导弹翼面结构摄动矩阵法可靠性设计研究

给出了导弹翼面结构可靠性预测与可靠性设计的随机有限元摄动矩阵法的基本原理与算式；提出对翼面壁板厚度作可靠性设计的思路，并用ＦＯＲＴＲＡＮ语言编制了可在微机上运行的计算机程序。试算表明：由本文方法得到的结果与试验数据的统计分析结果十分一致。本文的方法可以应用于常用的战术导弹翼面结构的可靠性预测与可靠性设计。     

高精度星间微波测距技术

卫卫跟踪（SST）技术是目前地球重力场测量最有价值和应用前景的方法之一。高精度K波段星间微波测距系统（KBR K Band Ranging System）低低卫卫跟踪（SST-Ⅱ）重力卫星的关键有效载荷，它是一微米量级的测距系统，通过处理高精度的星间距离和距离变化率数据，可以恢复出地球重力场。在研究星间双路微波测距原理的基础上，提出了一种KBR系统的基本结构，详细描述了数据处理过程和KBR系统研究需要突破的关键技术，分析了国内目前的研究水平，给出了我国未来开展KBR系统研究的一些建议。     

武汉上空中层顶大气重力波活动的钠层荧光激光雷达观测研究

从中国科学院武汉物理与数学研究所钠荧光激光雷达自1999年至今的观测数据中选取了分布于全年26天的数据进行重力波活动的分析研究.统计结果表明,武汉中层顶区的重力波活动非常频繁:26天总观测时间累计约为185.5 h,总共观测到124个重力波活动,平均发生频度为每小时0.7个波,且波的出现频度与地方时有一定关系.这些波的垂直波长主要分布在3-7km,垂直相速主要位于0.1-0.5 m/s.与国外报道的结果相比较,波长数值与分布较为一致,但相速明显较低.武汉中层顶区重力波活动的另一特点是多波过程很频繁,多、单波过程的出现比例约为3:2.利用钠层相对密度扰动时空图方法,给出了武汉中层顶区重力波传播和破碎现象的典型结果.还利用单色波模型对部分钠层数据进行了单色波相关参数的提取.      

Gravity modeling in aerospace applications

The science of inertial navigation has evolved to the point that the traditional gravity model is a principal error source in advanced, precise systems. Specifically, the unmodeled vertical deflections of the earth's gravitational field are a major contributor to CEP (circular error probable) divergence in precise terrestrial inertial navigation systems (INS). Over the years, several studies have been undertaken to the development of advanced techniques for accurate, real-time compensation of gravity disturbance vectors. More complex on-board gravity models which compute vertical deflection components will reduce the CEP divergence rate, but imperfect modeling due to on-board processing limitations will still cause residual vertical deflection errors. In order to eliminate or reduce gravity-induced errors in the INS requires measurement of gravity disturbance values and in-flight compensation to the inertial navigator. It is assumed in this paper that gravity disturbance values have been measured prior to the airborne mission and various techniques for compensation are to be considered. As part of a screening process in this study, several gravity compensation techniques (both deterministic and stochastic models) were investigated. The screening process involved identification of gravity models and algorithms, and developments of selection criteria for subsequent screening of the candidates.     

偏置动量卫星耦合通道外干扰力矩补偿方法

为实现偏置动量卫星滚动-偏航耦合通道外干扰力矩的前馈补偿,根据两通道的姿态动力学模型,从理论上分析了包括常值与周期干扰的外干扰力矩对滚动-偏航姿态的影响。由此导出飞轮前馈补偿项的数学表达式,并论证了引入外力矩对飞轮角动量进行卸载的必要性。仿真结果表明,该法能有效削弱外干扰力矩对星体姿态尤其是偏航姿态的影响,大幅提高星体控制精度。     

气动力矩和重力梯度矩实现微小卫星三轴姿态控制

提出运用低轨道两个主要环境力矩 (重力梯度矩和气动力矩 )实现微小卫星三轴姿态被动控制方案。重力梯度矩提供俯仰和滚转恢复力矩 ,气动力矩提供偏航和俯仰恢复力矩 ;通过姿态稳定性分析和姿控过程动态仿真 ,结果表明此卫星具有结构简单、姿态稳定精度高的优点。     

