静电陀螺寻北仪的力学原理

静电陀螺仪是当今世界上精度最高的陀螺仪,研制静电陀螺寻北仪是为了寻求高精度的方位测量仪器。采用静电陀螺仪组成寻北仪可采用以下两种方式：力反馈方式和自由陀螺方式。前者水平方向包含两个力反馈回路,通过测量反馈回路电流得出方位角。后者陀螺自由转动数分钟,通过测量静电陀螺水平轴偏角得出方位角。该文讨论了力反馈方式和自由陀螺方式静电陀螺寻北仪力学原理,其中包括两种方式下坐标变换及获得方位角的算法推导,并得出结论。     

静电陀螺寻北仪中的磁干扰

电磁兼容性的问题尤其对采用静电陀螺作为核心元件的高精度寻北仪越来越显得重要。有关静电陀螺的文献对于静电干扰讨论较多,本文则侧重对静电陀螺寻北仪中的磁干扰进行讨论。磁干扰包括外部磁干扰和内部磁干扰,外部磁干扰可通过严格的电磁屏蔽加以排除,对于内部磁干扰本文推导了有关数学关系式,必要时可以加以补偿。     

超滤法分级和纯化蛋白质的现状和前景(英文)

超滤法具有高产率、低成本、容易放大等显著优点,但其低选择性一直限制其在生物蛋白制品的分级和纯化中的应用。本文总结和分析了超滤法用于蛋白质分级和纯化的近期研究成果,对其低选择性的原因进行了分析,提出并论证了提高超滤选择性的技术途径。     

A massive phytoplankton bloom induced by an ecosystem-scale iron fertilization experiment in the equatorial Pacific Ocean

The seeding of an expanse of surface waters in the equatorial Pacific Ocean with low concentrations of dissolved iron triggered a massive phytoplankton bloom which consumed large quantities of carbon dioxide and nitrate that these microscopic plants cannot fully utilize under natural conditions. These and other observations provide unequivocal support for the hypothesis that phytoplankton growth in this oceanic region is limited by iron bioavailability.     

变更图的边添加

证明了:对任何整数t≥6和d≥2,从一条长为d的简单路通过添加t条边后得到的图的最小直径上界为[d-2/t 1] 2,如果d∈J'(t,k)={2k(t 1) 1,2k(t 1) 2,2k(t 1)-t 1}∪{2k(t 1)-t h:h=6,7,…,t};其他情形为[d-2/t 1] 1.这个证明改进了已知结果,而且[d-2/t 1] 1是最好的上界.     

The fate of injectant coal in blast furnaces: The origin of extractable materials of high molecular mass in blast furnace carryover dusts

The aim of the work was to investigate the fate of injectant coal in blast furnaces and the origin of extractable materials in blast furnace carryover dusts. Two sets of samples including injectant coal and the corresponding carryover dusts from a full sized blast furnace and a pilot scale rig have been examined. The samples were extracted using 1-methyl-2-pyrrolidinone (NMP) solvent and the extracts studied by size exclusion chromatography (SEC). The blast furnace carryover dust extracts contained high molecular weight carbonaceous material, of apparent mass corresponding to 10⁷?10⁸ u, by polystyrene calibration. In contrast, the feed coke and char prepared in a wire mesh reactor under high temperature conditions did not give any extractable material. Meanwhile, controlled combustion experiments in a high-pressure wire mesh reactor suggest that the extent of combustion of injectant coal in the blast furnace tuyeres and raceways is limited by time of exposure and very low oxygen concentration. It is thus likely that the extractable, soot-like material in the blast furnace dust originated in tars is released by the injectant coal. Our results suggest that the unburned tars were thermally altered during the upward path within the furnace, giving rise to the formation of heavy molecular weight (soot-like) materials.     

多余的知识

12岁那年，父亲要教我学游泳。隔壁住着一位体育老师，我去串门的时候，发现一本小册子，似乎叫《水上自救法》，便借回家阅读。没翻两页，父亲下班回来了，看见这本书，一把就夺过去，锁进抽屉，说：“儿子，我们游泳去！”约三、四天时间，我就能够“狗刨”了。经过一个暑假，我已能在水上玩得欢。后来的一天，父亲就将《水上自救法》还给我。我满怀兴趣地看了一遍，当夜，就按书中列举的一些险情做了几个惊恐的梦。6年前，我们当地一名富商回故乡投资，想在风景秀丽的山脚下建一所疗养院。他找到当地一位名医，请教此举的可行性。名医经…     

Temperature variations on the Tibetan Plateau over the last two millennia

The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e.