基于AOE网的过站航班保障进程优化

航班地面保障是机场运行的重要环节，为了提升航班地面保障效率，针对某机场航班地面保障流程构建AOE 网，通过该机场A-CDM 系统记录的航班节点数据求出该机场航班地面保障作业的“关键路径”。通过对关键路径上可压缩工序的分析，对该机场的地面保障作业流程进行优化。以我国西南地区某机场航班地面保障的实际数据为基础，剔除不可抗力造成的不正常数据，分别计算保障流程优化前后的航班过站时间。结果表明：在33 组航班数据中，该机场使用AOE 网络优化后的保障作业流程比优化前平均减少地面保障作业时长6.1 分钟/架次，说明通过合理地优化航班地面保障进程，可以有效提高机场的运行效率。     

TE_（113）模波导侧壁耦合滤波器的研究

文章描述了一种侧壁耦合波导滤波器的设计方法,详细探讨了侧壁耦合结构,并在对侧壁耦合分析的基础上,使用CST软件仿真了一部TE113模侧壁耦合滤波器,实现了四阶椭圆函数特性,仿真结果与实测结果吻合良好。另外,对寄生耦合与简并模式耦合机构之间的关系也进行了深入探讨。     

基于最临界约束准则法的机翼主承力结构优化

利用最临界约束准则法对某型飞机机翼主承力结构在强度，位移，扭转角，稳定性和尺寸约束下，以最小重量为目标函数进行了优化，并在实际操作过程中依据机翼结构的复杂性对最临界约束准则法做了相应的修改。结果表明，应用最临界约束准则法进行机翼结构优化时，效率较高，机翼结构重量稳定下降，优化效果明显。     

拓扑优化在机载计算机结构设计中的应用

为了解决机载计算机零件结构设计过程中出现的材料分布不合理及重量要求苛刻等问题，在设计过程中引入拓扑优化。介绍了基于变密度法的拓扑优化理论，以Hyperworks／Optistruct为拓扑优化分析平台，对某机载计算机零件进行了拓扑优化，确定了零件的最佳材料分布。结果表明：通过优化设计可以在保持零件基本结构性能的基础上减轻其重量。     

偏转弹头导弹控制系统设计与仿真

根据弹头的可偏转特性,利用无根多刚体系统动力学方法建立了偏转弹头导弹的动力学模型,并对通道间的耦合特性及弹头偏转对弹体运动的影响进行了分析。在此基础上,将通道间的耦合及弹头偏转对弹体运动的影响作为干扰项处理,将气动参数的非线性变化等效为标称参数的摄动,利用变结构控制理论设计了偏转弹头导弹的控制器。仿真结果表明,所设计的变结构控制器能够有效地减小和消除俯仰、偏航通道对滚转通道的耦合作用以及弹头偏转对弹体运动的影响,较好地抑制了导弹气动参数的摄动,具有较高的稳态精度和良好的动态性能。     

邻近空间无线通信连接技术的探讨

文章研究了CCSDSPSLP（空间数据系统咨询委员会邻近空间链路协议）的连接技术,从连接帧格式、指令内容、状态逻辑、参数配置等方面进行了深入分析,重点研究了物理层、编码与同步子层的底层功能及接口细节,并从实现的角度讨论了三种优化连接的方法流程,为基于PSLP的设备研制做出了具备应用价值的技术探索.     

Contribution of ionospheric TEC anomalies to detecting the seismic precursors related to the 2008 Oran-Algeria event

The ionospheric anomalies observed before any notable earthquake have become the subject of predictive research in the field of seismo-ionospheric coupling and/or Solid Earth-Atmosphere. In this paper, the concept of ionospheric modeling has been applied using total electronic content (TEC); derived from dual-frequency GPS recordings from about sixty permanent geodetic stations. The study and the analysis of the anomalous TEC variations, quantifiable on a regional scale, allowed us to detect the principal precursors of the M_w 5.5 earthquake that hit Oran on June 06th, 2008. The envisaged analytical approach is based principally on the time delays estimation relating to the seismic responses from the triggering (lithospheric seismic source) until their recording in data Rinex (GPS_IGS stations) through the reflection system of the electromagnetic waves on the ionospheric level (F2-layer).Indeed, in term of location, the longitude-latitude coordinates of the Oran event epicenter (0.658°W, 35.883°N) affecting the coastal margin of Western Algeria without too much material damage. Although the magnitude of this earthquake is qualified moderate (M_w 5.5, seismic intensity scale V-VI), one can observe apparent disturbances in the terrestrial electromagnetic spectrum associated with ionospheric TEC variations. In the domain of geodetic data analysis, we have noted a significant increase in the ionospheric TEC, which announces the arrival of a seismic precursor several days before the main studied event. Against this background, we emphasize that any seismic event, of significant magnitude, often carries information associated with other variants involved in the package of earthquake studied. Among these variants we evoke the effect of the magnetic field and the effect of the surrounding environment, etc. As for the specific behavior of the GPS_TEC signal, obtained from the Rinex data, and its interaction with the associated seismic activity, we highlight the existence of a spectral conformity between the geomagnetic field and that of the TEC content (spontaneous polarization of the TEC).Finally, we have just confirmed the effectiveness of this forecasting approach which relates the seismo-ionospheric precursors that are embedded in the physical trace of the electromagnetic signal relative to significant and/or moderate earthquakes (M ≥ 5); such as the envisaged case of the 2008 Oran event.     

Hemisphere-coupled modeling of nighttime medium-scale traveling ionospheric disturbances

Nighttime medium-scale traveling ionospheric disturbances (MSTIDs), which have tilted frontal structures in the midlatitude ionosphere, are investigated by the midlatitude ionosphere electrodynamics coupling (MIECO) model in this study. It has been proposed that the electrodynamic coupling between the E and F regions plays an important role in generating MSTIDs within a few hours. An intriguing aspect of MSTIDs is that they were simultaneously observed at magnetic conjugate locations in the Northern and Southern Hemispheres. In order to study the hemisphere-coupled electrodynamics, the MIECO model has been upgraded to consist of two simulation domains for both hemispheres in which the electrostatic potential is solved by considering electrodynamics in both hemispheres. The simultaneous occurrence of MSTIDs at the magnetic conjugate stations has clearly been reproduced when the F-region neutral wind satisfies the unstable condition in both hemispheres and a sporadic-E layer is given only at the Northern (summer) Hemisphere. Even if the unstable condition is satisfied in the summer hemisphere, an unfavorable F-region neutral wind in the winter hemisphere largely suppresses the growth of MSTIDs in both hemispheres.     

Lunar geophysical parameters inversion based on gravity/topography admittance and particle swarm optimization

This paper presents a FORTRAN computer program. The program as code will be used for lunar parameter inversions based on gravity/topography admittance. This will be done by assuming that the lunar lithosphere is modeled as a thin elastic spherical shell. The parameters discussed here include; load ratio, crustal thickness, subsurface load depth, crustal density and elastic lithosphere thickness. The admittance of the best-fitting model can be found through automatically adjusting misfits between one theoretical admittance and an observed one. The results in this paper indicate that this research’s theoretical model is reasonable for exploring the best-fitting parameters. In addition, this code is not only able to automatically and simultaneously calculate the global optimum solution of the parameters studied, but also performs well in computational speed. The code can be easily modified to include more parameter inversions; such as the inversion for subsurface density anomaly and the case of considering infilling material in some lunar mare basins.