改进 K-均值算法在雷达辐射源信号预分选中的应用

雷达辐射源信号分选是电子对抗领域一个关键技术,随着电子技术的发展,电磁环境日趋复杂,信号分选的难度越来越大,在这样的条件下,我们应该寻求新的解决问题的方法.本文首先概述了雷达辐射源信号分选意义、系统组成和分选流程,然后介绍了改进 K-均值算法.为了有效实现信号分选,提出了基于改进K-均值算法的信号分选方法,该方法可对到达角、载频和脉宽参数进行分选.最后进行了仿真实验,结果表明该方法实现简单,分选效果较好     

气膜约束对轴系固有频率影响的试验

对10kg转子进行自由状态和有气膜约束两种状态下的试验模态分析,试验结果给出了转子平动、锥动和一阶弯曲时的固有频率及其振型等模态参数,分析了轴承供气压力变化对轴系固有频率的影响.进行了轴系升降速试验,结果表明:气膜约束下的模态分析结果比自由状态下的更接近于升降速试验的结果.试验结果为气体轴系固有频率的确定以及控制参数的选取提供了依据,也为下一步轴系振动控制奠定了基础.      

Ionospheric disturbances on 8 September, 2010: Was it connected with the incoming moderate Chongqing earthquake?

Earthquake prediction stimulates the searches for a correlation between seismic activity and ionospheric anomalies. Contrary to common focuses on strong earthquakes, we report the ionospheric disturbances, 2 days before a moderate Ms = 4.7 Chongqing earthquake (29.4°N, 105.5°E, depth = 7.0 km, occurred at 21:21 LT, 10 September, 2010) with the data of ground-based ionosondes and IGS receivers. The data covering the period under the quiet geomagnetic conditions and a geomagnetic storm was analyzed with upper and lower bounds. It is found that there were significant enhancements of foF2 and total electron content (TEC) on the afternoon of 8 September, 2010, with a limited area close to the epicentre, which was different from the feature of ionospheric perturbations triggered by the geomagnetic storm on 15 September. Taking into account the heliogeomagnetical condition, we conclude that the observed ionospheric enhancements were very likely associated with the forthcoming moderate Chongqing earthquake, which implies that the relationship between the amplitudes of ionospheric disturbances and earthquakes is very complicated.     

一种基于非平稳信号分析的时相调制信号解调算法

基于非平稳信号分析方法,对时相调制(Time-Phase Modulation,TPM)信号的时频分布特性进行了详细分析,建立了TPM调制信号相位突变与时频分布幅度的映射关系,利用该映射提出了一种基于非平稳信号分析的TPM调制信号解调算法,并对该解调算法性能进行了理论分析,讨论了最佳判决门限选取方法,仿真结果验证了理论分析的正确性。理论分析及仿真表明,基于非平稳信号分析的TPM调制信号解调算法获得了优于传统的相关解调的调制系统差错性能。     

射频干扰对InSAR干涉处理的影响分析

窄带干扰是低频段InSAR系统面临的主要射频干扰之一,它的存在会对干涉相位产生严重影响,进而导致高程反演误差。本文推导了窄带干扰影响下的InSAR干涉相位的解析表达式,给出了干涉相位对窄带干扰各参数的敏感度方程,仿真分析了窄带干扰对P波段InSAR系统干涉处理的影响。结果表明,窄带干扰经过成像后其幅度调制函数近似为方位时间的sinc函数,在SAR图像中表现为沿距离向的干扰条带。干涉相位对窄带干扰信号的功率较敏感,对其频率较不敏感,干涉相位和高程反演误差随着干信比的增加而增加。     

一种用于WorldView-2遥感图像的波段分组融合方法

针对WorldView-2卫星遥感图像,提出一种基于波段分组的多光谱图像与全色光图像融合新方法。该方法以全色光波段与多光谱各波段光谱响应的匹配特点为依据,首先将八波段多光谱图像分成两组,然后分别设计融合模型再进行分组融合,最终得到多光谱各波段的融合结果,分组策略简单、实用。实验结果表明,该方法在融合WorldView-2遥感图像时能够在提高空间分辨率和保持光谱信息方面达到更好的平衡,优于现有的几种融合方法。     

