参量型空气折射率传感系统

本系统分别利用传感器测出空气的温度、气压和湿度三个参量,把测量值用一个通用于不同机型的接口电路连接到微机进行数据处理并计算出空气折射率值。文中叙述了传感器及其检测电路的设计原理,给出了检测和接口电路框图、计算公式和程序流程图。整个系统已通过联机调试和初步的对比试验。     

利用MF雷达对耀斑期间电离层D区电子密度的观测研究

利用MF雷达观测资料对X级别耀斑爆发期间在66-80km高度之间的电子密度进行了研究，观测到了耀斑爆发期间电子密度的突然增加，在较低高度上的电子密度的时间变化趋势与耀斑的软X射线辐射通量相关．电子密度的变化强度依赖于具体的耀斑参数，有些耀斑引起的电子密度增加高达400cm^-3，有些仅为100cm^-3左右．但耀斑期间在这一高度区间增加的总电子含量增量仅占耀斑辐射引起的整个电离层总电子含量增量的千分之一左右．最后，利用恢复阶段电子密度的时间变化过程估算了1997年11月4日耀斑期间部分高度上的有效复合系数．     

飞机V型外倾双垂尾载荷校准技术

根据垂尾载荷校准及建模需求,对飞机V型外倾双垂尾结构受载情况进行了分析和简化,确定了校准试验载荷,研制了垂尾载荷校准试验专用龙门梁架。采用液压协调加载技术,完成了外倾双垂尾载荷校准试验,建立了满足测载要求的载荷模型。此种方法充分利用了左右垂尾外倾、双垂尾之间空间较大的特点,对左右垂尾对称施加向外的单点、多点载荷,加载载荷侧向分量左右自平衡,垂向分量依靠飞机自身重量即可平衡,飞机不需要复杂的固定与约束。试验中采用先搭建龙门框架,再停放飞机的方法,降低了试验风险、加快了试验进度,取得了良好的试验结果,对其他此类结构的载荷校准具有一定的借鉴作用。     

飞机变形自动化测量方法研究

为解决以往飞机变形测量模式中人工干预较多,受测量环境影响较大,测量时间长等问题,基于Geo COM技术和RS232,在计算机与全站仪之间进行数据交换,设计了一套自动化测量系统。在测量过程中由标志点的机体理论坐标反算其在当前测站中的极坐标,从而在测量过程中驱动全站仪指向待测点,减少人工瞄准时间,并由计算机实时解算结果数据。经实际飞行试验验证表明,测量时间缩短为原来时间一半,大大提高了工作效率。     

用测量法调节某型涡轮的轮背间隙

Cooling Turbine 204050是波音737飞机采用的一种涡轮冷却器,其传统的调节轮背间隙的方法操作繁琐、效率低下。本文介绍了一种测量法来调节204050的轮背间隙,该方法具有可靠性高、操作方便、效率高等优点。     

双向比对高精度物理时间同步方法

提出一种面向未来卫星在轨应用的闭环物理高精度时间同步方法。比较了所提方法与其他时间同步方法的区别与优势，建立了远程系统时间同步基本模型与误差传递模型，基于双向测距和时间传递技术分析了高精度钟差获取原理，给出了时钟调整环路的时域频域参数依赖关系。完成了高精度时间同步地面试验系统构建，测试了开环非调钟状态下钟差测量精度误差、闭环调钟状态下时间同步准确度误差以及长时运行情况下的时间同步监测结果。测试结果表明，该方法能够实现优于1 ns量级的时间同步，为高精度时间同步技术研究提供了新的途径。     

Hybrid integration method for highly maneuvering radar target detection based on a Markov motion model

To detect highly maneuvering radar targets in low signal-to-noise ratio conditions, a hybrid long-time integration method is proposed, which combines Radon-Fourier Transform (RFT), Dynamic Programming (DP), and Binary Integration (BI), named RFT-DP-BI. A Markov model with unified range-velocity quantification is formulated to describe the maneuvering target’s motion. Based on this model, long-time hybrid integration is performed. Firstly, the whole integration time is divided into multiple time segments and coherent integration is performed in each segment via RFT. Secondly, non-coherent integration is performed in all segments via DP. Thirdly, 2/4 binary integration is performed to further improve the detection performance. Finally, the detection results are exported together with target range and velocity trajectories. The proposed method can perform the long-time integration of highly maneuvering targets with arbitrary forms of motion. Additionally, it has a low computational cost that is linear to the integration time. Both simulated and real radar data demonstrate that it offers good detection and estimation performances.     

基于激光的便携式飞机装配接缝质量检测仪及应用

介绍了一种基于激光的便携式接缝质量检测仪的工作原理及硬件组成。使用该检测仪对飞机缝隙和台阶阶差进行了测量,通过与人工测量进行对比验证,证明了该装置可实现对特征三维信息的快速自动检测,工作准确可靠。     

仿真代理在导弹制导半实物仿真试验系统中的应用

针对独立运行的导弹制导半实物仿真试验系统接入联合试验系统的问题，应用了仿真代理的方法。在对原有系统控制关系进行最小化的改造前提下，通过控制接口的转换，实现了半实物仿真试验系统与其它异类异构系统之间的互联，拓展了半实物仿真试验系统的应用。     

Observations of a quasi-90-day oscillation in the MLT winds and tides over an equatorial station using meteor radar winds

An evident signature of a least studied quasi-90-day oscillation is found in the winds and tides in the MLT from an equatorial station, São João do Cariri (7.4°S, 36.5°W). The oscillation is found to appear mainly in certain intervals with small but appreciable seasonal (fourth harmonic of annual oscillation) contribution. The maximum amplitude of the oscillation is found to be around 10 m/s in the zonal wind. The enhancement peak of the oscillation exhibits downward movement indicating a plausible role of upward moving waves/tides in carrying its imprint from below to the MLT. Similar oscillation feature in the tropospheric zonal wind and ozone may imply its lower atmospheric origin as a component of the intraseasonal oscillation (ISO) that moves upward by modulating the tides. Subsequently, the propagating tides (mainly semidiurnal) are enhanced by the ozone in the stratosphere through absorption of solar UV radiation and finally manifest the oscillation in the MLT. Consistency of the present findings with the past investigations are observed in some aspects of the oscillation, whereas existing mismatches in others are believed to be due to geophysical variability depending on space and time among various locations on the globe.