基于矢量磁强计的磁场梯度张量仪误差校正方法

卫星在轨运行时,本体会产生一定的磁干扰,一般通过伸杆将传感器远离卫星本体安装,或者通过多个磁场传感器测量磁场梯度的方法来消除卫星本体的磁干扰.使用磁场梯度张量仪测量磁场梯度时,张量仪本身的构型会给测量带来误差.通过对5种主要的张量仪构型进行误差仿真,对比5种构型的张量测量误差,发现十字形构型张量仪的测量误差最小.除了构型带来的误差,张量仪的主要测量误差还包括组成张量仪的三轴磁强计本身的误差和非对准误差.本文使用椭球拟合算法对磁强计本身的误差进行校正,校正后磁强计测量总场的均方根误差为0.864nT.针对张量仪的非对准误差,提出了正交系间非对准误差的校正方法.仿真结果表明,校正后的非对准角度误差≤3.2×10-5 rad,能够很好地降低张量仪的非对准误差.      

卫星磁部件分布对梯度法消除剩磁的影响分析

在工程实施中双探头梯度法的误差系数只能达到0.5~0.3,意味着只能消除50%~70%的卫星剩磁干扰。文章研究双探头梯度法消除卫星本体剩磁的原理和工程上双探头梯度法的误差来源,并分析了卫星剩磁部件的分布对磁心的影响,以及磁心与双探头位置的关系在双探头梯度法中的关键作用。当磁心位置确定,并且双探头安装连线通过磁心,双探头梯度法的处理误差能够实现最小化。仿真试验表明,在优化剩磁部件分布和双探头部署位置的情况下,双探头梯度法的误差系数可以从0.4降低到0.03以下。     

多点磁场协同探测反演电离层电流密度

相对于传统的单点磁场探测,多点磁场协同探测可以同时获得各测点磁场,消除探测磁场随时间的变化,能更好地计算空间电流密度.根据由多点磁场反演计算空间电流密度的计算方法,开展数值仿真,分析卫星编队数量、卫星编队构型、卫星定位偏差、卫星姿态测量误差、磁场测量误差、外部磁场强度及外部电流密度等对电流反演误差的影响.仿真结果表明,5星编队优于4星编队.在5星编队条件下,卫星姿态测量误差、卫星编队构型和外部磁场强度是反演误差的主要来源.根据仿真结果,当卫星姿态误差为0.001°,卫星编队尺度约为100km时,赤道区域电流密度的反演相对误差约为24%.      

地基伪卫星系统多址测距误差的校正算法

相对于卫星导航,地基伪卫星与接收机距离较近,测距中不涉及电离层传播等误差,易实现高精度测距和定位。但由于地基伪卫星位置固定,在信号连续发射模式下伪卫星信号间的多址干扰(MAI)会引起相对恒定的测距误差,针对地基伪卫星系统这一特点,提出一种基于反馈串行干扰抵消(SIC)的测距算法。首先对全部伪卫星信号进行捕获跟踪和功率估计,然后通过串行干扰抵消算法降低强功率伪卫星信号对期望测距信号的干扰,通过反馈模式进一步提高干扰抵消算法的性能。仿真结果表明,该方法可有效改善地基伪卫星系统强远近效应区域内的测距性能,不考虑其他误差下在强远近效应区域内基于码环可将伪卫星测距性能从10 m以上降低到约0.3 m。     

编队卫星空间状态参数估计量对ATI测速精度影响

基于对影响沿航向干涉(ATI)测速精度的特征量分析,建立了卫星空间状态参数估计量与ATI测速精度特征量,特征量与测速的关联数学模型。仿真给出了不同场景设置下的特征量精度、误差传播矩阵和测量误差传递关系的精度影响因子,以及最终空间状态参数估计量对测速精度的影响。     

