星间链路天线相对姿态的地面模拟

星间链路天线的相对姿态模拟为星间链路的测试验证提供近真实的动态姿态环境,是星间链路系统地面测试的重要组成部分。建立多个坐标系统将两颗卫星天线的位置和姿态联系起来,利用卫星星历将天线的相对姿态表示为一颗卫星天线在另一颗卫星天线坐标系中的方向向量,利用两个二轴转台实现此方向向量,最终通过控制转台的转角模拟卫星天线的相对姿态变化。同时计算天线波束的方向,分析了两颗卫星的可见性。天线相对姿态的模拟为星间链路的建立和保持提供动态测试环境。     

无人机全空域飞行影响因素分析

进入全空域飞行是未来无人机发展的必然趋势,所面临的关键问题是安全性和空中交通管理.根据无人机大、中、小型,低、中、高速并存的特点,分析了无人机安全性和影响其全空域飞行能力的关键因素与改进方法,包括建立分类管理机制,提高自主导航与控制能力,进行动态任务规划,采取协调机制,增强环境感知与规避能力等.进一步提出了无人机空域飞行的建模/仿真理论框架,目标是在提高无人机可靠性的基础上,使其具备全空域飞行能力,从而降低无人机使用成本、提高空域共享能力,实现有人机、无人机共享空域.      

输入受限的编队卫星分布式姿态协同控制

研究了跟踪时变参考姿态情况下的编队飞行卫星协同控制问题,提出了一种非线性饱和的分布式协同控制器。在控制器中引入了一个双曲正切函数向量,保证了连续控制输入的有界性。采用Barbalat引理对姿态跟踪情况下闭环协同控制系统的稳定性进行了分析,得出了系统渐近稳定的结论。通过对各种条件下的仿真,验证了算法的有效性,并确立了编队卫星信息流图的拓扑结构和控制器增益等因素与暂态过程中相对姿态保持性能的关系。     

飞行员视觉信息流强度模拟及适人性分析

为了合理地确定飞行员在执行飞行任务时的视觉信息流强度,开发了飞机座舱显示界面仿真模型,以被试的正确反应率和反应时间来评价作业绩效.通过实验和数据分析得到以下结果:所建立的视觉信息流模型中视觉信息流强度曲线符合正态分布.不同的视觉信息量完成任务差异显著,信息量增加到一定程度时辨识变慢,出现错误的几率升高;在相同视觉信息量情况下,夜晚与白天、动态与静态执行任务辨识和绩效差异显著,白天要比夜晚、静态要比动态辨识效率和绩效更好.      

星载可展开天线热振动数值分析

根据非耦合动力学理论及有限元方法,研究分析了星载可展开天线的热振动。利用半正弦波温度冲击模拟热动力荷载,对天线典型节点的热振动位移和应力以及形面精度进行了数值分析。研究表明,急剧变化的温度荷载将导致该天线结构发生热振动,热振动响应明显大于静力学响应。     

基于AFDX网络的飞行管理仿真系统

系统建模与数字仿真是大型客机飞行管理系统研发的重要阶段.初步建立了基于航空电子全双工交换式以太网(AFDX,Avionics Full-Duplex Switched Ethernet)的飞行管理系统分布式实时仿真系统模型.对飞行计划、飞行导引、轨迹预测、性能计算、综合导航、导航数据库、综合显示等核心功能进行了分析建模和算法开发.并在此基础上对飞行管理计算机、综合导航系统、自动飞行系统等仿真子系统进行了设计,在满足实时性要求的前提下,基于AFDX网络与分布式仿真结构实现了对以飞行管理计算机系统为核心的航空电子仿真系统的集成,给出了一种通用的、基于AFDX网络的飞行管理系统分布式仿真框架.仿真系统的运行结果证明:基于AFDX网络的分布式仿真结构能够有效满足实时性要求,提高网络通信性能.      

