thermal testing using Differential Scanning Calorimetry (DSC) and Dynamic Mechanical Analysis (DMA) were performed. Results show small but significant changes in several material properties between the control (0 Gy) and 35 Gy samples, indicating that proton irradiation could have a effect on the long term performance of UHMWPE in both medical and space flight applications.     

Highly Elliptical Orbits for Arctic observations: Assessment of ionizing radiation

The ionizing radiation environment was analyzed for a variety of potential Highly Elliptical Orbits (HEOs) with orbital periods ranging from 6 h to 24 h suitable to continuously monitor the Arctic region. Several models available from the ESA Space Environment Information System (SPENVIS) online tool were employed, including the new-generation AE9/AP9 model for trapped radiation. Results showed that the Total Ionizing Dose (TID) has a well-pronounced local minimum for the 14-h orbit, which is nearly identical to the overall minimum observed for the longest orbital period (24 h). The thickness of slab aluminum shielding required to keep the annual TID below 10, 5 and 3.33 krad (i.e. 150, 75 and 50 krad for 15 years of mission duration) for a 14-h orbit is 2.1, 2.7 and 3.1 mm respectively. The 16-h orbit requires an additional 0.5 mm of aluminum to achieve the same results, while the 24-h orbit requires less shielding in the order of 0.2–0.3 mm. Comparison between the AE8/AP8 and AE9/AP9 models was conducted for all selected orbits. Results demonstrated that differences ranged from −70% to +170% depending on orbit geometry.     

Properties of the high area-to-mass ratio space debris population at high altitudes

In the framework of its space debris research activities ESA established an optical survey program to study the space debris environment at high altitudes, in particular in the geostationary ring and in the geostationary transfer orbit region. The Astronomical Institute of the University of Bern (AIUB) performs these surveys on behalf of ESA using ESA’s 1-m telescope in Tenerife. Regular observations were started in 1999 and are continued during about 120–140 nights per year. Results from these surveys revealed a substantial amount of space debris at high altitudes in the size range from 0.1 to 1 m. Several space debris populations with different dynamical properties were identified in the geostationary ring. During the searches for debris in the geostationary transfer orbit region a new population of objects in unexpected orbits, where no potential progenitors exist, was found. The orbital periods of these objects are clustered around one revolution per day; the eccentricities, however, are scattered between 0 and 0.6. By following-up some of these objects using the ESA telescope and AIUB’s 1-m telescope in Zimmerwald, Switzerland, it was possible to study the properties of this new population. One spectacular finding from monitoring the orbits over time spans of days to months is the fact that these objects must have extreme area-to-mass ratios, which are by several orders of magnitudes higher than for ‘normal-type’ debris. This in turn supports the hypothesis that the new population actually is debris generated in or near the geostationary ring and which is in orbits with periodically varying eccentricity and inclination due to perturbations by solar radiation pressure. In order to further study the nature of these debris, multi-color and temporal photometry (light curves) were acquired with the Zimmerwald telescope. The light curves show strong variations over short time intervals, including signals typical for specular reflections. Some objects exhibit distinct periodic variations with periods ranging from 10 to several 100 s. All this is indicative for objects with complicated shapes and some highly reflective surfaces.     

带电粒子云的演变过程

根据带电粒子云从破碎点开始向空间扩散过程中粒子云密度和形状的变化规律,以几何形状和起主要作用的因素为特征,定义了球形、椭球形、绳形、螺旋线形、全方位弥漫直至球壳形6个演变阶段.论述了在各个阶段的主要特征和对演变过程起主要作用的因素.分析了在各个阶段电磁场对带电粒子的摄动影响,比较了带电粒子云与不带电粒子云在演化过程上的差异.在球形阶段起主要作用的是分离速度,带电碎片之间的排斥力加快了碎片扩散的速度.从椭球形阶段到球壳形阶段,带电粒子和不带电粒子的演化规律基本一致.带电粒子的演化过程加快或减慢取决于粒子带正电或带负电.将电场摄动力等效于改变地球引力的大小,罗列了阶段转换标志点时刻的计算公式.利用计算机仿真的方法,给出了各个阶段不带电碎片云和带电碎片云分布示意图,验证了演变过程阶段划分和电磁场摄动分析的合理性.     

Active debris removal of multiple priority targets

Today’s space debris environment shows major concentrations of objects within distinct orbital regions for nearly all size regimes. The most critical region is found at orbital altitudes near 800 km with high declinations. Within this region many satellites are operated in so called sun-synchronous orbits (SSO). Among those, there are Earth observation, communication and weather satellites. Due to the orbital geometry in SSO, head-on encounters with relative velocities of about 15 km/s are most probable and would thus result in highly energetic collisions, which are often referred to as catastrophic collisions, leading to the complete fragmentation of the participating objects. So called feedback collisions can then be triggered by the newly generated fragments, thus leading to a further population increase in the affected orbital region. This effect is known as the Kessler syndrome.     

空间碎片减缓措施及其研究对策

随着人类空间技术的进步和发展 ,每年发射进入太空的人造天体越来越多。当这些人造天体失效后 ,由于目前人类对其缺乏及时有效的回收手段 ,随着时间的推移 ,堆积在太空中的废弃物将越来越多 ,总有一天人类再也不能向太空中发射任何人造天体。因此为了合理利用和保护有限的太空资源 ,则必须减少或清除太空垃圾。文章正是基于上述目的 ,在人类尚无有效回收手段的情况下 ,考虑利用现有的技术提出一些空间碎片的减缓措施 ,并在此基础上提出中国对空间碎片减缓应采取的对策