甲居走进绝美乡村

甲居是距丹巴县城二十多公里的一个山村，最早．知道这个地方是从实际充当了旅游先行者的摄影家们的图片上。那如梦幻般的田园景致吸引着无数人趋之荇鹜，并获得了“中国最美的乡村”的称号。[编者按]     

变速恒频电源系统的数字仿真研究

建立了脉宽调制型交直交变速恒频电源系统的数学模型，研制了仿真软件，并给出了仿真实例。研究表明，本文的方法和软件可以进行变速恒频电源系统部件级和系统级的仿真分析，为设计和分析该系统提供了有力的工具。文中的方法和软件也可以用于分析恒速恒频和高压直流电源系统，为开发一套完整的飞机电源系统仿真软件奠定了基础。     

改进力控方案完成异形孔装配

讨论了改进的力／位混合控制方案、异形孔装配策略规划及其在ＪＲＢ－１机器人上的实现。简述了该方案的优点，在ＪＲＢ－１机器人上实现所解决的问题，提出用适应性增益解决力控环稳定问题。文中还结合异形孔装配给出了装配任务的描述和装配策略的自动生成方法。     

超声爬波无损检测方法的研究

本文介绍了超声无损检测中一种具有较好应用前景的波型──超声爬波。试验研究了爬波检测时缺陷定位、定性评定的方法，并给出了主要结论。     

人工释能法求解线性代数方程组

本文建立求解线性代数方程组的人工释能法迭代格式,并给出该迭代格式收敛的充分必要条件和最佳释能时机,同时给出实现人工释能法的数值计算方法及其数值稳定性条件。     

燃烧室头部进气规律对煤粉燃烧效率的影响

用实验方法研究了火焰筒式煤粉燃烧室头部进气规律对燃烧效率的影响。通过对6种结构的头部配气方案的分析比较,得出了煤粉燃烧室合理的头部配气方案,为今后煤粉燃烧室的设计和工作状态的选择提供了重要的实验依据。     

建立腔体热释电探测器相对光谱响应度标尺的研究

由于腔体热释电探测器在宽光谱范围内具有相对平坦的光谱响应度,因此经常被用作标定探测器相对光谱响应度的工作基准。但是在标定过程中通常认为腔体热释电探测器是无光谱选择性的,即R(λ)为常数。这样就会使测量结果不够准确,因此建立腔体热释电探测器相对光谱响应度的标尺是非常重要的。本文主要介绍了建立腔体热释电探测器相对光谱响应度标尺的原理和方法,并通过实验利用该方法建立了腔体热释电探测器相对光谱响应度的标尺,从而使该腔体热释电探测器成为红外光谱响应度测量装置的工作基准。     

基于层次分析法的飞行模拟训练评价体系设计

为科学完善地描述飞行模拟训练中的应急处置程序,提升飞行员专业驾驶技术水平,本文提出飞行模拟训练评价体系,并通过层次分析法构造3阶判断矩阵,检测矩阵一致性指标为0.037,具有可接受性;并采用关联度进行数据分析量化计算,为飞行训练考核标准奠定理论基础。     

多机并联火箭羽流流场及其底部热环境分析

For the problem that the plume flow field structure of a multi engine parallel rocket is complicated and the bottom thermal environment is extremely harsh, which may cause the failure of the engine structural components, the plume flow field and thermal environment at different altitudes are studied through numerical simulation. The result is compared with the measured results in flight which shows that when the rocket is flying at a low altitude, the plume of the engines do not interfere with each other. As the flight altitude increases, the plumes gradually expand and begin to interfere with each other, and finally there is an obvious backflow at the bottom of the rocket. The maximum heat flux at the moment of take off is basically the same as the measured value in flight. Before the backflow occurs, the heat flux mainly consists of radiant heat, the convective heat flow increases as the flight altitude grows, but it is also much smaller than the peak heat flow at takeoff. The result has certain guiding significance for the optimal design of engine structure thermal protection.     

A comprehensive study of the 2016 Mw 6.0 Italy earthquake based on high-rate (10 Hz) GPS data

The 2016 M_w 6.0 Italy earthquake is successfully recorded by the near-field 10?Hz GPS and 200?Hz Strong Motion (SM) stations, providing valuable data for this study. A comprehensive study of this earthquake is carried out based on GPS data, which contains coseismic deformations analysis, noise analysis, seismic wave picking, and magnitude determination. The noise of most GPS-derived displacement waveforms can be described as a combination of white noise, flicker noise, and random walk noise after the earthquake occurrence, and the spectral indices vary significantly for most stations, implying that the seismic signals have affected the noise characteristic of GPS-derived displacement waveforms. S-transform is employed to assess the GPS capability to detect the seismic arrival time. The SM station AMT and the GPS station AMAT are in good agreement in seismic wave picking, and the difference is only 1.2?s in the north component, suggesting that the outcome of seismic wave picking using GPS data is reliable. Then, a classic empirical formula is employed to determine the moment magnitude. A robust moment magnitude (Mw 5.90) can be estimated by the nine GPS stations with about 23.9?s. If four GPS stations near the epicenter is chosen to determine the magnitude, it only take 13.0?s to retrieve a reliable preliminary (Mw 5.82) magnitude, which is 5.4?s ahead of nine stations. In addition, Cross Wavelet Transform (XWT) is adopted to measuring the correlation and phase relationship between GPS and SM records. The result of XWT analysis indicates 10?Hz GPS is capable of capturing reliable and accurate coseismic dynamic deformations, as evidenced by the XWT-based semblance being close to 1 between GPS and SM records. The above results confirm the capability of 10?Hz GPS to capture coseismic dynamic deformations, detect seismic arrival time, and determine earthquake magnitude. Moreover, rapid magnitude determination based on 10?Hz GPS data can be regarded as an important supplement to Earthquake Early Warning (EEW).