纳米校准与测试——基于纳米测量机的试验性研究

主要介绍了基于纳米测量机的高阶梯差台阶标准样板和深沟槽深度标准样板计量测试和校准工作研究,包括在NMM上对两种标准样板进行计量测试和校准、在NMM上安装不同的探测传感器时纳米级深度标准样板和台阶高度样板的校准比较、以及在研航空基金项目"在NMM上实现小型非球面的坐标扫描轮廓测量方法".     

三星对地面辐射源的高程修正定位算法与误差研究

提出了用最小二乘估计解算辐射源位置,在迭代过程中通过地理信息系统查询并不断修正目标高程,同时其定位误差进行了分析和仿真。结果表明,修正高程误差后可以改进目标高程定位精度,进而促进水平定位精度,水平定位精度的提高又会促进在高度上的定位,从而使整体的定位精度得到了改善。     

具有尖侧缘的非圆截面机身头部几何参数影响研究

有侧滑时,尖侧缘的非圆截面机身头部在中等和大迎角下,可具有方向稳定性.在计算研究的基础上,选择了3个不同上、下表面高度和两个不同侧缘角的模型进行了低速风洞试验.风洞试验结果表明,无侧滑时,机身的升力、阻力和俯仰力矩的绝对值都随高度增大而减小,在α<30°内,表面高度对横向特性影响较小,α=30~60°时,呈现复杂的影响趋势;尖锐侧缘机身比圆侧缘机身产生的升力和阻力都大些,但俯仰力矩差别不大;随着迎角的增大,对横向特性的影响明显;有侧滑时,上表面b/a=0.75的机身和下表面b/a=0.25的机身对方向稳定性的影响最显著,尖锐侧缘比圆侧缘对方向稳定性有更大的影响.     

不同边界层厚度下高马赫数进气道自起动过程研究

为了探寻入口边界层厚度变化对高马赫数进气道自起动性能的影响,对简化的二元高马赫数进气道的加速自起动过程进行数值仿真研究,分析了边界层厚度对自起动过程中流场波系结构变化和自起动性能的影响机制,获得了不同边界层厚度下的进气道自起动性能及主分离包高度的变化规律。结果表明:随着边界层相对厚度从0.05增加至0.3,进气道的自起动马赫数一开始保持不变,然后快速增大;相同主流条件下,不起动流场跨越主分离包无量纲压升和主分离包高度随边界层相对厚度的增大均变小;边界层动量损失厚度和跨越主分离包无量纲压升对进气道起动性能影响重大。     

定时定点月面着陆全程轨道控制设计

针对定时定点月面着陆的目标要求，提出了全程轨道控制设计方法。进行了包括地月转移、近月制动、环月降轨和动力下降的全程轨道控制的分段设计和联合规划，实现在入轨轨道偏差条件下的定时定点月面着陆。分别构建了中途修正、近月制动、环月降轨三段轨道控制的规划变量和目标参数；根据轨道倾角建立了动力下降点与着陆点的匹配转换关系。设计了中途修正、近月制动、环月降轨、动力下降的全程轨道控制策略的联合规划。建立了着陆位置偏差与轨道倾角偏差、着陆时间偏差与轨道半长轴偏差的修正关系，修正设计了中途修正目标倾角和近月制动目标半长轴。仿真算例表明，在入轨偏差轨道条件下，保证了中途修正后的飞行轨道与标称轨道基本一致，实现了与标称状态基本一致的定时定点月面着陆。可应用于月球着陆、月球采样返回以及载人登月等实施月面定时定点着陆任务的轨道设计和控制实施。     

多普勒导航雷达测高自校信号的分析

本文详细分析了采用周期自动校准技术的多普勒导航雷达测高装置自校时的信号关系。在数学分析的基础上,作者认为,为保证在高度测量时稳定获取自校信号,应调节馈线的长度(微波相位)。实验证明,分析是正确的。     

基于FPGA的天线控制系统设计

介绍一种基于 FPGA(Field Program mable Gate Array)的共轴式双旋翼无人驾驶直升机遥测遥控数字引导的天线控制系统的设计方案 ,讨论其总线控制、步进电机控制、输入信号处理模块的设计思路及关键技术。该系统经过设计、布线、仿真测试 ,并应用于某型号无人驾驶直升机     

Comparing topside and bottomside-measured characteristics of the F2 layer peak

The ionospheric characteristics of the F2 layer peak have been measured with ionosondes from the ground or with satellites from space. The most common characteristics are the F2-peak density NmF2 and peak height hmF2. In addition to these two parameters this paper studies the F2-peak scale height. Comparing the median values of hmF2 and NmF2 obtained from topside and bottomside sounding shows good agreement in general. The Chapman scale height values for the F2 layer peak derived from topside profiles, H_m,top, are generally several times larger than H_m,bot derived from bottomside profiles.     

0 °C isotherm height for satellite communication in Malaysia

The 0 °C isotherm height is an important parameter for prediction of rain attenuation of microwave and millimeter wave for Earth-space communication. The variations of 0 °C isotherm heights for two monsoon seasons have been studied based on an analysis of radiosonde over three stations. The exceedence probability statistics of rain height are compared between the two seasons. The results on the 0 °C isotherm height can be utilized for the estimation of attenuation of microwave and millimeter wave due to rain over Earth-space paths. Attenuations of radio wave due to rain at frequencies above 10 GHz and above have also been estimated using the 0 °C isotherm height so derived.     

Variations in the ionospheric scale height parameter at the F2 peak over Grahamstown,South Africa

The Grahamstown, South Africa (33.3°S, 26.5°E) ionospheric field station operates a Lowell digital pulse ionospheric sounder (Digisonde) whose output includes scaled parameters derived from the measured ionogram. One of these output parameters is the ionospheric scale height parameter (H), and this paper presents an analysis of the seasonal, diurnal, and solar activity variations of this parameter over the Grahamstown station. Ionosonde data from three years 2002, 2003, and 2004 were used in this study. The data was subjected to a general trend analysis to remove any outliers and then the monthly median data were used to explore the different variations. The results of this analysis were found to be similar to what has already been presented in the literature for low latitude stations, and are presented as well as the correlation at this mid-latitude station between the H parameter, the IRI shape parameter (B0), and the peak electron density (NmF2).