基于动态RCS的无人机航迹实时规划

传统的无人机航迹规划主要采用仅考虑无人机与雷达距离的简化雷达威胁模型,未充分考虑无人机雷达散射截面RCS(Radar Cross-Section)随自身姿态角改变而产生的动态变化.据此,提出了无人机周向动态RCS模型,并建立了综合考虑无人机动态RCS与雷达距离的探测概率模型,利用遗传算法进行了基于动态RCS的航迹实时规划,计算结果与传统航迹规划结果进行了对比.仿真结果表明该模型的可行性和有效性,能充分利用无人机自身的优势规避威胁,满足无人机的航迹实时规划的要求.      

基于离散事件方法的AFDX建模与仿真

采用了建模仿真的方法来分析航空电子全双工交换式以太网(AFDX,Avionics Full Duplex switched ethernet)协议.通过对AFDX协议的抽象,基于离散事件的建模方法,以基本的网络元素来抽象化网络中的端系统、交换机等设备,以离散事件来描述网络设备的行为,以此构建了AFDX网络模型,并依据模型实现了仿真.网络演算是一种理论计算AFDX最坏延迟界限的方法,将典型场景下仿真得到的结果与理论计算的结果进行比较,验证了模型.通过不同流量方案下仿真结果的对比,对AFDX进行了传输特性的分析.      

Day-to-day variability of equatorial anomaly in GPS-TEC during low solar activity period

The ionospheric total electron content (TEC) in the northern hemispheric equatorial ionization anomaly (EIA) crest region is investigated by using dual-frequency signals of the Global Positioning System (GPS) acquired from Rajkot (Geog. Lat. 22.29°N, Geog. Long. 70.74°E; Geom. Lat. 14.21°N, Geom. Long. 144.90°E), India. The day-to-day variability of EIA characteristics is examined during low solar activity period (F10.7∼83 sfu). It is found that the daily maximum TEC at EIA crest exhibits a day-to-day and strong semi-annual variability. The seasonal anomaly and equinoctial asymmetry in TEC at EIA is found non-existent and weaker, respectively. We found a moderate and positive correlation of daily magnitude of crest, Ic with daily F10.7 and EUV fluxes with a correlation coefficient of 0.43 and 0.33, respectively indicating an existence of a short-term relation between TEC at EIA and the solar radiation even during low solar activity period. The correlation of daily Ic with Dst index is also moderate (r = −0.35), whereas no correlation is found with the daily Kp index (r = 0.14) respectively. We found that the magnitude of EIA crest is moderately correlated with solar flux in all seasons except winter where it is weakly related (0.27). The magnitude of EIA crest is also found highly related with EEJ strength in spring (r = 0.69) and summer (r = 0.65) than autumn (0.5) and winter (r = 0.47), though EEJ is stronger in autumn than spring.     

The South Pole-Aitken basin region,Moon: GIS-based geologic investigation using Kaguya elemental information

Using Geographic Information Systems (GIS), we performed comparative analysis among stratigraphic information and the Kaguya (SELENE) GRS data of the ∼2500-km-diameter South Pole-Aitken (SPA) basin and its surroundings. Results indicate that the surface rock materials (including ancient crater materials, mare basalts, and possible SPA impact melt) are average to slightly elevated in K and Th with respect to the rest of the Moon. Also, this study demonstrates that K and Th have not significantly changed since the formation of SPA. The elemental signatures of the impact basin of Fe, Ti, Si, O through time include evidence for resurfacing by ejecta materials and late-stage volcanism. The oldest surfaces of SPA are found to be oxygen-depleted during the heavy bombardment period relative to later stages of geologic development, followed by both an increase in silicon and oxygen, possibly due to ejecta sourced from outside of SPA, and subsequent modification due to mare basaltic volcanism, which increased iron and titanium within SPA. The influence of the distinct geologic history of SPA and surroundings on the mineralogic and elemental abundances is evident as shown in our investigation.