旋转弹气动力建模与飞行轨迹仿真

运用一种自回归滑动平均(ARMA)的时域气动力建模方法,以计算流体力学与刚体动力学(CFD/RBD)耦合仿真的输出结果为样本,对旋转弹的非定常气动力进行建模。利用建立的气动力模型与刚体动力学方程求解模块耦合,实现了旋转弹轨迹的快速仿真,并讨论了不同的建模方式对仿真精度的影响。算例结果表明:采用气动力模型与刚体动力学方程耦合仿真技术可以在不同初始发射条件下进行旋转弹飞行姿态与运动轨迹预测,且与CFD/RBD仿真结果吻合较好,证明ARMA气动力建模方法可以在保证旋转弹轨迹预测精度的同时大幅缩短仿真时间,节省计算资源。     

应用于超级电容储能系统的双向DC/DC变换器混沌控制方法研究

超级电容储能系统(SCESS)主要通过对双向DC/DC变换器进行控制来快速平抑直流母线电压的波动。为了抑制控制过程中所产生的一些分岔和混沌现象,提出了一种应用于SCESS的混沌控制方法。分析了该方法的控制原理,并根据非线性动力学理论建立了双向DC/DC变换器的离散迭代模型；然后设计了一种能够自动调节补偿斜率的混沌控制信号；最后对该信号作用下的异步切换函数和同步切换映射式进行了数值求解,从而绘出系统分叉图。通过仿真和试验证明,该方法能够有效抑制SCESS的分岔和混沌现象,提高了系统的稳定工作范围和动态响应速度。     

基于双力源的叠加式多维力传感器校准装置研究CSCD

介绍了一种基于叠加机原理的双力源多维力传感器校准装置的设计与研制,对装置的测量不确定度进行了分析,通过对三分量力传感器的校准实验,证明了校准装置不仅可以对多分量力传感器进行单分量校准,还能方便地实现耦合误差的校准。     

Modeling novel methodologies for unmanned aerial systems–Applications to the UAS-S4 Ehecatl and the UAS-S45 Bálaam

The rising demand for Unmanned Aerial Systems(UASs) to perform tasks in hostile environments has emphasized the need for their simulation models for the preliminary evaluations of their missions. The efficiency of the UAS model is directly related to its capacity to estimate its flight dynamics with minimum computational resources. The literature describes several techniques to estimate accurate aircraft flight dynamics. Most of them are based on system identification. This paper presents an alternative methodology to obtain complete model of the S4 and S45 unmanned aerial systems. The UAS-S4 and the UAS-S45 models were divided into four sub-models, each corresponding to a specific discipline: aerodynamics, propulsion, mass and inertia, and actuator. The‘‘aerodynamic" sub-model was built using the Fderivatives in-house code, which is an improvement of the classical DATCOM procedure. The ‘‘propulsion" sub-model was obtained by coupling a two-stroke engine model based on the ideal Otto cycle and a Blade Element Theory(BET) analysis of the propeller. The ‘‘mass and the inertia" sub-model was designed utilizing the Raymer and DATCOM methodologies. A sub-model of an actuator using servomotor characteristics was employed to complete the model. The total model was then checked by validation of each submodel with numerical and experimental data. The results indicate that the obtained model was accurate and could be used to design a flight simulator.     

地面飞行模拟器动力学建模与应用研究

地面飞行模拟器的训练效果主要取决于动力学建模的逼真度和满足正常/特殊情况飞行任务的程度。首先,分析了影响飞机动力学特性和飞行员操作各个因素的相互关系,旨在从任务飞行、故障飞行和特殊环境条件飞行三方面拓展地面飞行模拟器的模拟能力;其次,进行了飞机空中编队、方向舵故障、雨中飞行以及非线性起落架减振支柱的仿真。研究结果表明,拓展地面飞行模拟器的应用范围是实际飞行的需要且技术可行,关注细节的部件建模更是提高地面飞行模拟器逼真度和可信度的关键。     

小型固定翼无人机绳钩回收过程动力学分析

绳钩回收作为小型固定翼无人机的一种精确定点拦阻无损回收技术,近年来在国内外得到迅速发展。本文以某型无人机的绳钩回收系统为研究对象,对绳钩回收系统进行了参数化处理并建立了两种动力学仿真模型。一是在考虑回收架柔性基础上建立了基于Lagrange方程的绳钩回收系统的动力学仿真模型,二是在考虑绳索变形和系统结构细节基础上建立了基于MSC.ADAMS的绳钩回收系统的多体动力学仿真模型。通过上述两种仿真模型的算例分析以及与某型无人机绳钩回收试验的测试数据作对比,验证了两种动力学仿真模型在绳钩回收系统不同设计阶段的适用性和有效性。     

一种温度动态调节方法及其动态性能仿真研究

航空气源模拟试验台主要用于模拟不同飞行状态时发动机给空气管理系统的供气,由于飞机爬升、降落时发动机供气参数会急剧变化,因此航空气源模拟试验台需具备动态能力.基于一种温度动态调节方法,在合理简化的基础之上采用NHT方法对其温度动态性能进行了仿真研究,仿真结果表明该温度动态调节方法能够满足温度动态性能需求,对动态航空气源模拟试验台的设计选型有较高的参考价值.     

涡环伞降末敏子弹的稳态扫描动力学特性

综合采取理论建模、高空自由落体试验及可视化仿真相结合的方法,研究了一种涡环伞降末敏子弹的稳态扫描动力学特性。基于第一类拉格朗日方程,建立了由弹体、降落伞、伞盘、摩擦盘、连杆所组成的五刚体动力学模型,并应用ADAMS、MATALB及VR相结合的方法进行了弹道计算和可视化仿真研究。通过在高空热气球上投放试验样弹的方法,得到了伞弹系统的运动图像、平均落速、转速等弹道数据。对比研究得出:涡环伞的运动稳定性良好,可使末敏子弹保持匀速旋转降落状态,弹体达到稳定后的落速约为13.5 m/s,转速约为3 r/s,稳态扫描角接近于弹体的静态悬挂角,仿真计算与试验结果的一致性较好。      

考虑非理想噪声干扰的直升机飞行动力学模型辨识方法

利用MATLAB/SIMULINK平台搭建了直升机仿真实验系统，并以UH-60直升机为对象实现了考虑非理想噪声干扰的仿真飞行实验。建立了非理想噪声数学模型并基于增广最小二乘法设计 了一套同时考虑模型参数和噪声参数的综合辨识算法，在此基础上，利用仿真实验数据实现了UH-60直升机纵向飞行动力学模型的辨识与验证。最后，通过与普通最小二乘法的对比验证了本文方法的优越性。      

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.