内装式空射运载火箭重力出舱机箭耦合动力学分析

研究了以运输机为平台的内装式运载火箭空射过程载机和火箭的耦合动力学建模。建模针对两个阶段：第一阶段，火箭固定于载机机舱内，两者构成一个整体，按照普通刚体的力学方法处理；第二阶段，火箭解锁后，沿着舱内的发射筒向外滑行，载机和火箭形成两刚体相互作用的耦合系统，基于牛顿-欧拉法建立系统动力学模型。载机在空射火箭过程中，油门和升降舵满偏，在加速前飞的同时拉大姿态俯仰角，火箭在自身重力分量和惯性力的作用下，沿着机舱内的发射筒加速向外滑行，直至与载机分离。数值仿真分析了空射过程载机的重要力学参数的变化过程，验证了载机操控策略的可行性和安全性，可为未来中国空射运载火箭技术设计提供数据参考。     

捷联式航空重力测量系统的数据处理方法比较与分析

重力数据处理对获取高精度重力异常值有着重要作用，是重力测量的核心技术。重力仪在搭载运动载体进行重力测量时，载体的高频振动对重力测量数据和GPS数据均会产生不可避免的干扰，导致提取的重力异常粗值含有大量高频噪声。围绕重力数据的处理方法这一核心技术，介绍了FIR低通滤波、零相移滤波、标准Kalman滤波、正反Kalman滤波4种滤波方法的基本原理，运用这4种方法处理了SAG捷联式重力仪的某次实际飞行测量数据，比对了基于SINS/GPS组合导航和SINS/DGPS组合导航的重力测量数据处理结果。通过对本次试验重复测线内符合精度进行比对，验证了4种方法的可行性和优劣性，同时验证了SAG重力仪的测量精度。     

Simulating planetary wave propagation to the upper atmosphere during stratospheric warming events at different mountain wave scenarios

Parameterization schemes of atmospheric normal modes (NMs) and orographic gravity waves (OGWs) have been implemented into the mechanistic Middle and Upper Atmosphere Model (MUAM) simulating atmospheric general circulation. Based on the 12-members ensemble of runs with the MUAM, a composite of the stratospheric warming (SW) has been constructed using the UK Met Office data as the lower boundary conditions. The simulation results show that OGW amplitudes increase at altitudes above 30 km in the Northern Hemisphere after the SW event. At altitudes of about 50 km, OGWs have largest amplitudes over North American and European mountain systems before and during the composite SW, and over Himalayas after the SW. Simulations demonstrate substantial (up to 50–70%) variations of amplitudes of stationary planetary waves (PWs) during and after the SW in the mesosphere-lower thermosphere of the Northern Hemisphere. Westward travelling NMs have amplitude maxima not only in the Northern, but also in the Southern Hemisphere, where these modes have waveguides in the middle and upper atmosphere. Simulated variations of PW and NM amplitudes correspond to changes in the mean zonal wind, EP-fluxes and wave refractive index at different phases of the composite SW events. Inclusion of the parameterization of OGW effects leads to decreases in amplitudes (up to 15%) of almost all SPWs before and after the SW event and their increase (up to 40–60%) after the SW in the stratosphere and mesosphere at middle and high northern latitudes. It is suggested that observed changes in NM amplitudes in the Southern Hemisphere during SW could be caused by divergence of increased southward EP-flux. This EP-flux increases due to OGW drag before SW and extends into the Southern Hemisphere.     

Case study of inclined sporadic E layers in the Earth’s ionosphere observed by CHAMP/GPS radio occultations: Coupling between the tilted plasma layers and internal waves

We have used the radio occultation (RO) satellite data CHAMP/GPS (Challenging Minisatellite Payload/Global Positioning System) for studying the ionosphere of the Earth. A method for deriving the parameters of ionospheric structures is based upon an analysis of the RO signal variations in the phase path and intensity. This method allows one to estimate the spatial displacement of a plasma layer with respect to the ray perigee, and to determine the layer inclination and height correction values. In this paper, we focus on the case study of inclined sporadic E (E_s) layers in the high-latitude ionosphere based on available CHAMP RO data. Assuming that the internal gravity waves (IGWs) with the phase-fronts parallel to the ionization layer surfaces are responsible for the tilt angles of sporadic plasma layers, we have developed a new technique for determining the parameters of IGWs linked with the inclined E_s structures. A small-scale internal wave may be modulating initially horizontal E_s layer in height and causing a direction of the plasma density gradient to be rotated and aligned with that of the wave propagation vector k. The results of determination of the intrinsic wave frequency and period, vertical and horizontal wavelengths, intrinsic vertical and horizontal phase speeds, and other characteristics of IGWs under study are presented and discussed.     

