航天器相对运动水滴型悬停轨道研究

对航天器相对运动的C-W方程进行了分析,提出了航天器相对运动轨道设计中的一种水滴型悬停轨道,能够实现航天器相对空间目标在一定范围内进行悬停,并且只需使用脉冲速度增量控制即可实现长时间的悬停。文章对悬停轨道的悬停周期与目标航天器轨道参数和悬停位置的关系,以及悬停控制所需的速度增量ΔV进行了分析,给出了进行悬停轨道选择及设计的工程方法,并对C-W方程的状态转移矩阵进行了推导,得到了由常规的后方伴飞轨道使用脉冲速度控制方案进入目标星正下方的悬停位置的初始速度增量、转移时间及末端速度增量。根据分析结果,水滴型悬停轨道有利于工程实现,其设计方法可以应用于航天器在轨服务、侦察、巡视等任务的轨道设计。     

“高分五号”全谱段相机可展开定标漫反射板设计

为了对"高分五号"卫星全谱段光谱成像仪的太阳反射谱段辐射性进行长期监测与校正,并针对其谱段范围宽、精度要求高、口径大、使用寿命长等特点与要求,优化设计了可展开的漫反射板进行全光路全视场的辐射定标。定标漫反射板安装在相机光学系统的前端侧面,不影响相机正常成像,在定标时通过驱动机构展开漫反射板到相机前端,根据"高分五号"卫星轨道特点、定标能量要求及相机安装矩阵等设计定标漫反射板展开角度为39°。研制了430 mm×430 mm大尺寸聚四氟乙烯漫反射板组件以保证在展开时满足全光路全视场的定标,漫反射板在420～2 400 nm光谱范围内半球反射率高于95%,在相机观测方向BRDF变化优于2.5%。同时,设计了漫反射板稳定性监视辐射计用于监测漫反射板在轨性能衰减,监测精度1.5%。在轨定标精度分析为4.76%,满足指标要求。     

基于GA-PSO的低轨星座传感器资源优化调度方法

针对低轨星座目标跟踪传感器资源调度,基于函数优化和组合优化理论,建立了传感器资源优化调度模型,并设计了基于遗传算法-粒子群优化(GA-PSO)的优化调度算法。仿真结果表明,与现有的构造优化调度算法相比,该算法的性能更优,但运算量有所增加。     

基于北斗GEO卫星双频观测值连续监测电离层延迟

利用北斗GEO卫星观测数据直接计算电离层延迟。由于GEO卫星具有固定穿刺点和静地的特性,使得观测站监测电离层变化时可不考虑空间变化,并可进行连续不间断监测。通过分析北斗GEO卫星三种频率码伪距和载波相位观测值不同组合,选取B1&B2双频计算电离层延迟为最优组合,采用相位平滑伪距的方法计算电离层延迟TEC,相较其他电离层模型,该方法的优点是不会引入模型误差,可得到连续的高精度的电离层延迟监测结果。     

NPF算法在X射线脉冲星导航中的应用研究

针对X射线脉冲星导航中航天器模型的强非线性、高阶模型不确定性等问题,提出应用非线性预测滤波(NPF)算法实时估计航天器的轨道信息。首先,建立具有模型不确定性的X射线脉冲星导航定轨指标函数,优化得到满足指标函数最小的系统模型误差值,通过降低模型不确定性的影响来提高航天器自主定轨精度。对STK生成的“火星探路者”和“金星快车”及“北斗一号”三种航天器轨道数据进行分析,仿真结果表明,该算法比EKF算法具有更高的定轨精度,能够满足深空以及近地轨道航天器的自主定轨精度指标要求。     

Influence of time variable geopotential models on precise orbits of altimetry satellites,global and regional mean sea level trends

