排序方式: 共有49条查询结果,搜索用时 15 毫秒
21.
针对惯导系统中应用较为成熟的RS232、RS422、RS485、CAN 等数据传输
方法传输带宽低、可靠性低、距离近并且引入电磁干扰等问题,将基于IEEE-1394b 的光
通信引入惯导系统。利用惯导系统中FPGA 资源配合物理层芯片和光电转化模块,搭建
基于IEEE-1394b 的数据传输系统。详细介绍了各个模块的工作流程,为满足数据传输特
殊需求对链路层请求方式和数据包进行惯导专用化改进。借助QuartusⅡ 集成开发环境
提供的SignalTapⅡ逻辑分析仪进行验证。结果表明,数据传输系统可以使用立即请求发
送广播形式的异步数据包,也可以进行点对点异步数据传输,实现了预期目标。该方法
不仅屏蔽了惯性导航系统的外界电磁干扰,还实现了惯导系统的大带宽、高可靠传输,
具有很高的工程应用价值。 相似文献
22.
23.
24.
针对先进航空电子系统对数据网络的高速和混合通信的需求,基于分布式控制、实时存取和故障容忍的设计思想,进行了分布式光纤网络的结构设计和协议选择.重点分析了光纤链路、介质访问控制协议、拓扑、容错技术和网络管理软件.分析结果表明,基于1394b总线的分布式容错光纤网络能提供确定和可靠的通信,同时该吉比特光纤链路满足误码率要求且功率余量达13dB.因此它是具有高带宽、低延迟和易扩展优势的高综合网络结构. 相似文献
25.
Claudia Stummer Christian Siemes Roland Pail Björn Frommknecht Rune Floberghagen 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2012
This paper describes the upgrade of the GOCE Level 1b gradiometer processing as part of ESA’s Payload Data Segment (PDS). Four processing steps have been identified which can be improved: 1. The optimal determination of the angular rates of the satellite, based on a combination of star sensor and gradiometer data. This is the so-called angular rate reconstruction. 2. The optimal determination of the spacecraft’s attitude, again based on a combination of star sensor and gradiometer data. 3. The combination of data of all simultaneously available star sensors. And, 4. the calibration of the measured accelerations is improved by taking the time dependence of selected calibration parameters into account. 相似文献
26.
27.
对比分析经历模拟特定环境的环境交变试验、盐雾试验、加速老化试验和太阳辐射试验前后泡沫塑料的压缩强度、闭孔率、线胀系数和热导率等性能。结果表明,HCFC-141b型聚氨酯泡沫塑料经历环境老化后,压缩强度和热导率增加,线胀系数减小,闭孔率略有增加,热导率增加。太阳辐照试验对泡沫性能影响最大,试样SD-4压缩强度提高32%,闭孔率先增加后减少,线胀系数降低19%,热导率升高30%。 相似文献
28.
S.A. Wolff L.H. Coelho M. Zabrodina E. Brinckmann A.-I. Kittang 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2013
Successful growth and development of higher plants in space rely on adequate availability and uptake of water and nutrients, and efficient energy distribution through photosynthesis and gas exchange. In the present review, literature has been reviewed to assemble the relevant knowledge within space plant research for future planetary missions. Focus has been on fractional gravity, space radiation, magnetic fields and ultimately a combined effect of these factors on gas exchange, photosynthesis and transport of water and solutes. 相似文献
29.
S. Karakula W. Tkaczyk F. Giovannelli 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》1984,3(10-12)
In the spherical accretion onto massive objects, the matter may be heated up to temperatures as high as 1012 °K. In such a hot plasma, the thermal bremsstrahlung (e-e and e-p) and π° decay from inelastic collisions of protons are the main γ-ray sources. We determined the γ -ray production spectra from the π° decay and from bremsstrahlung for different temperatures. The expected γ-ray spectra were evaluated too in order to fit experimental data. We have fitted COS B data from 3C 273 using a two temperatures plasma model. The best fit is for
(M8 is the black hole mass in 108 M) which gives
. The hard X-ray measurements do not contradict the bremsstrahlung spectrum. 相似文献
Full-size image (1K)
30.
M.S. Skidmore R.M. Ambrosi 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2009,44(9):1019-1029
Understanding the evolution of Mars requires determining the composition of the surface and atmosphere of the planet. The European Space Agency’s ExoMars rover mission, which is expected to launch in 2016, is part of the Aurora programme. The instruments on the rover will search for evidence of life on Mars and will map a sub-section of the Martian surface, extracting compositional information. Currently our understanding of the bulk composition (and mineralogy) of Mars relies on orbital data from instruments on-board satellites such as 2001 Mars Odyssey, Mars Reconnaissance Orbiter and Mars Express, in addition to in-situ instrumentation on rovers such as Spirit and Opportunity. γ-ray spectroscopy can be used to determine the composition of Mars, but it has yet to be successfully carried out in-situ on Mars. This study describes some of the results obtained from the γ-ray spectrometer on 2001 Mars Odyssey during solar proton events and discusses whether the increased emissions are useful in γ-ray spectroscopy. The study shows that although increased γ-ray emissions were expected from the Martian surface during a solar proton event, they were not detected from orbit probably due to insufficient signal-to-background. However, this does not preclude the possibility of measuring changes in γ-ray flux corresponding to changes in solar activity on the surface of the planet. 相似文献