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现代产权制度的重要内容之一是产权要具有可交易性。对资不抵债、无规模效益、重复建设、资产闲置的国有企业实施出售、兼并、股份转让等产权交易 ,可实现资源的有效配置 ,完成国有经济的战略性调整。在产权交易过程中 ,为防止国有资产的流失 ,提高社会经济效益 ,保护国家和人民的利益 ,应充分注意国有企业产权交易中的资产定价、资产有价证券化、资本市场及产权交易效率等问题 相似文献
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科技论文的投稿策略 总被引:1,自引:1,他引:1
徐行 《西安航空技术高等专科学校学报》2007,25(3):77-80
目的为作者的科技论文写作和成功投稿提供借鉴和帮助;方法以编辑的视角多方面解读影响科技论文投稿命中率的因素;结果从了解并选择所投刊物,撰写科技论文应有的几个注重,投稿时若干注意事项和策略等三方面分析了科技论文的投稿策略;结论论文投稿有技巧和策略可循,但是作者真正应下工夫的地方,不是囿于方法,也不是囿于投稿策略和人际关系,而是要多参加科研实践,掌握素材,勤于笔耕,保证论文的学术价值。 相似文献
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目前,企业社会责任运动从西方向全世界扩散和渗透,日益为人们所认可和接受,成为一种国际潮流,对企业自身的可持续发展以及国际贸易的进步都具有重要的意义。在“文化与有效性模型”等相关理论模型的基础上,简析国际企业社会责任运动的新趋势,并重点阐述其对中国企业文化的深刻而具有长远意义的作用,指出在企业、政府、社会的大力支持下,中国企业文化要向与国际企业社会责任运动相融合的方向前进,才具有生命力。 相似文献
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丁照祥 《中国民航学院学报》1990,(4)
本文提出采用适当参数的短幅外摆线的等距线替代产生自交的短幅外摆线的等距线或复合齿形作为摆线轮的齿形,以便于既能够保持复合齿形提高效率的目的,又能够简化工艺,提高工效,同时满足摆线齿的修形要求,增大齿顶强度,使啮合传动平稳。文中还给出了一种机型的计算结果和放大的图样。 相似文献
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在几何不可调的二元外压式斜板进气道的设计中,选择合理的斜板和唇口几何能数是最重要的问题之一。本文对一个设计马赫数为1.8的这类进气道的斜板和唇口参数进行了风洞试验研究。用缩尺模型风洞试验,对比分析了不同斜板角和不同外侧唇口内唇角,唇缘半径对进气道内流特性的影响,结果表明,对确定的进气道布局,斜板角小的变化对进气道超音速内流总压恢复系数,稳态出口流场周向畸变指数及喘振裕度的影响很大,唇口参数小的改变 相似文献
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为分析活动目标的随机飞行状态和减小导弹的脱靶量,提出了数学模拟打靶的一种新方法。其中包括卡尔曼滤波理论结合最大似然法的应用,以及建立相对运动的离散化模型和灵敏度矩阵。为改善飞行状态的估计精度,论述了确立飞行弹道修正协方差矩阵的概念。除此之外,还讨论了导引敏感器静态误差影响脱靶量的估计问题。 相似文献
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S. M. Krimigis D. G. Mitchell D. C. Hamilton S. Livi J. Dandouras S. Jaskulek T. P. Armstrong J. D. Boldt A. F. Cheng G. Gloeckler J. R. Hayes K. C. Hsieh W.-H. Ip E. P. Keath E. Kirsch N. Krupp L. J. Lanzerotti R. Lundgren B. H. Mauk R. W. McEntire E. C. Roelof C. E. Schlemm B. E. Tossman B. Wilken D. J. Williams 《Space Science Reviews》2004,114(1-4):233-329
The magnetospheric imaging instrument (MIMI) is a neutral and charged particle detection system on the Cassini orbiter spacecraft designed to perform both global imaging and in-situ measurements to study the overall configuration and dynamics of Saturn’s magnetosphere and its interactions with the solar wind, Saturn’s atmosphere, Titan, and the icy satellites. The processes responsible for Saturn’s aurora will be investigated; a search will be performed for substorms at Saturn; and the origins of magnetospheric hot plasmas will be determined. Further, the Jovian magnetosphere and Io torus will be imaged during Jupiter flyby. The investigative approach is twofold. (1) Perform remote sensing of the magnetospheric energetic (E > 7 keV) ion plasmas by detecting and imaging charge-exchange neutrals, created when magnetospheric ions capture electrons from ambient neutral gas. Such escaping neutrals were detected by the Voyager l spacecraft outside Saturn’s magnetosphere and can be used like photons to form images of the emitting regions, as has been demonstrated at Earth. (2) Determine through in-situ measurements the 3-D particle distribution functions including ion composition and charge states (E > 3 keV/e). The combination of in-situ measurements with global images, together with analysis and interpretation techniques that include direct “forward modeling’’ and deconvolution by tomography, is