GPS-only gravity field recovery with GOCE,CHAMP, and GRACE

Gravity missions such as the Gravity field and steady-state Ocean Circulation Explorer (GOCE) are equipped with onboard Global Positioning System (GPS) receivers for precise orbit determination (POD), instrument time-tagging, and the extraction of the long wavelength part of the Earth’s gravity field. The very low orbital altitude of the GOCE satellite and the availability of dense 1 s GPS tracking data are ideal characteristics to exploit the contribution of GPS high-low Satellite-to-Satellite Tracking (hl-SST) to gravity field determination. We present gravity field solutions based on about 8 months of GOCE GPS hl-SST data from 2009 and compare the results with those obtained from the CHAllenging Minisatellite Payload (CHAMP) and Gravity Recovery And Climate Experiment (GRACE) missions. The very low orbital altitude of GOCE significantly improves gravity field recovery from GPS hl-SST data above degree 20, but not for the degrees below 20, where the quality of the spherical harmonic coefficients remains essentially unchanged. Despite the limited time span of GOCE data used, the gravity field of the Earth can be resolved up to about degree 115 using GPS data only. Empirically determined phase center variations (PCVs) of the GOCE onboard GPS helix antenna are, however, mandatory to achieve this performance.     

Impact of covariance information of kinematic positions on orbit reconstruction and gravity field recovery

Gravity missions are equipped with onboard Global Positioning System (GPS) receivers for precise orbit determination (POD) and for the extraction of the long wavelength part of the Earth’s gravity field. As positions of low Earth orbiters (LEOs) may be determined from GPS measurements at each observation epoch by geometric means only, it is attractive to derive such kinematic positions in a first step and to use them in a second step as pseudo-observations for gravity field determination. The drawback of not directly using the original GPS measurements is, however, that kinematic positions are correlated due to the ambiguities in the GPS carrier phase observations, which in principle requires covariance information be taken into account. We use GRACE data to show that dynamic or reduced-dynamic orbit parameters are not optimally reconstructed from kinematic positions when only taking epoch-wise covariance information into account, but that essentially the same orbit quality can be achieved as when directly using the GPS measurements, if correlations in time are taken into account over sufficiently long intervals. For orbit reconstruction covariances have to be considered up to one revolution period to avoid ambiguity-induced variations of kinematic positions being erroneously interpreted as orbital variations. For gravity field recovery the advantage is, however, not very pronounced.     

Remote sounding of atmospheric gravity waves with satellite limb and nadir techniques

Recent advances in satellite techniques hold great potential for mapping global gravity wave (GW) processes at various altitudes. Poor understanding of small-scale GWs has been a major limitation to numerical climate and weather models for making reliable forecasts. Observations of short-scale features have important implication for validating and improving future high-resolution numerical models. This paper summarizes recent GW observations and sensitivities from several satellite instruments, including MLS, AMSU-A, AIRS, GPS, and CLAES. It is shown in an example that mountain waves with horizontal wavelengths as short as 30 km now can be observed by AIRS, reflecting the superior horizontal resolution in these modern satellite instruments. Our studies show that MLS, AMSU-A and AIRS observations reveal similar GW characteristics, with the observed variances correlated well with background winds. As a complementary technique, limb sounding instruments like CRISTA, CLAES, and GPS can detect GWs with better vertical but poorer horizontal resolutions. To resolve different parts of the broad GW spectrum, both satellite limb and nadir observing techniques are needed, and a better understanding of GW complexities requires joint analyses of these data and dedicated high-resolution model simulations.     

深空探测重力模拟飞行器方案设想

为解决失重环境对航天员生理健康的影响,在调研国内外重力飞行器研究现状的基础上,结合重力模拟飞行器的原理及人造重力舒适度影响因素,提出了一种通过自旋产生人造重力的深空探测飞行器方案设想。最后给出了重力模拟飞行器建设的实施规划、总体方案、在轨组装流程及技术难点。深空探测重力模拟飞行器稳定运转可为空间工作生活的航天员提供与地面无异的重力环境,将为执行深空探测任务提供必要的环境保障。