光纤陀螺随机调制的理论分析及实验

偏置稳定性是描述陀螺性能的重要指标,而电路中的交叉干扰是导致陀螺输出漂移的重要原因.采用随机调制的方法能够减小陀螺中交叉干扰产生的输出漂移.采用快速傅立叶变换(FFT)的方法对方波调制和随机调制产生的交叉干扰进行了分析,分析结果表明,采用方波调制时,交叉干扰与方波同频,无法滤除,导致陀螺输出的偏置误差以及陀螺输出对光强的依赖性;而采用随机调制,交叉干扰与方波频率不同,能够滤除,从而减小交叉干扰带来的随机漂移.采用的随机调制为-3π/2,-π/2,π/2,3π/2调制,能够保证陀螺工作点在灵敏度最高的偏置点上,其频谱主要成分为方波基波的偶次谐波,通过陀螺电路中的滤波,能够将其滤掉,消除交叉干扰对陀螺输出带来的干扰.对方波调制和随机调制分别进行了实验,通过实验,证明了该方法的正确性,得到了随机调制能够抑制光纤陀螺中由于交叉干扰产生的输出漂移的结论.     

应用太阳帆悬停探测哑铃形小行星

研究了太阳帆航天器在哑铃形小行星引力场内的悬停探测可行性问题。哑铃形小行星代表了一类细长形的小行星,文中首先建立哑铃形小行星的简化动力学模型。针对可变反射面积的太阳帆,给出其在小行星引力场内的悬停动力学方程,并仿真求解了哑铃形小行星附近的太阳帆可行悬停探测区域。     

太阳帆推进任务的快速仿真方法

研究太阳帆的力学特性和轨道控制设计方法,导出太阳帆的无奇点控制律.提出通过STK中MATLAB语言编写的嵌入式脚本（Plug in Script）来将由控制律得到的光压力加速度矢量,添加到STK轨道计算力学模型中,从而进行轨道控制的方法.仿真结果表明,对于常规方法难以进行仿真分析的航天器动力学模型（如太阳帆）,所提出的方法能快速灵活地支持其相应的任务,并增强任务场景的可视化,从而实现利用STK丰富的功能特性进行复杂航天任务的设计、分析和验证.     

三维试验粒子轨道法在磁层粒子全球输运中的应用

根据磁层粒子动力学理论, 通过偶极磁场模型验证利用三维试验粒子轨道方法模拟近地球区(r < 8R_e)带电粒子运动特征的可靠性. 在此基础上, 以太阳风和磁层相互作用的全球MHD模拟结果为背景, 利用三维试验粒子轨道方法, 对非磁暴期间南向行星际磁场背景下太阳风离子注入磁层的情形进行数值模拟, 并对北向行星际磁场背景下太阳风离子注入极尖区以及内磁层的几种不同情形进行了单粒子模拟. 模拟结果反映了南向和北向行星际磁场离子向磁层的几种典型输入过程, 揭示出行星际磁场南向时太阳风粒子在磁层内密度分布的晨昏不对称性以及其在磁鞘和磁层内的大致分布, 并得出统计规律. 模拟结果与理论预测和观测结论相一致, 且通过数值模拟发现, 行星际磁场北向时靠近极尖区附近形成的非典型磁镜结构对于能量粒子经由极尖区注入环电流区域过程有重要的影响和作用.      

深空探测太阳电池阵应用及关键技术分析

从1958年启动月球探测活动至今,经过几十年的发展,人类在深空探测领域取得重大成果。本文首先介绍地内行星、地外行星与登陆探测等领域探测器用太阳电池阵技术的应用情况,同时结合地内行星探测、地外行星探测与登陆探测任务所面临的不同空间环境特点对航天器太阳电池阵进行关键技术分析,梳理深空探测任务对太阳电池阵不同的技术需求及其所需解决的关键问题,从中得出未来深空探测太阳电池阵技术的趋势是将向更高效率太阳电池阵、环境自适应技术、高重量比功率、高体积比功率的方向发展。     

Where does the heliospheric modulation of galactic cosmic rays start?

The long outstanding question of where the heliospheric (solar) modulation of galactic cosmic rays actually begins, in terms of spatial position, as well as at what high kinetic energy, can now be answered. Both answers are possible by using the results of an advanced numerical model, together with appropriate observations. Voyager 1 has been exploring the outskirts of the heliosphere and is presently entering what can be called the very local interstellar medium. It has been generally expected, and accepted, that once the heliopause is crossed, the local interstellar spectrum (LIS) should be measured in situ by the Voyager spacecraft. However, we show that this may not be the case and that modulation effects on galactic cosmic rays can persist well beyond the heliopause. For example, proton observations at 100 MeV close to the heliopause can be lower by ∼$\sim$25% to 40% than the LIS, depending on solar modulation conditions. It is also illustrated quantitatively that significant solar modulation diminishes above ∼$\sim$50 GeV at Earth. It is found that cosmic ray observations above this energy contain less that 5%$5\%$ solar modulation effects and should therefore reflect the LIS for galactic cosmic rays. Input spectra, in other words the very LIS, for solar modulation models are now constrained by in situ observations and can therefore not any longer be treated arbitrarily. It is also possible for the first time to determine the lower limit of the very LIS from a few MeV/nuc to very high energies.     

基于PWM_ON_PWM调制方式的控制力矩陀螺框架电机驱动控制

控制力矩陀螺框架电机驱动电路采用的脉宽调制方式不同,所产生的电机转矩脉动也会不同.针对无刷直流电机驱动的控制力矩陀螺框架系统,从换相期间转矩脉动、非换相期间转矩脉动及脉宽调制方式的应用改进3个方面对不同脉宽调制方式进行分析,得出采用PWM_ON_PWM方式的转矩脉动最小,适用于控制力矩陀螺框架系统的高精度控制要求.通过仿真验证了分析的正确性.     

太阳帆航天器被动姿态控制研究

针对由有效载荷、太阳帆和4个控制叶片所组成的太阳帆航天器系统,从物理模型出发,利用欧拉方程建立了姿态动力学模型,并通过数值仿真对太阳帆航天器基于控制叶片的对日定向性能进行了研究。研究结果表明,在行星际飞行中太阳帆航天器可以通过使控制叶片保持偏置来保持姿态稳定。     

Nickel Isotopic Composition and Nickel/Iron Ratio in the Solar Wind: Results from SOHO/CELIAS/MTOF

Using the Mass Time-of-Flight Spectrometer (MTOF)—part of the Charge, Elements, Isotope Analysis System (CELIAS)—onboard the Solar Heliospheric Observatory (SOHO) spacecraft, we derive the nickel isotopic composition for the isotopes with mass 58, 60 and 62 in the solar wind. In addition we measure the elemental abundance ratio of nickel to iron. We use data accumulated during ten years of SOHO operation to get sufficiently high counting statistics and compare periods of different solar wind velocities. We compare our values with the meteoritic ratios, which are believed to be a reliable reference for the solar system and also for the solar outer convective zone, since neither element is volatile and no isotopic fractionation is expected in meteorites. Meteoritic isotopic abundances agree with the terrestrial values and can thus be considered to be a reliable reference for the solar isotopic composition. The measurements show that the solar wind elemental Ni/Fe-ratio and the isotopic composition of solar wind nickel are consistent with the meteoritic values. This supports the concept that low-FIP elements are fed without relative fractionation into the solar wind. Our result also confirms the absence of substantial isotopic fractionation processes for medium and heavy ions acting in the solar wind.