不同重力环境下间隙铰链关节磨损分析

为研究不同重力环境对空间机构间隙铰链关节磨损的影响，将机械系统摩擦学行为和动力学行为相耦合，建立了磨损与动力学耦合分析模型和数值计算框架。首先采用非线性弹簧阻尼模型作为间隙处接触碰撞力的计算模型，同时采用Coulomb 法来计算运动副间隙处的摩擦力，进而建立了含间隙的机构动力学模型；然后通过基于Archard磨损模型二次开发的ANSYS程序来计算磨损，其中运用节点位移的方法来描述磨损过程。结果表明：当间隙关节转速较低时，重力对于关节轴承的磨损分布和磨损程度的影响很大，轴承出现集中磨损现象，磨损间隙急剧增加，严重影响机构的性能和精度；随着关节转速升高，重力对间隙关节磨损的影响逐渐减弱，轴承的磨损分布、磨损程度和关节最大磨损间隙的增长率将逐渐与微重力环境下趋同。     

机载托架自动校准系统的设计与实现

为了解决机载托架传统校准方法精度低、耗时、费力等问题,设计了一种高精度、高效率并且操作简单的成品托架自动校准系统。该系统运用调平精度较高的"循环多次"最高点不动调平方法,建立高精度机载托架校准的静力学数学模型,运用VC与Matlab的COM接口编程技术开发机载托架自动校准系统,并建立良好的人机交互界面。试验结果表明,利用该方法对机载托架进行校准,无论是校准精度还是校准效率都较传统方法有很大提高。     

ZSGA?2型重力敏感器关键技术分析与试验验证

与国外主流海洋重力仪相比，国产海洋重力仪的分辨率低一个数量级，这制约了国产海洋重力仪的应用。针对国产海洋重力仪亟需提高分辨技术的需求，根据ZSGA-2型重力敏感器的工作原理，建立了弹性系统的力学模型，并开展了样机的静态性能测试。测试结果表明，经零位漂移和大地固体潮汐修正后的静态精度达到了0.03mGal，样机随重力仪进行楼层高差测量的重复性为0.15mGal。该型重力敏感器的分辨率已经达到了国外同类产品的技术水平，并具备了一定的动态适应性，为该型高分辨率零长弹簧重力敏感器开展高动态环境适应性技术研究奠定了坚实基础。     

超导重力仪器:机遇与挑战

超导重力仪器是利用超导电性构建的精密相对重力测量仪器，其工作于4.2K液氦温度，具有仪器固有噪声低、稳定性好的特点。阐述了超导重力仪和超导重力梯度仪两种仪器的工作原理与技术特征，简要介绍了作者所在课题组超导重力仪器研制的进展情况。分析了我国资源勘查用航空超导重力梯度仪研制所面临的机遇与挑战，提出了应对技术挑战的策略方法。     

平台式重力仪航空重力测量数据后处理技术研究

针对航空重力测量对数据后处理的要求,结合平台式重力仪系统的组成与工作原理,在重力异常信号的频域特征基础上,设计出一套有严格频域规范的航空重力数据后处理流程,并对某海域实测数据进行了处理。结果表明,重力异常值内符合精度为12条东西测线达到0.43mGal/140s和0.84mGal/100s,4条南北测线达到0.39mGal/140s和0.79mGal/100s;以同测线GT-2A单次测量结果为标准值统计标准差,12条东西测线为0.72mGal/140s和0.98mGal/100s,4条南北测线为1.41mGal/140s和1.53mGal/100s。结果表明,设计的航空重力测量数据后处理方法可以实现重力异常信号的高精度提取。     

三维数模随动下的机翼结构重量优化

目前,基于快速建模下的重量重心估算系统得到了快速发展。为了进一步提高结构重量估算精度,研究了如何在重量重心快速分析(WCGA)系统环境中构建优化模块。以机翼结构重量优化为例,提出优化流程,对优化模块功能进行分解,给出模型简化要求。以A320飞机机翼为例,对梁和长桁进行优化,结果显示,经过优化,有效减轻了结构重量,且相比于传统的减重优化设计方法,极大提高了计算效率。