一种航天器单脉冲差模角跟踪系统的标定及测试方法

介绍了航天器单脉冲差模角跟踪系统的组成和基本原理;针对捕获跟踪系统性能与射频通道相位特性的相关性,提出了在无线状态下通过用户目标在一定范围内按一定轨迹运动进行射频通道相位标定及跟踪性能测试的方法;在此基础上进一步提出了利用信号源模拟用户目标在角跟踪系统天线坐标系下不同位置时天线输出的射频信号,进行有线状态下射频通道性能的测试方法。标定及测试方法通过地面试验验证了可行性和有效性,可用于航天器单脉冲差模角跟踪系统在地面的通道相位标定、跟踪性能测试和射频通道性能测试,以实现角跟踪系统对用户目标高精度、稳定的跟踪。     

一种基于迭代的多音干扰消除方案

针对正交频分复用技术(OFDM)系统的多音干扰,本文提出先通过增加频域分辨率进行多音干扰识别,再基于迭代运算逐个对多个单音干扰进行参数估计、重构和消除的方案。其中,在多音干扰识别阶段,使用Zoom FFT技术以提高频域分辨率并简化计算复杂度。然而,Zoom FFT后的降采样序列点数不一定满足2的整数次幂,对于单音干扰参数估计,此时可采用经典的基于离散傅里叶变换(DFT)的最大似然参数估计(DFT-MLE),但当采样点数太大时,DFT运算将带来很大的实现复杂度。本文在基于DFT-MLE算法基础上给出一种基于快速傅里叶变换(FFT)的单音参数估计法FFT-MLE,不仅简化了运算复杂度,而且相比DFT-MLE其估计性能有更好的鲁棒性。最后的仿真结果说明了该多音干扰消除方案的有效性。     

基于自适应算法的Stewart平台微振动低频激励控制研究

针对空间微振动环境模拟的需求,以Stewart平台为对象,研究低频微振动激励控制.传统定增益控制器需要反复调节参数来获取满意的系统输出,同时由于摩擦等因素引起的非线性现象,导致难以在低频段建立精确的系统模型,以上问题均给控制器的设计带来困难.为此,设计一种自适应控制器加传统PID控制器的控制方案,并针对自适应控制器对于非参数不确定性等因素敏感的问题,采用dead-zone技术对自适应律进行修正,以提高控制器的鲁棒性.将此算法应用于Stewart微激励控制系统中,实验结果表明系统平台可以很好的输出单自由度与多自由度低频正弦激励,验证控制器在实际工程中的有效性.     

Investigation of vertical profile of rain microstructure at Ahmedabad in Indian tropical region

The microstructure of rain has been studied with observations using a vertical looking Micro Rain Radar (MRR) at Ahmedabad (23.06°N, 72.62°E), a tropical location in the Indian region. The rain height, derived from the bright band signature of melting layer of radar reflectivity profile, is found to be variable between the heights 4600 m and 5200 m. The change in the nature of rain, classified on the basis of radar reflectivity, is also observed through the MRR. It has been found that there are three types of rain, namely, convective, mixed and stratiform rain, prevailing with different vertical rain microstructures, such as, Drop Size Distribution (DSD), mean drop size, rain rate, liquid water content and average fall speed of the drops at different heights. It is observed that the vertical DSD profile is more inhomogeneous for mixed and stratiform type rain than for convective type rain. It is also found that the large number of drops of size <0.5 mm is present in convective rain whereas in stratiform rain, drops concentration is appreciable up to 1 mm. A comparison of measurements taken by ground based Disdrometer and that from the 200 m level obtained from MRR shows good agreement for rain rate and DSD at smaller rain rate values. The results may be useful for understanding rain structures over this region.