空间机器人的目标捕获自适应控制

首先推导了基座姿态受控空间机器人系统运动学关系,得到了广义雅可比矩阵。根据目标的运动来规划机械臂末端在惯性空间的期望轨迹。对机器人动力学和运动学关系式进行线性参数比,分别对动力学待估参数和运动学待估参数设计在线修正律,在关节空间采用自适应控制。对于存在动力学参数不确知的机器人系统,算法保证了系统的渐近稳定,在成目标捕获任务的同时,控制基座姿态保持在期望范围之内。以平面两关节空间机器人系统为对象进行了仿真,结果表明了算法的可行性和有效性。     

月球引力转弯软着陆的制导控制研究

对于月球引力转弯软着陆过程 ,采用反馈线性化方法 ,对高度和速度信息分别设计了跟踪制导控制律 ,并应用微分几何的有关理论证明了这两种跟踪制导控制系统的李雅普诺夫稳定性。此外 ,根据软着陆系统推力、燃料和状态的约束条件 ,给出了引力转弯着陆过程初始条件的可达集合。最后给出的软着陆跟踪制导实例 ,只需要测得斜向距离、速度和姿态角度信息。这种制导方法测量简单 ,适于低成本的软着陆任务。     

小卫星的自适应姿态控制

分析了小卫星的姿态动力学及运动学方程；利用姿态动力学方程为一动力学参数矢量的线性函数这一事实，考虑存在参数不确定性，提出了一种自适应控制方法；证明了这种方法可以保证控制系统全局渐近稳定。仿真结果验证了该方法的有效性。     

基于GPS与磁强计组合的姿态确定

提出了一种基于信息融合的姿态确定方法用于姿态确定。利用星上的GPS接收机和磁强计两种敏感的测量，基于广义卡于尔曼滤波理论及信息融合理论，发展了基于此两种敏感器的全局最优融合估计算法。来确定卫星的姿态和姿态角速度。并对处法进行了设计和仿真，通过与单独使用GPS确定姿态的算法进行对比分析。结果验证了该算法进行对比分析，结果验证了该算法的优越性。     

防静电白色热控涂层的空间环境性能试验

通过在氧化锌晶格中掺入重金属离子，得到具有防静电功能的白色颜料，再以丙烯酸树脂为粘合剂制备出空间飞行器外表面用的ACR－1防静电白色热控涂层；研究了空间环境效应（包括紫外辐照，电子和质子辐照）对该热控涂层太阳吸收率的影响并与有机硅白色热控涂层进行了比较，地面模拟空间环境试验研究结果证明，ACR－1防静电白色热控涂层具有良好的空间稳定性。     

无人机舵面负载模拟系统的小脑模型控制

为解决无人机舵面负载模拟系统中非线性和多余力矩扰动问题,利用小脑模型神经网络非线性逼近能力强、结构简单、适于实时控制等特点,采用小脑模型和传统PD(Proportional-Derivative)控制结合的复合控制策略,由小脑模型实现前馈控制,PD控制实现反馈控制,以保证在系统运行各阶段的控制精度.分析讨论了复合控制的不稳定性问题,研究了基于可信度分配和学习率自适应调整的改进型小脑模型的应用情况,提出一种适用于单输入单输出系统的简化小脑模型复合控制设计方法.仿真结果表明该方法有效地解决了小脑模型和PD复合控制的不稳定问题,改善了系统动态加载性能,并具有很好的抗干扰性能.     

多径信道下图像的信源信道联合编码调制传输

针对多径衰落信道提出了一种基于小波变换并结合OFDM(Orthogonal Frequency Division Multiplexing)自适应调制的图像传输方法和信源信道联合带宽功率优化分配算法.给出了编码传输方法结构,对有噪信道下基于小波变换的图像编码传输实现和失真估计问题及多误码率OFDM自适应调制比特功率优化分配问题进行了建模和分析,使得信源量化编码与OFDM调制能够方便地结合起来,并进一步得到了相应的信源信道联合优化带宽功率分配方法.仿真和分析表明,该方法实现了多径信道下图像的信源信道联合编码调制传输,编解码复杂度和延迟小,且信源信道联合优化的带宽功率分配可有效提高信道资源利用效率.     

Using the radial basis function neural network to predict ionospheric critical frequency of F2 layer over Wuhan

Neural networks (NNs) have been applied to ionospheric predictions recently. This paper uses radial basis function neural network (RBF-NN) to forecast hourly values of the ionospheric F₂ layer critical frequency(f_oF₂), over Wuhan (30.5N, 114.3E), China. The false nearest neighbor method is used to determine the embedding dimension, and the principal component analysis (PCA) is used to reduce noise and dimension. The whole study is based on a sample of about 26,000 observations of f_oF₂ with 1-h time resolution, derived during the period from January 1981 to December 1983. The performance of RBF-NN is estimated by calculating the normalized root-mean-squared (NRMSE) error, and its results show that short-term predictions of f_oF₂ are improved.     

Comparison of ionospheric F2 peak parameters foF2 and hmF2 with IRI2001 at Hainan

Monthly median values of foF2, hmF2 and M(3000)F2 parameters, with quarter-hourly time interval resolution for the diurnal variation, obtained with DPS4 digisonde at Hainan (19.5°N, 109.1°E; Geomagnetic coordinates: 178.95°E, 8.1°N) are used to investigate the low-latitude ionospheric variations and comparisons with the International Reference Ionosphere (IRI) model predictions. The data used for the present study covers the period from February 2002 to April 2007, which is characterized by a wide range of solar activity, ranging from high solar activity (2002) to low solar activity (2007). The results show that (1) Generally, IRI predictions follow well the diurnal and seasonal variation patterns of the experimental values of foF2, especially in the summer of 2002. However, there are systematic deviation between experimental values and IRI predictions with either CCIR or URSI coefficients. Generally IRI model greatly underestimate the values of foF2 from about noon to sunrise of next day, especially in the afternoon, and slightly overestimate them from sunrise to about noon. It seems that there are bigger deviations between IRI Model predictions and the experimental observations for the moderate solar activity. (2) Generally the IRI-predicted hmF2 values using CCIR M(3000)F2 option shows a poor agreement with the experimental results, but there is a relatively good agreement in summer at low solar activity. The deviation between the IRI-predicted hmF2 using CCIR M(3000)F2 and observed hmF2 is bigger from noon to sunset and around sunrise especially at high solar activity. The occurrence time of hmF2 peak (about 1200 LT) of the IRI model predictions is earlier than that of observations (around 1500 LT). The agreement between the IRI hmF2 obtained with the measured M(3000)F2 and the observed hmF2 is very good except that IRI overestimates slightly hmF2 in the daytime in summer at high solar activity and underestimates it in the nighttime with lower values near sunrise at low solar activity.     

TC4钛合金的微动磨损及防护

对Ｔｉ－６Ａｌ－４Ｖ合金在１８℃，１００℃２５０℃下的微动磨损特性及防护工艺进行了研究。表明：该合金微动磨损的主要磨损形式是疲劳脱层，其磨损量随温度升高而下降，高渐微动磨损量与磨损区表面所形成的氧化层的性质及厚度有关。