基于模型预测控制的多约束火星精确着陆制导律研究

主要研究了火星着陆动力下降段考虑燃料消耗和实际任务约束条件的制导律设计问题。选取可变推力发动机作为执行机构,首先建立了着陆器在动力下降段的运动方程及质量变化方程;其次对实际任务中需要考虑的斜坡、推力幅值和方向等约束条件建立了约束模型;接下来通过构造由控制量和状态量构成的性能指标,提出一种基于模型预测控制的多约束火星精确着陆制导算法。可实现多种约束条件下的指标最优精确着陆任务。最后,通过数值仿真对比了本文与已有典型着陆策略,验证了所提算法可以在满足约束条件的前提下有效地完成既定火星精确着陆任务。     

结构动力模型一体化降阶技术

本文提出应用一体化降价技术实现结构动力模型的有效降阶，即首先在物理空间用动力缩聚（dy-namic condensation）法，然后在状态空间用平衡模型降阶（Balance Model Reduction）法，降低原始模型的阶数，这样就能结合有限元分析中物理模型降阶技术及控制理论中平衡降阶法的优点，所得降阶模型不仅阶数较低，而且所得状态空间方程具有可观且可控的优点。仿真表明，这种一体化降价技术算法稳定，计算精度高。     

多级安全关系数据模型研究及其改进

讨论了基本的多级安全模型存在的主要缺陷，如推理通道问题。系统的可用性、灵活性受到严格的“向下读，向上写”规则的限制问题．不能保证数据完整性。通过引入多实例和伪元组．并重新定义读写规则．使改进后的模型更具安全性、灵活性和可用性。     

基于最小总体偏差和区域信息Snake模型的图像分割

提出基于最小总体偏差和区域信息Snake模型的图像分割方法。根据最小总体偏差准则，用包含区域信息的变力替换在气球力Snake模型中的恒定力，并应用于图像分割。实验结果表明，该模型与初始轮廓曲线位置无关，能自动分割模糊边界。对于带椒盐噪声的图像，应用该模型也能取得满意的分割效果。     

连续波激光对弹道导弹的毁伤效应

本文对美国报导的洲际弹道导弹“大力神”Ⅰ型贮箱与“飞毛腿”弹道导弹受强激光辐照演示实验的破坏模式和破坏机理进行了分析。认为：用激光拦截助推段弹道导弹时,其液体贮箱壳体和固体燃料发动机壳体是最易损的,生存能力很低;在新型号设计时应进行结构加固。     

航天器与空间碎片的混合编队重构控制与应用

针对空间碎片清理问题,提出了一种利用航天器与空间碎片混合编队队形重构控制技术捕获碎片的方法。首先,分析了地/月—日系L2拉格朗日平动点附近的限制性三体环境,并建立了编队卫星相对运动动力学模型;其次,提出了以太阳光压力作为航天器与空间碎片编队队形重构的控制力,实现各从星接近空间碎片的目的;最后,设计了基于线性二次型的最优控制器,并在Matlab/Simulink环境下进行仿真实验。仿真结果表明该方法可控制从星到达期望的位置(空间碎片的位置),且太阳帆板的姿态变化在可控范围内,进而证明了该方案可以应用于复杂空间环境下的碎片清理任务。     

基于GMF方法的捕风一号风速反演分析

全球尺度高时空分辨率海面风场探测是当前全球气象研究及预报预测领域的关注热点之一,传统海面风场探测技术存在测量区域有限,且受天气环境限制明显等问题.基于全球导航卫星系统-反射(GNSS-R)测量技术风速反演原理,以捕风一号1级数据产品为输入,欧洲中期天气预报中心再分析风速数据为参考风速,采用地球物理模型函数(GMF)方法...     

Stochastic modelling considering ionospheric scintillation effects on GNSS relative and point positioning

Global Navigation Satellite Systems (GNSS), in particular the Global Positioning System (GPS), have been widely used for high accuracy geodetic positioning. The Least Squares functional models related to the GNSS observables have been more extensively studied than the corresponding stochastic models, given that the development of the latter is significantly more complex. As a result, a simplified stochastic model is often used in GNSS positioning, which assumes that all the GNSS observables are statistically independent and of the same quality, i.e. a similar variance is assigned indiscriminately to all of the measurements. However, the definition of the stochastic model may be approached from a more detailed perspective, considering specific effects affecting each observable individually, as for example the effects of ionospheric scintillation. These effects relate to phase and amplitude fluctuations in the satellites signals that occur due to diffraction on electron density irregularities in the ionosphere and are particularly relevant at equatorial and high latitude regions, especially during periods of high solar activity. As a consequence, degraded measurement quality and poorer positioning accuracy may result.     

Upper limit of the total magnetic flux in an active region according to the photometric-magnetic dynamical model

The photometric-magnetic dynamical model handles the evolution of an individual sunspot as an autonomous nonlinear, though integrable, dynamical system. One of its consequences is the prediction of an upper limit of the sunspot areas. This upper limit is analytically expressed by the model parameters, while its calculated value is verified by the observational data. In addition, an upper limit for the magnetic strength inside the sunspot is also predicted, and then, we obtain the following significant result: The upper limit of the total magnetic flux in an active region is found to be of about 7.23 × 10²³ Mx, namely, phenomenologically equal to the magnetic flux concentrated in the totality of the granules of the quiet Sun, having a typical maximum magnetic strength of about 12G. Therefore, the magnetic flux concentrated in an active region cannot exceed the magnetic flux concentrated in the photosphere as a whole.     

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.