Regulation of cellulose synthesis in Acetobacter xylinum by cyclic diguanylic acid

Cellulose is the most abundant renewable carbon resource on earth and is an indispensable raw material for the wood, paper, and textile industries. A model system to study the mechanism of cellulose biogenesis is the bacterium Acetobacter xylinum which produces pure cellulose as an extracellular product. It was from this organism that in vitro preparations which possessed high levels of cellulose synthase activity were first obtained in both membranous and soluble forms. We recently demonstrated that this activity is subject to a complex multi-component regulatory system, in which the synthase is directly affected by an unusual cyclic nucleotide activator enzymatically formed from GTP, and indirectly by a Ca (2+) -sensitive phosphodiesterase which degrades the activator. The cellulose synthase activator (CSA) has now been identified as bis-(3' 5')-cyclic diguanylic acid (5'G3'p5'G3'p) on the basis of mass spectroscopic data, nuclear magnetic resonance analysis and comparison with chemically synthesized material. We also report here on intermediary steps in the synthesis and degradation of this novel circular dinucleotide, which have been integrated into a model for the regulation of cellulose synthesis.     

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.