轨道测量差分精确定轨方法

航天器轨道精确测定重要环节之一是有效地消除观测系统误差,在轨道测量数据处理时,一类是利用轨道约束自校准技术来估算和校准系统误差,另一类可以应用测元差分方法来消除系统误差(例如导航卫星测定目标)。本文提出一种新的差分技术,即利用观测数据时序差分消除系统误差技术,并推导相应确定航天器轨道的公式。     

ATLAS2K--以信号描述为核心的可扩展的可移植的自动测试语言

详细介绍了以信号描述为核心的新一代测试语言ATLAS2K的特点及层模型，并提出了ATLAS2K在自动测试设备ATE中的应用。     

直升机主最低设备清单的确定

为提高民用直升机的利用率和经济性,可编制主最低设备清单(MMEL).根据AC313型机MMEL项目的经验,总结出民用直升机MMEL的确定逻辑决断程序,并探讨MMEL在军用直升机上的应用前景.     

The formation of sulfate and elemental sulfur aerosols under varying laboratory conditions: implications for early earth

The presence of sulfur mass-independent fractionation (S-MIF) in sediments more than 2.45?×?10(9) years old is thought to be evidence for an early anoxic atmosphere. Photolysis of sulfur dioxide (SO(2)) by UV light with λ?相似文献   

Potential climatic impact of organic haze on early Earth

We have explored the direct and indirect radiative effects on climate of organic particles likely to have been present on early Earth by measuring their hygroscopicity and cloud nucleating ability. The early Earth analog aerosol particles were generated via ultraviolet photolysis of an early Earth analog gas mixture, which was designed to mimic possible atmospheric conditions before the rise of oxygen. An analog aerosol for the present-day atmosphere of Saturn's moon Titan was tested for comparison. We exposed the early Earth aerosol to a range of relative humidities (RHs). Water uptake onto the aerosol was observed to occur over the entire RH range tested (RH=80-87%). To translate our measurements of hygroscopicity over a specific range of RHs into their water uptake ability at any RH < 100% and into their ability to act as cloud condensation nuclei (CCN) at RH > 100%, we relied on the hygroscopicity parameter κ, developed by Petters and Kreidenweis. We retrieved κ=0.22?±0.12 for the early Earth aerosol, which indicates that the humidified aerosol (RH < 100 %) could have contributed to a larger antigreenhouse effect on the early Earth atmosphere than previously modeled with dry aerosol. Such effects would have been of significance in regions where the humidity was larger than 50%, because such high humidities are needed for significant amounts of water to be on the aerosol. Additionally, Earth organic aerosol particles could have activated into CCN at reasonable-and even low-water-vapor supersaturations (RH > 100%). In regions where the haze was dominant, it is expected that low particle concentrations, once activated into cloud droplets, would have created short-lived, optically thin clouds. Such clouds, if predominant on early Earth, would have had a lower albedo than clouds today, thereby warming the planet relative to current-day clouds.     

基于模型参考模糊自适应的转台摩擦力矩补偿研究

为克服某型伺服转台在摩擦力矩干扰下引起的低速“爬行”问题,设计了基于模型参考模糊自适应的摩擦补偿控制方法;并基于所建立的数学模型对该摩擦补偿方法进行了lyapunov稳定性证明,采用Matlab进行了仿真试验分析。仿真结果表明,该摩擦补偿方法能够有效抑制摩擦干扰的不利影响,提升了转台低速跟踪的平稳性,从而显著提高了转台的低速伺服精度。