电静液作动器自调节积分鲁棒运动控制

针对电静液作动器系统中存在的匹配干扰及不匹配干扰,基于扩张状态观测器,设计了一种自调节积分鲁棒控制方法。首先设计扩张状态观测器估计系统的匹配不确定性并且进行前馈补偿;然后设计自调节积分鲁棒控制器分别处理系统的不匹配干扰和状态估计误差,实现了电静液作动器的渐近跟踪控制;最后通过仿真验证了该控制方案的有效性。结果表明：相较于传统的PID控制器,该控制器的跟踪误差约为0.2mm,控制精度达到0.4%左右。     

基于扩张状态观测器的永磁同步电机自抗扰无源控制

针对传统永磁同步电机滑模控制存在的抖振以及系统抗扰动鲁棒性差问题,提出一种基于扩张状态观测器的永磁同步电机自抗扰无源控制方法。转速外环设计自适应滑模控制器,采用扩张状态观测器对系统干扰项进行观测,用其进行前馈补偿。电流内环将无源控制与自抗扰控制相融合,得到dq旋转坐标系下的电压给定。新型控制方法可有效抑制系统抖振,增强系统鲁棒性。试验结果验证了所提控制方法的有效性和实用性。     

基于自适应方法的多无人机编队队形控制

针对"长机-僚机"近距编队队形因风场扰动而不能保持期望队形的问题,首先,提出了一种自适应队形保持控制的方法,该方法可用于抵消因风场不确定性对无人机的横侧向和前行方向所产生的距离误差,同时能够保持无人机编队稳定飞行。其次,由于风场的不确定性会引起"长机-僚机"之间的动力学发生变化,因此设计了一种基于"长机-僚机"相对运动模型的自适应控制律用以估计风场在3个方向的大小,进而控制无人机之间的相对运动以消除风场不确定性所产生的距离误差并保持速度的一致性,最终实现保持期望的队形。再次,通过构建合理的李雅普诺夫函数,证明无人机编队在风场干扰下能够保持编队稳定飞行,同时"长机-僚机"之间相对横向、横侧向以及纵向的距离误差均接近零。最后,通过仿真验证：所提出的自适应控制方法具有良好的鲁棒性,这为工程实践提供理论依据。     

火星电离层探测

火星已经成为深空探测的重要目标之一, 登陆火星并在火星生存是人类探测火星的终极目标, 因此电离层是必须了解的火星电磁环境. 火星电离层探测包括直接探测和间接探测. 直接探测精度高, 有较高的空间分辨率, 但是观测时间短, 无法提供长期稳定的探测结果. 对火星电离层的间接探测结果主要来自无线电掩星探测和顶部雷达探测. 无线电掩星探测可实现对火星电离层整个电子密度剖面的长期稳定探测, 但其空间水平分辨率较低, 且可探测的电离层太阳天顶角范围受到地球与火星轨道的限制. 顶部雷达探测对火星电离层的探测具有很高的时间分辨率和空间分辨率, 且同样可进行长期稳定探测, 为火星电离层研究提供了最新的支持. 通过对火星电离层探测的基本方法及典型观测结果的分析, 提出通过几种探测方法适当结合的方式, 同时对火星电离层进行观测, 能够大大推进对火星电离层的研究.      

转动壳体行波振动的有限元分析方法

转动壳体由于离心力与哥氏力的影响 ,其振动频率随转速变化 ,并且同一振型对应两个不同频率的前、后行波。本文给出了用有限元法计算转动壳体的有限元公式 ,用 MSC/ NASTRAN的 DMAP语言编制了形成哥氏力矩阵与离心刚度矩阵的程序 ,并将计算结果与实验进行了对比     

基于互联网的导航定位增强信息大规模实时播发研究

在卫星导航系统中，可通过注入增强信息的方法提高导航定位精度、可靠性和完好性。导航定位增强信息一般由卫星播发，通过互联网播发导航定位增强信息是近期一个新的研究热点。本文综述了互联网播发技术的研究现状，提出了一个基于互联网的导航定位增强信息大规模实时播发系统模型，采用基于对等网络技术、具有自组织特性的分层混合结构覆盖网络，有效降低了系统构建和管理的复杂性。论文还分析了导航定位增强信息播发的实时性和安全性需求，并提出了解决思路。     

