Study of daytime vertical E × B drift velocities inferred from ground-based magnetometer observations of ΔH,at low latitudes under geomagnetically disturbed conditions

In this study, 30 storm sudden commencement (SSC) events during the period 2001–2007 for which daytime vertical E × B drift velocities from JULIA radar, Jicamarca (geographic latitude 11.91°S, geographic longitude 283.11°E, 0.81°N dip latitude), Peru and ΔH component of geomagnetic field measured as the difference between the magnitudes of the horizontal (H) components between two magnetometers deployed at two different locations Jicamarca (geographic latitude 11.91°S, geographic longitude 283.11°E, 0.81°N dip latitude) and Piura (geographic latitude 5.21°S, geographic longitude 279.41°E, 6.81°N dip latitude), in Peru, were considered. It is observed that a positive correlation exists between peak value of daytime vertical E × B drift velocity and peak value of ΔH for the three consecutive days of SSC. A qualitative analysis made after selecting the peak values of daytime vertical E × B drift velocity and ΔH showed that 57% of the events have daytime vertical E × B drift velocity peak in the magnitude range 20–30 m/s and 63% of the events have ΔH peak in the range 80–100 nT. The maximum probable (45%) range of time of occurrence of peak value for both vertical E × B drift velocity and ΔH during the daytime hours were found to be the same, i.e., 10:00–12:00 LT. A strong positive correlation was also found to exist between the daytime vertical E × B drift velocity and ΔH for all the three consecutive days of SSC, for all the events considered. To establish a quantitative relationship between day time vertical E × B drift velocity and ΔH, linear and polynomial (order 2 and 3) regression analysis (Least Square Method (LSM)) were carried out, considering the fully disturbed day after the commencement of the storm as ‘disturbed period’ for the SSC events selected for analysis. The formulae indicating the relationship between daytime vertical E × B drift velocity and ΔH, for the ‘disturbed periods’, obtained through the regression analysis were verified using the JULIA radar observed E × B drift velocity for 3 selected events. Root Mean Square (RMS) error analysis carried out for each case suggest that polynomial regression (order 3) analysis provides a better agreement with the observations from among the linear, polynomial (order 2 and 3) analysis.     

基于TMS320F2812的卫星天线稳定控制系统的设计

对卫星天线稳定跟踪系统的工作原理进行了分析,设计了一种基于DSP TMS320F2812的天线稳定控制器,详细分析了系统的原理、构成、设计方法,概要介绍了DSP芯片的特点及其电路设计和系统软件的设计及其模块划分和功能,在matlab上对系统进行了仿真实验,得到了良好的仿真效果。     

三层铝板结构高速撞击损伤与极限特性

利用二级轻气炮发射铝球弹丸,在真空环境下高速撞击双层铝板和三层铝板结构,研究撞击速度、板间距、铝板厚度对结构撞击损伤的影响。然后分析三层铝板结构的撞击极限速度,并与相同面密度的双层铝板结构的试验结果进行比较。结果表明,当面密度相同时,三层铝板结构比双层铝板结构具有更强的高速撞击防护能力,增加首层铝板厚度有助于提高三层铝板结构高速撞击防护性能,当第二层铝板位于首层铝板与舱壁中间位置时,三层铝板结构的高速撞击防护性能趋于最佳。     

支柱式沉浸水橇降载性能相关影响因素

支柱式沉浸水橇可降低水陆两栖飞机着水运动中的冲击载荷,其降载效果与水陆两栖飞机的运动参数有关。利用一般耦合算法对水陆两栖飞机着水运动进行仿真,并将结果与相关试验值比对以验证仿真方法的有效性。采用此方法研究了水橇着水角、飞机着水水平速度与飞机着水垂向速度对支柱式沉浸水橇降载性能的影响。结果表明:水橇着水角、飞机着水水平速度与飞机着水垂向速度对水橇降载性能影响显著,合理地控制水橇的着水角与速度,可获得良好的降载效果。      

四点法圆度与轴系误差测量系统

通过四点法实现圆度、轴系误差的分离与补偿，可以获得很高的测量精度。本文讨论该系统的测量原理及相应机械结构、光电变换、信号采集和微机接口的设计要点。     

Measured properties of the cosmic background radiation

After a pioneering period when the observers were mainly interested in checking the general properties of the Cosmic Background Radiation through observations at still higher frequencies, the observational efforts are now devoted to the discovery of features in the mean panorama, in particular :i) Distortions in the frequency spectrum, ii) Spatial anisotropies at various angular scales; iii) Polarization. The observational information is reviewed.     

燃烧室中平均流速对速度耦合与压力耦合的影响

对热力发动机中存在的线性振荡燃烧的研究，通常假设速度耦合与压力耦合的作用独立无关且作用结果可以线性相加。本文通过对压耦合与速度耦合现象的分析，说明了使这一假设不合理的平均流速界限，并给予了实验证明。     

飞机前起落架支柱旋转机构角度及角速度测试方法的优化

本文介绍一种利用步进电机驱动某系列飞机前起落架操纵机构,在套筒与支柱旋转机构处采用平行四连杆结构的工装,利用旋转编码器实现操纵机构与支柱旋转机构角度与角速度精确测量的优化测试方法,并成功应用于测试设备。     

一种基于新三维随机Hough变换的航迹起始算法

针对雷达跟踪多目标时,目标点迹受杂波、噪声等因素影响,航迹起始难度大的问题,利用三维空间直线表示方法提出了一种4参数三维Hough变换算法.该算法是对传统二维Hough变换的拓展,它结合了传统的二维随机Hough变换理论,是一种新的三维随机Hough变换算法.通过该算法对理论数据和实测数据进行验证,结果表明,对于航迹区别较大的目标,该算法的航迹起始成功概率为98.5％;对于空间航迹相近的目标,该算法可成功将目标航迹从杂波中提取出来,虽然可能会出现航迹混淆,但利用目标先验信息可解决该问题,实现航迹起始.     

典型水文环境下航空声呐浮标双基地作用范围

航空声呐浮标双基地探测是应对水下目标声隐身能力持续提高的有效技术途径之一。分析了航空声呐浮标的指标,给出了双基地声呐配置,采用双基地声呐方程为依据,利用数值仿真的方法计算了 3种典型海洋环境条件下双基地声呐浮标探测范围,讨论了海洋环境对双基地声呐探测的影响,为航空声呐浮标双基地战术使用奠定技术基础。