对失效卫星特征点的自适应位姿跟踪控制

为满足对失效卫星上某个特征点位置悬停的同时使追踪星上敏感器指向该特征点,展开了对失效卫星特征点与追踪星间相对动力学建模与控制的研究。在追踪星本体坐标系下建立了六自由度相对位姿动力学模型,并结合失效卫星上特征点的运动规律,给出追踪星的期望跟踪位置和期望跟踪姿态。考虑到追踪星质量、转动惯量、系统所受扰动力、扰动力矩及失效卫星转动惯量的不确定性,设计了复合自适应位姿跟踪控制律,并通过Lyapunov法证明了闭环系统稳定性。对输出受限情况,采取设计控制参数调节过程及输出限幅措施。在仿真条件下,系统在自适应控制律下能够以位置误差约1cm、姿态误差约0.01°完成位姿跟踪任务;增大不确定参数偏差后,位置跟踪误差增至约7cm,姿态误差增至约0.1°;对控制参数进行调节后,可在不影响跟踪精度的条件下在指定范围内限制输出幅值,将幅值限制在指定范围内,并减小控制所需冲量的9%和冲量矩的30%。     

中国地区MAGSAT卫星标量和矢量磁异常图

使用MAGSAT卫星资料,编绘中国及邻近地区的卫星磁异常图(10°N—60°N,70°E—140°E)。为了提取地壳异常场,必须从观测资料中消除主磁场、磁层场,感应场和电离层场。本文选用GSFC(12/83)地磁场模型,消除主磁场,磁层场和感应场。为了进一步消除电离层场的影响,改善相邻轨道磁异常的一致性,用纬度的二次多项式拟合每一条轨道的初始地壳异常,并从初始地壳磁异常值减去这一拟合值,从而获得最后的地壳异常值(△X,△Y,△Z,△F)。把研究地区分成1°×1°的网格,将每个网格内的磁异常进行平均,以获得网格中心点的异常值。根据这些网点值绘制中国及邻近地区的卫星标量和矢量磁异常图。等值线间隔为2nT。为了检验卫星磁异常图的可靠性,将卫星资料分成黎明组、黄昏组和联合组,分别进行处理和绘制卫星磁异常图。结果表明:根据上述资料绘制的卫星磁异常图有很好的一致性。中国地区的卫星磁异常值位于—10nT—10nT。卫星磁异常与区域构造特征有较好的一致性;塔里木地台、扬子地台和中朝地台是正磁异常区,西藏高原是负磁异常区。卫星磁异常反映出下地壳磁化强度的横向不均匀性。     

利用GNSS反射信号载波测量湖面高度变化

给出一种利用导航卫星反射信号的载波相位测量光滑湖面高度变化的方法.首先建立载波相位观测方程,通过在直射与反射信号的观测量之间求单差,再在历元间求双差的方法,消除了大量误差并得到了直射与反射信号的几何路径差;然后根据各颗卫星的观测值和高度角等信息计算出湖面高度变化,并把各卫星得到的湖面高度度变化值进行加权平均以提高测量系统的精度和可靠性.仿真验证了方法在-15dB信噪比下达到了毫米级的测量精度.     

利用TIE-GCM模式计算电离层电流及夜间电离层磁场

电离层电流产生的磁场是地磁场卫星测绘时需要剔除的干扰源.利用电离层热层模式TIE-GCM计算电离层中的中性风、重力驱动和压强梯度等形成的电离层电流的全球分布,分析电流在特定位置产生的磁场及磁场三分量随纬度的变化规律.结果表明,E层尤其是磁赤道和极区的电流密度较大,可达103nA·m-2量级,F层电流密度量级约为10nA·m-2.在磁静日（Kp≤ 1）夜间22:00LT-04:00LT,电离层电流在中低纬度（南北纬50°之间）产生的磁场量级为几个nT,且磁场的南北向分量和径向分量基本大于东西向分量.通过与CHAMP卫星磁测数据分析比较,发现TIE-GCM模式计算电离层干扰磁场在中低纬度可以取得较好的结果,但在高纬度地区的效果不理想,还需进一步改进模式以提高计算精度.      

