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S-ALOHA协议在无线接入系统中的实现 总被引：4，自引：0，他引：4
张静 《成都信息工程学院学报》2003,18(3):287-290
讨论了时分多址技术在点对多点无线通信系统中的应用，分析了S—ALOHA协议的性能，给出S—ALOHA在系统中的实现。 相似文献
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针对传统TDMA体制数据传输时延较大的缺点,提出了一种适用于卫星导航系统星间链路的可抢占时隙的TDMA体制,并抽象出了该TDMA体制下的时隙编排优化目标,结合卫星导航系统星座的星间可视性,以顶点着色为理论基础提出了一种优化的时隙编排算法。仿真结果表明,与GPS星间链路的TDMA体制相比,所提出的TDMA体制可达到相同的卫星自主定轨精度以及系统用户等效观测误差(URE)性能,同时大幅提高了系统通信性能。 相似文献
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Erik Swietlicki Jingchuan Zhou Olle H. Berg Bengt G. Martinsson Gran Frank Sven-Inge Cederfelt Ulrike Dusek Axel Berner Wolfram Birmili Alfred Wiedensohler Brett Yuskiewicz Keith N. Bower 《Atmospheric Research》1999,50(3-4)
The hygroscopic properties of sub-micrometer aerosol particles were studied in connection with a ground-based cloud experiment at Great Dun Fell, in northern England in 1995. Hygroscopic diameter growth factors were measured with a Tandem Differential Mobility Analyser (TDMA) for dry particle diameters between 35 and 265 nm at one of the sites upwind of the orographic cloud. An external mixture consisting of three groups of particles, each with different hygroscopic properties, was observed. These particle groups were denoted less-hygroscopic, more-hygroscopic and sea spray particles and had average diameter growth factors of 1.11–1.15, 1.38–1.69 and 2.08–2.21 respectively when taken from a dry state to a relative humidity of 90%. Average growth factors increased with dry particle size. A bimodal hygroscopic behaviour was observed for 74–87% of the cases depending on particle size. Parallel measurements of dry sub-micrometer particle number size distributions were performed with a Differential Mobility Particle Sizer (DMPS). The inorganic ion aerosol composition was determined by means of ion chromatography analysis of samples collected with Berner-type low pressure cascade impactors at ambient conditions. The number of ions collected on each impactor stage was predicted from the size distribution and hygroscopic growth data by means of a model of hygroscopic behaviour assuming that only the inorganic substances interacted with the ambient water vapour. The predicted ion number concentration was compared with the actual number of all positive and negative ions collected on the various impactor stages. For the impactor stage which collected particles with aerodynamic diameters between 0.17–0.53 μm at ambient relative humidity, and for which all pertinent data was available for the hygroscopic closure study, the predicted ion concentrations agreed with the measured values within the combined measurement and model uncertainties for all cases but one. For this impactor sampling occasion, the predicted ion concentration was significantly higher than the measured. The air mass in which this sample was taken had undergone extensive photochemical activity which had probably produced hygroscopically active material other than inorganic ions, such as organic oxygenated substances. 相似文献
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Karine Sellegri Paolo Villani David Picard Regis Dupuy Colin O'Dowd Paolo Laj 《Atmospheric Research》2008,90(2-4):272-ICNAA07
The hygroscopic growth factor (HGF) of 85 nm and 20 nm marine aerosol particles was measured during January 2006 for a three-week period within the frame of the EU FP6 project MAP (Marine Aerosol Production) winter campaign at the coastal site of Mace Head, using the TDMA technique. The results are compared to aerosol particles produced in a simulation tank by bubbling air through sea water sampled near the station, and through synthetic sea water (inorganic salts). This simulation is assimilated to primary production. Aitken and mode particles (20 nm) and accumulation mode particles (85 nm) both show HGF of 1.92 and 2.01 for particles generated through bubbling in natural and artificial sea water respectively. In the Aitken mode, the marine particles sampled in the atmosphere shows a monomodal HGF slightly lower than the one measured for sea salt particles artificially produced by bubble bursting in natural sea water (HGF = 1.83). This is also the case for the more hygroscopic mode of accumulation mode particles. In addition, the HGF of 85 nm particles observed in the atmosphere during clean marine sectors exhibits half of its population with a 1.4 HGF. An external mixture of the accumulation mode marine particles indicates a secondary source of this size of particles, a partial processing during transport, or an inhomogeneity of the sea water composition. A gentle 90 °C thermo-desorption results in a significant decrease of the number fraction of moderately hygroscopic (HGF = 1.4) particles in the accumulation mode to the benefit of the seasalt mode, pointing to the presence of semi-volatile compounds with pronounced hydrophobic properties. The thermo-desorption has no effect on the HGF of bubble generated aerosols, neither for synthetic or natural sea water, nor on the atmospheric Aitken mode, indicating that these hydrophobic compounds are secondarily integrated in the particulate phase. No difference between night and day samples is observed on the natural marine aerosols regarding hygroscopicity, but a more pronounced sensitivity to volatilization of the 1.4 HGF mode in the accumulation mode is observed during the day. 相似文献
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TDMA／SS系统同步技术 总被引：1，自引：0，他引：1
目前，通信卫星系统普遍采用星上信号处理技术，为了满足高容量系统的要求，近几年发展了许多新的技术，其中为了解决多个点波束区域的通信，被称为时分多址／星上交换（TDMA／SS）技术便应运而生。因为使用TDMA时，一方面需要所有地球站的时间系统与同一参考源保持同步，另一方面，参考源也必须与卫星上的同步窗相关。二十世纪七十年代，许多学提出了各种各样的TDMA／SS同步解决方案，在此详细论述了TDMA／SS系统同步中的一些主要问题，对解决同步的方案作了比较，并分析了各种方案的特点。 相似文献
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Hygroscopic growth of aerosol particles and its influence on nucleation scavenging in cloud: Experimental results from Kleiner Feldberg 总被引：8，自引：0，他引：8
Birgitta Svenningsson Hans-Christen Hansson Alfred Wiedensohler Kevin Noone John Ogren Anneli Hallberg Roy Colvile 《Journal of Atmospheric Chemistry》1994,19(1-2):129-152
The hygroscopic growth of individual aerosol particles has been measured with a Tandem Differential Mobility Analyser. The hygroscopic growth spectra were analysed in terms of diameter change with increasing RH from 20% to 85%. The measurements were carried out during the GCE cloud experiment at Kleiner Feldberg, Taunus, Germany in October and November 1990.Two groups of particles with different hygroscopic growth were observed. The less-hygroscopic group had average growth factors of 1.11, 1.04 and 1.02 for particle diameters of 50, 150 and 300 nm, respectively. The more-hygroscopic group had average growth factors of 1.34, 1.34, and 1.37 for the same particle diameters. The average fraction of less-hygroscopic particles was about 50%. Estimates of the soluble fractions of the particles belonging to the two groups are reported.Hygroscopic growth spectra for total aerosol, interstitial aerosol and cloud drop residuals were measured. A comparison of these hygroscopic growths of individual aerosol particles provides clear evidence for the importance of hygroscopic growth in nucleation scavenging. The measured scavenged fraction of particles as a function of diameter can be explained by the hygroscopic growth spectra. 相似文献
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