During the last decade a significant progress has been reached in the investigation of the gravity field of the Earth. Besides static, also time variable geopotential models have been recently created. In this paper we investigate the impact of the recent time variable geopotential models on altimetry satellite orbits and such altimetry products based on these orbits, as global and regional mean sea level trends. We show that the modeling of time variable gravity improves the orbit solutions, at least for the GRACE period where time variable gravity is sufficiently accurately observed by this mission. Our analysis includes six geopotential models jointly developed by GFZ German Research Centre for Geosciences and Space Geodesy Research Group (CNES/GRGS) Toulouse: the stationary model EIGEN-GL04S, a stationary version of EIGEN-6S (EIGEN-6S_stat), a corrected version of EIGEN-6S and three enhanced versions of EIGEN-6S called EIGEN-6S2, EIGEN-6S2A and EIGEN-6S2B. By “stationary” we mean “containing periodic parameters such as annual and semi-annual variations, but no secular (drift) terms”. We computed precise orbits for the radar altimetry satellites ERS-1, ERS-2, TOPEX/Poseidon, and Envisat over 20 years between 1991 and 2011. The orbit, single-mission and multi-mission altimetry crossover analyses show that the time variable models EIGEN-6S_corrected, EIGEN-6S2 and its two precursors EIGEN-6S2A/B perform notably better than the stationary models for the GRACE period from 2003 onwards. Thus, using EIGEN-6S2 and EIGEN-6S2A/B we have got 3.6% smaller root mean square fits of satellite laser ranging observations for Envisat, as when using EIGEN-GL04S. However, for the pre-GRACE period 1991–2003, the stationary geopotential models EIGEN-GL04S and EIGEN-6S_stat as well as EIGEN-6S2 having no drift terms for degree 3–50 at this time interval perform superior compared to EIGEN-6S_correct and EIGEN-6S2A/B which contain drifts for this period. We found, that the time variable geopotential models have a low (0.1–0.2 mm/yr) impact on our results for the global mean sea level trend. However, we found strong East/West differences up to 3 mm/yr in the regional mean sea level trends when using orbits of all four satellites based on time variable and stationary geopotential models. We show that these differences are related to the relative drifts of the centers-of-origin between the orbit solutions based on the time variable and stationary geopotential models. From the results of our detailed study, we conclude that the final version of the time variable gravity field model EIGEN-6S2 performs best for the four satellites tested. This model provides the most reliable and mission-consistent sea level estimates for the whole time period from 1992 to 2010. This model is of maximum spherical harmonic degree and order 260 and contains time series for drifts as well as annual and semiannual variations of the spherical harmonic coefficients for degree 2–50.     

深空通信中继下行链路特性研究及仿真分析

在深空通信中,由于信号传输距离遥远,功率受限的下行链路信号衰减巨大。为解决上述问题,分析地球大气层和外层自由空间的传输特性差异,提出以地球同步轨道卫星为中继站的下行链路的构想,根据每一段链路特性的不同选择载波频率。仿真结果表明,中继链路可以提高信号传输的信噪比、增大信道容量、降低误码率,提高了深空通信下行链路的可靠性。     

在轨地球同步卫星地球敏感器干扰及指向计算

从工程应用角度,基于太阳、月球位置和卫星轨道根数推导了太阳和月球对地球同步轨道卫星红外地球敏感器干扰的计算公式及预报方法,同时给出了安全模式下卫星Z轴跟踪太阳时星上天线指向变化的计算模型。计算结果和卫星下传遥测数据验证了方法的正确性,可用于实际卫星管理。     

利用摆动地球敏感器两个探测器输出的姿态确定

摆动地球敏感器是地球同步通信卫星控制系统的重要部件。这种敏感器主要用于卫星的姿态测量,测量量作为控制系统的输入信号计算控制输出量。摆动地球敏感器有4个探测器,目前在轨卫星的基本使用方法均为至少使用3个探测器的测量信息进行姿态确定。本文给出了使用2个探测器测量确定卫星姿态的计算方法,并结合实际情况给出了使用策略。这种姿态确定方法大大拓宽了地球敏感器的使用范围,增加了地球敏感器的冗余性,延长了部件的使用寿命。     

一种有摄初轨计算的单位矢量法

根据单位矢量法测轨原理，在人造卫星轨计算的单位矢量法（ＵＶＭ１）的基础上，给出了利用人造地球卫星观测资料测定有摄初轨的一种方法（ＰＵＶＭ１。本方法既适用于测角资料，也适用于测距资料和测速资料，以及这些没类型资料的和种组合；适用于任意偏心率，任意轨道倾角的人造地球卫生；有利于提高初轨测定精度，并改善整个计算过程的收敛性