编队飞行小卫星群的相对自主定轨算法研究

针对有参考星的编队飞行小卫星群的自主位置保持 ,研究了基于星间测距的主从星相对自主定轨的可行性及其算法。考虑突发测量噪声对算法稳定性的影响 ,在迭代EKF算法中引入弱化因子 ,对误差较大的观测量实施“软删除” ,相比抗差Kalman滤波 ,性能稳定、额外计算量小、适于星载实现。仿真表明 ,无摄动运动下的相对定轨误差可控制在 0 1m左右 ;J2 项摄动的情况下的相对定轨误差约为 2m。     

Impact of the orbital eccentricity on the attitude performance before and after the deorbiting phase for Alsat-1

Due to the presence of periodic forcing terms in the gravity gradient torque, orbit eccentricity may produce large response for the roll, yaw and pitch angles. This paper investigates the influence of the orbit eccentricity on the performance of the attitude determination and control subsystem (ADCS) pointing of passive Low Earth Orbit (LEO) satellites stabilized by a gravity gradient boom or having long appendages before and after the deorbiting operation. The contribution of this work is twofold. First, the satellite attitude dynamics and kinematics are modeled by introducing the orbit eccentricity in the equations of motion of a LEO satellite in order to provide the best scenario in which satellite operators can keep the nominal functionality of LEO satellites with a gravity gradient boom after the deorbiting operation. Second, a Quaternion-based Extended Kalman Filter (EKF) is analyzed when the orbit eccentricity is considered in order to determine the influence of this disturbance on the convergence and stability of the filter. The simulations in this work are based on the true parameters of Alsat-1 which is a typical LEO satellite stabilized by a gravity gradient boom. The results show that the orbit eccentricity has a big influence on the pointing system accuracy causing micro-vibrations that affect the geocentric pointing particularly after the deorbiting phase. In this case, satellites have no orbital correction option. The Quaternion-based Extended Kalman Filter analyzed in this paper, achieved satisfactory results for eccentricity values less than 0.4 with respect to pointing system accuracy. However, singularities were observed for eccentricity values greater than 0.4.     

Science objectives of the magnetic field experiment onboard Aditya-L1 spacecraft

The Aditya-L1 is first Indian solar mission scheduled to be placed in a halo orbit around the first Lagrangian point (L1) of Sun-Earth system in the year 2018–19. The approved scientific payloads onboard Aditya-L1 spacecraft includes a Fluxgate Digital Magnetometer (FGM) to measure the local magnetic field which is necessary to supplement the outcome of other scientific experiments onboard. The in-situ vector magnetic field data at L1 is essential for better understanding of the data provided by the particle and plasma analysis experiments, onboard Aditya-L1 mission. Also, the dynamics of Coronal Mass Ejections (CMEs) can be better understood with the help of in-situ magnetic field data at the L1 point region. This data will also serve as crucial input for the short lead-time space weather forecasting models.The proposed FGM is a dual range magnetic sensor on a 6?m long boom mounted on the Sun viewing panel deck and configured to deploy along the negative roll direction of the spacecraft. Two sets of sensors (tri-axial each) are proposed to be mounted, one at the tip of boom (6?m from the spacecraft) and other, midway (3?m from the spacecraft). The main science objective of this experiment is to measure the magnitude and nature of the interplanetary magnetic field (IMF) locally and to study the disturbed magnetic conditions and extreme solar events by detecting the CME from Sun as a transient event. The proposed secondary science objectives are to study the impact of interplanetary structures and shock solar wind interaction on geo-space environment and to detect low frequency plasma waves emanating from the solar corona at L1 point. This will provide a better understanding on how the Sun affects interplanetary space.In this paper, we shall give the main scientific objectives of the magnetic field experiment and brief technical details of the FGM onboard Aditya-1 spacecraft.     

捕风一号卫星总体设计与技术特点

捕风一号卫星是中国首次实现基于星载导航卫星反射信号测量(global navigation satellite system-reflection,GNSS-R)技术的气象卫星,采用新型L波段海面风场信息探测技术,在风场测量、海面飓风风速反演等方面为国家气象、防灾减灾等行业提供服务.从系统设计角度介绍了捕风一号卫星的总...     