应用端部效应改善的LS+NN模型进行日长变化预报

现有ΔLOD(Delta Length-Of-Day,日长变化)预报模式在进行周期项与残差项拟合分离时,通常没有考虑LS(Least Squares,最小二乘)拟合序列的端部效应,预报精度难以取得较大提高。针对端部效应现象,首先采用时间序列分析模型在ΔLOD序列两端进行数据延拓,构成一个新序列,然后用新序列求得LS外推模型系数,再结合LS外推模型和NN(Neural Network,神经网络)对原始ΔLOD序列进行预测。算例表明,在ΔLOD序列两端增加延拓数据,能有效改善LS拟合序列的端部效应;端部效应改善的LS+NN模型的预报精度明显优于常规LS+NN模型,精度最大提高了17.86%。该方法不仅适用于LS+NN模型,也适用于LS外推模型与其他模型的组合。     

Higher order ionospheric error correction in BDS precise orbit determination

The ionospheric error affects the accuracy of the Global Navigation Satellite Systems observation and precise orbit determination. Usually, only the first order ionospheric error is considered, which can be eliminated by the ionospheric-free linear combination observation. But the remaining higher order ionospheric error will affect the accuracy of observations and their applications. In this paper, the influence of the higher order ionospheric error have been studied by using the International Geomagnetic Reference Field 13 and the Global Ionosphere Maps model produced by the Center for Orbit Determination in Europe. Focus on ionospheric error, the experiment of paper at doy 302 in 2019, which show that the second order ionospheric error impacting BeiDou Navigation Satellite System (BDS) B1I and B3I observation is 6.3569 mm and 11.8484 mm, respectively. Whereas, the third order ionospheric error impacting BDS B1I and B3I observation is 0.1734 mm and 0.3977 mm, respectively. Due to the current measurement accuracy of BDS carrier-phase observation can reach 2 mm, the influence of high order ionospheric error on observation should be considered. For BDS precise orbit determination, the orbit overlapping results are indicated that its orbit accuracy can be improved approximately 5 mm with the higher order ionospheric error correction, which is also in agreement with the results of Satellite Laser Ranging in this work.     

An update global model of hmF2 from values estimated from ionosonde and COSMIC/FORMOSAT-3 radio occultation

In this paper, we present our recent work on developing an updated global model of the ionospheric F2 peak height hmF2 parameter by combining data from the Constellation Observing System for Meteorology, Ionosphere and Climate (COSMIC/FORMOSAT-3) radio occultation (RO) measurements and from the extended global ionosonde stations. In particular, 10 Chinese ionosonde stations’ data are newly introduced into this study. The modeling technique used is based on a two-layer empirical orthogonal function (EOF) expansion. Global distributions of hmF2 maps calculated using the newly constructed global model and the one provided by the International Reference Ionosphere model (IRI-ITU-R) are compared with the global distributions of hmF2 obtained by the COSMIC RO measurements and quantitative statistical analysis of the differences between the model results and those of the COSMIC RO measurements is made for the low (2008) and high (2012) solar activity years. The obtained average root-mean-square differences (RMSEs) for our model are 27.7 km (11.1%) and 31.0 km (9.8%), respectively for the years 2008 and 2012, whereas those for the IRI-ITU-R model are 39.9 km (16.9%) and 35.0 km (11.6%), respectively. Comparison of the results calculated both by our model and the IRI-ITU-R model with the digisonde observation is also made. The comparisons show that the newly constructed global hmF2 model can reproduce reasonably well the observations and perform better than IRI-ITU-R model.     

Global characteristics of ionospheric electric fields and disturbances during the first hours of magnetic storms

The ionospheric plasma density can be significantly disturbed during magnetic storms. In the conventional scenario of ionospheric storms, the negative storm phases with plasma density decreases are caused by neutral composition changes, and the positive storm phases with plasma density increases are often related to atmospheric gravity waves. However, recent studies show that the global redistribution of the ionospheric plasma is dominated primarily by electric fields during the first hours of magnetic storms. In this paper, we present the measurements of ionospheric disturbances by the DMSP satellites and GPS network during the magnetic storm on 6 April 2000. The DMSP measurements include the F region ion velocity and density at the altitude of ∼840 km, and the GPS receiver network provides total electron content (TEC) measurements. The storm-time ionospheric disturbances show the following characteristics. The plasma density is deeply depleted in a latitudinal range of ∼20° over the equatorial region in the evening sector, and the depletions represent plasma bubbles. The ionospheric plasma density at middle latitudes (20°–40° magnetic latitudes) is significantly increased. The dayside TEC is increased simultaneously over a large latitudinal range. An enhanced TEC band forms in the afternoon sector, goes through the cusp region, and enters the polar cap. All the observed ionospheric disturbances occur within 1–5 h from the storm sudden commencement. The observations suggest that penetration electric fields play a major role in the rapid generation of equatorial plasma bubbles and the simultaneous increases of the dayside TEC within the first 2 h during the storm main phase. The ionospheric disturbances at later times may be caused by the combination of penetration electric fields and neutral wind dynamo process.