expected to yield a global assessment of magnetospheric structure and dynamics, including (a) magnetospheric ring currents and hot plasma populations, (b) magnetic field distortions, (c) electric field configuration, (d) particle injection boundaries associated with magnetic storms and substorms, and (e) the connection of the magnetosphere to ionospheric altitudes. Titan and its torus will stand out in energetic neutral images throughout the Cassini orbit, and thus serve as a continuous remote probe of ion flux variations near 20R
S (e.g., magnetopause crossings and substorm plasma injections). The Titan exosphere and its cometary interaction with magnetospheric plasmas will be imaged in detail on each flyby. The three principal sensors of MIMI consists of an ion and neutral camera (INCA), a charge–energy–mass-spectrometer (CHEMS) essentially identical to our instrument flown on the ISTP/Geotail spacecraft, and the low energy magnetospheric measurements system (LEMMS), an advanced design of one of our sensors flown on the Galileo spacecraft. The INCA head is a large geometry factor (G ∼ 2.4 cm2 sr) foil time-of-flight (TOF) camera that separately registers the incident direction of either energetic neutral atoms (ENA) or ion species (≥5∘ full width half maximum) over the range 7 keV/nuc < E < 3 MeV/nuc. CHEMS uses electrostatic deflection, TOF, and energy measurement to determine ion energy, charge state, mass, and 3-D anisotropy in the range 3 ≤ E ≤ 220 keV/e with good (∼0.05 cm2 sr) sensitivity. LEMMS is a two-ended telescope that measures ions in the range 0.03 ≤ E ≤ 18 MeV and electrons 0.015 ≤ E≤ 0.884 MeV in the forward direction (G ∼ 0.02 cm2 sr), while high energy electrons (0.1–5 MeV) and ions (1.6–160 MeV) are measured from the back direction (G ∼ 0.4 cm2 sr). The latter are relevant to inner magnetosphere studies of diffusion processes and satellite microsignatures as well as cosmic ray albedo neutron decay (CRAND). Our analyses of Voyager energetic neutral particle and Lyman-α measurements show that INCA will provide statistically significant global magnetospheric images from a distance of ∼60 R
S every 2–3 h (every ∼10 min from ∼20 R
S). Moreover, during Titan flybys, INCA will provide images of the interaction of the Titan exosphere with the Saturn magnetosphere every 1.5 min. Time resolution for charged particle measurements can be < 0.1 s, which is more than adequate for microsignature studies. Data obtained during Venus-2 flyby and Earth swingby in June and August 1999, respectively, and Jupiter flyby in December 2000 to January 2001 show that the instrument is performing well, has made important and heretofore unobtainable measurements in interplanetary space at Jupiter, and will likely obtain high-quality data throughout each orbit of the Cassini mission at Saturn. Sample data from each of the three sensors during the August 18 Earth swingby are shown, including the first ENA image of part of the ring current obtained by an instrument specifically designed for this purpose. Similarily, measurements in cis-Jovian space include the first detailed charge state determination of Iogenic ions and several ENA images of that planet’s magnetosphere.This revised version was published online in July 2005 with a corrected cover date. 相似文献