翼面动态压力测量

对７０°三角翼作大幅度仰运动时翼面非定常压力分布和振动鸭翼后面主翼面上非定常压力进行了测量。分析了缩减频率等参数对非定压力分布的影响。     

基于遗传算法的大气层外拦截弹拦截优化

提出了一种同时考虑大气层外拦截弹中段和末段飞行过程的拦截优化方法.首先建立了大气层外拦截弹中段和末段飞行的动力学模型,并设计了速度增益中制导律和鲁棒变结构末制导律;然后确定了影响拦截性能的优化控制参数及其约束条件,以拦截过程的燃料消耗质量和脱靶量最小为组合性能指标;最后采用具有全局最优性的遗传算法对这一拦截优化问题进行了仿真研究,并与复形调优算法的结果进行了比较.仿真结果表明,遗传算法与传统优化方法相比在解决大气层外拦截弹带约束复杂非线性组合优化问题时,能更好地收敛到全局最优值,并能有效降低大气层外拦截的燃料消耗和脱靶量.     

能谱变硬后的X射线对Ly12铝破坏效应的研究

用数值模拟方法讨论了X射线的能谱向短波方向变化后,对Ly12铝破坏效应的影响,对所得结果进行了分析和解释。     

利用喷管引射和旋翼下洗的红外抑制器特性研究

在波瓣引射器一次引射掺混后,提出利用旋翼下洗气流对弯曲混合管排气进行二次强迫混合的红外抑制器结构,并对该红外抑制器进行了有关流动混合特性的实验和数值研究,获得了主流和引射气流、下洗气流相互混合过程中,混合管内部及抑制器出口处的温度场和压力场等相关信息,以及表征引射-混合系统总体性能的引射系数等参数。结果表明:引入下洗气流可以改善出口分布的不均匀性,经过波瓣喷管引射器泵吸周围空气掺混冷却和利用旋翼下洗气流进行二次冷却,可以有效使排气温度降低50%。     

一种改进的微粒群优化算法

标准微粒群优化(PSO)算法是一种群体智能算法,它容易陷入局部极值点,进化后期收敛速度慢且精度较差,而且参数的选择对算法的优劣影响很大。针对这些缺点,首先提出了一种在位置进化方程中引进动态参数的方法,改进了标准微粒群算法收敛速度;然后通过在速度、位置进化方程中同时引进动态参数来提高算法收敛速度和收敛率。经J．D．Schaffer函数和LevyNo．5函数对改进算法的测试表明,相比于标准微粒群算法,该方法的收敛速度和平均收敛率均有大幅度提高。     

利用双目标优化寻求颤振抑制控制律

本文对一个三角机翼/外挂系统的颤振主动抑制进行了系统的研究。在理论上,对如何应用现代控制理论设计优化控制律进行了探讨;对非定常气动力拟合的Pade矩阵近似作了改进;提出了用理想极点和二次型性能指标进行双目标优化来确定加权矩阵的思想;在实现上,用状态观测器和单秩法极点配置两种方法设计了输出反馈控制律。风洞实验结果表明:用本文的方法所综合的控制律是合适有效的,成功地使机翼/外挂系统的颤振速度提高了15.7％,与理论计算结果吻合良好。     

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).     

对相控阵雷达自适应旁瓣对消的多点源压制干扰

分析了相控阵雷达自适应旁瓣对消的工作原理及方法.然后提出了用多台干扰设备协同工作的相参干扰.每台干扰设备在雷达处理间隔内发射能覆盖真实目标并且持续时间较短的干扰信号,多台设备协同工作在目标附近形成压制干扰.该方法影响雷达样本选择,从而降低自适应旁瓣对消的效果.仿真结果和外场试验表明了该方法的有效性.