Jitter reduction of a reaction wheel by management of angular momentum using magnetic torquers in nano- and micro-satellites

Nowadays, nano- and micro-satellites, which are smaller than conventional large satellites, provide access to space to many satellite developers, and they are attracting interest as an application of space development because development is possible over shorter time period at a lower cost. In most of these nano- and micro-satellite missions, the satellites generally must meet strict attitude requirements for obtaining scientific data under strict constraints of power consumption, space, and weight. In many satellite missions, the jitter of a reaction wheel degrades the performance of the mission detectors and attitude sensors; therefore, jitter should be controlled or isolated to reduce its effect on sensor devices. In conventional standard-sized satellites, tip-tilt mirrors (TTMs) and isolators are used for controlling or isolating the vibrations from reaction wheels; however, it is difficult to use these devices for nano- and micro-satellite missions under the strict power, space, and mass constraints. In this research, the jitter of reaction wheels is reduced by using accurate sensors, small reaction wheels, and slow rotation frequency reaction wheel instead of TTMs and isolators. The objective of a reaction wheel in many satellite missions is the management of the satellite’s angular momentum, which increases because of attitude disturbances. If the magnitude of the disturbance is reduced in orbit or on the ground, the magnitude of the angular momentum that the reaction wheels gain from attitude disturbances in orbit becomes smaller; therefore, satellites can stabilize their attitude using only smaller reaction wheels or slow rotation speed, which cause relatively smaller vibration. In nano- and micro-satellite missions, the dominant attitude disturbance is a magnetic torque, which can be cancelled by using magnetic actuators. With the magnetic compensation, the satellite reduces the angular momentum that the reaction wheels gain, and therefore, satellites do not require large reaction wheels and higher rotation speed, which cause jitter. As a result, the satellite can reduce the effect of jitter without using conventional isolators and TTMs. Hence, the satellites can achieve precise attitude control under low power, space, and mass constraints using this proposed method. Through the example of an astronomical observation mission using nano- and micro-satellites, it is demonstrated that the jitter reduction using small reaction wheels is feasible in nano- and micro-satellites.     

近地球赤道面轨道上磁性刚体卫星的混沌运动

讨论地球磁场中非自旋磁性刚体卫星在近赤道平面圆轨道上平面天平动的混沌问题.利用Melnikov方法预测出现混沌的可能性并数值验证混沌的存在性.研究表明地球磁场的周期扰动能引起卫星的混沌运动,扰动增大则混沌加强.      

相位差法测量磁传感器阵列的非平行度

随着磁传感器技术及磁测技术的发展,通过测量磁梯度张量进行磁探测及磁定位已成为磁探领域的新方法。但在磁梯度张量测量过程中,由于机械安装的误差导致的磁传感器阵列中各传感器的磁轴的不平行将会极大的降低磁定位的精度。本文提出了一种易于实现的磁传感器阵列非平行度测量方法--相位差法,并通过试验验证了其有效性。     

基于改进Faster R-CNN的失效卫星部件检测方法

基于光学图像对失效卫星部件的精确检测可以为失效卫星的定位与捕获等任务提供支撑。然而,失效卫星部件多为密集小目标,且其光照条件变化较大,这导致一般主干网络出现特征表征分辨率低、小目标漏检等问题。针对上述问题,提出了一种基于改进Faster R-CNN的失效卫星部件检测方法。首先,该方法在Faster R-CNN的基础上,融合高分辨网络构建新的特征提取主干网络,以获得可靠、高分辨率的特征表达式。其次,在模拟真实空间环境的条件下,利用1∶1的嫦娥卫星模型构建了一个信息丰富的失效卫星数据集。用该数据集进行验证,结果表明：该方法的平均精度为93.6%,与Faster R-CNN和Cascade R-CNN相比,对小部件检测的准确率与召回率分别平均提高了9.8%与5.4%。该方法可有效检测失效卫星部件。     

背景太阳风数值模拟的熵守恒格式

背景太阳风研究是根据行星际扰动传播情况预测空间天气状况的基础,磁流体（MHD）模拟是背景太阳风研究的重要手段.采用一种新的数值计算方式,利用Ideal GLM-MHD将计算过程中产生的磁场散度以c_h的速度向计算区域外传播,从而消去磁场散度;重构部分使用受约束的最小二乘法,将磁场散度作为约束条件添加到重构中,进一步对重构后的磁场梯度进行修正;通量计算采用满足热力学第二定律的熵守恒格式,该格式能够确保在计算过程中熵不增,保证数值稳定.研究结果表明,该方法应用于太阳风数值模拟的求解得到了更加稳定的结果.