Analysis of EET on Ca increasing the melting point of Mg17Al12 phase

The present investigation showed that the additions of Ca to the alloy AZ91 were mainly dissolved into the Mg17Al12 phase and increased its melting point and thermal stability, which would have great effects on the high- temperature properties of AZ91 alloy. The empirical electron theory (EET) of solid and molecules was used to calculate the valence electron structures (VES) of Mg17Al12 intermetallic compound with and without Ca addition. The results showed that Ca dissolving in Mg17Al12 phase increased the strength of bonds that control the thermal stability of Mg17Al12 phase. Additions of Ca also made the distribution of the valence electrons on the dominant bond network more uniform in the whole unit cell of Mg17Al12. The theoretical conclusions well account for the experimental results.     

纳米Co/Cu合金的磁性与退火热处理

系统研究了快淬Cox/Cu100-x(5≤X≤30)合金的磁性以及退火处理对磁性的影响。随退火温度的上升，Co颗粒在长大。当Co含量增加时，饱和磁化强度Ms和箸顽力Hc增大。Co含量少的样品，退火处理对磁化曲线影响大，Co含量多的样品与之相反。随退火温度TA升高，矫顽力Hc和剩余磁化强度Mr增大。在特征冻结温度（300K）下观察到一个大热滞效应。这个热滞温度远大于在ZFC曲线的峰值温度，这表明磁性颗粒的尺寸及形状有一较宽的分布。     

2,3,16,17-四羧基酞菁钴对氧还原的电催化作用

用循环伏安法及旋转圆盘-环电极研究了2,3,16,17-四羧基酞菁钴(CoTCPc)在溶液中及CoTCPc/GC修饰电极上对O_2还原的电催化作用。实验结果表明,CoTCPc对O_2电还原有明显的催化作用。在Co(Ⅱ)TCPc还原为Co(Ⅰ)TCPc的第一个峰电势附近,O_2在CoTCPc/GC修饰电极上定量地还原为H_2O_2,在稍负的第二个峰电势附近,有H_2O_2还原产生H_2O的过程发生。本文并对CoTCPc对O_2还原电催化过程的机理进行了讨论。     

Elemental composition of aerosols collected in the glacier area on Nyainqêntanglha Range, Tibetan Plateau, during summer monsoon season

In order to investigate the elemental composition in atmospheric aerosols and its sources in the glacier area over the Tibetan Plateau (TP), seven totally suspended particle samples were collected continuously at the col of the Zhadang glacier (30°28′N,90°39′E,5800 m a.s.l.), Nyainqêntanglha Range, southern TP, from June to October 2006. Twenty-seven elements (Li, Be, B, Na, Mg, Al, K, Ca, Sc, Ti, V, Fe, Mn, Zn, Ga, As, Rb, Sr, Y, Cd, Cs, Ba, Tl, Pb, Bi, Th, U) were analyzed by Inductively Coupled Plasma Mass Spectrometry (ICP-MS). The result indicates that the concentrations of most elements (especially crustal elements) are lower than values at the Nam Co Station during the same period of 2005, and also much lower than other sites in the TP such as Wudaoliang and Waliguan. This suggests that elemental compositions of aerosols in the Zhadang glacier area may represent the background levels of the middle/upper troposphere over the TP. Crustal enrichment factors (EFs) reveal that several elements (e.g. B, Zn, As, Cd, Pb and Bi) may have anthropogenic sources. The southern TP is mainly influenced by the summer Indian monsoon during the sampling period. Backward air mass trajectory analysis suggests that air masses in the region may originate from South Asia. Therefore, anthropogenic pollutants from South Asia may be transported by the summer Indian monsoon to the region which clearly affects the atmospheric environment in the southern TP during the summer monsoon season.     

融盐包裹法合成球形正极材料LiNi_(0.7)Co_(0.2)Al_(0.1)O_2(英文)

以球形Ni(OH)2为核心原料,Al(NO3)3.9H2O、Co(NO3)2.6H2O和LiNO3为包裹原料,采用融盐包裹法在空气中煅烧合成了单相固溶体LiNi0.7Co0.2Al0.1O2。用XRD研究了合成产物的物相和结构,用SEM研究了合成产物的形貌,用电池性能测试仪研究了合成产物的电化学性能。实验结果表明,合成产物具有α-NaFeO2型层状有序结构、球状形貌和良好的电化学性能。     

以十七大精神为指导 努力构建和谐西藏

党的十七大报告对构建社会主义和谐社会作出了新的阐述,我们应当深刻领会十七大关于构建和谐社会的新精神,深刻认识构建社会主义和谐西藏的重大意义,并按照十七大精神的要求,在经济发展的基础上,大力加强社会建设,努力改善民生,以促进西藏社会的和谐和不断进步。     

Co@CNTs的制备及性能表征

采用球磨处理增加碳纳米管的结构缺陷,提高其反应活性,并以简单水热法合成了Co@CNTs复合物.用XRD、SEM、TEM对其结构和形貌进行了表征.结果显示,球磨处理后CNTs长度变短,复合物中CNTs与Co分布均匀,Co为纳米颗粒且有部分生长在CNTs表面.电化学性能测试结果表明,Co@CNTs电极比Co电极具有更高的放电容量、更好的循环稳定性及抗腐蚀性能.     

一种黑曲霉斜面培养基的优化方法

通过一系列实验,优化了黑曲霉Co827的斜面培养基配比.优化后的斜面培养基为3.5°Be～ 3.6°Be麦芽汁培养基.采用优化后的培养基,单菌落孢子数达到167.2×105左右,产孢子能力提高了15.07％,通过摇瓶验证,产酸达到14.40％,提高了3％左右.     

Environmental changes reflected by n-alkanes of lake core in Nam Co on the Tibetan Plateau since 8.4 kaB.P.

The n-alkanes are extracted from NMLC-1 core that was drilled in the Nam Co, central Tibet. They are measured by using Gas Chromatography and Mass Spectrometry (GC/MS) for componential and quantitative analyses. According to the constructed depth-age model, the component and concentration of n-alkanes, together with total organic carbon (TOC), total nitrogen (TN) and carbonate are used to elu- cidate palaeoenvironmental changes of Nam Co during the past 8.4 ka. The results indicate that Holo- cene environment performs three stages in the lake area. In the stage of 8.4―6.7 kaB.P., it was warmer while precipitation slightly increased. This stage was ended by an obvious cold/dry event. During 6.7― 5.8 kaB.P., temperature increased rapidly and reached its maximum values at about 6.0 kaB.P. The environments were warm/wet optimum for the blooming of terrestrial plants and submerged aquatic plants. After that, temperature decreased continuously and showed the lowest values at about 3.0 kaB.P. From 2.9 kaB.P. to the present, temperature rose again but alternated with cold and warm. The lake area tended to be dry after 1.4 kaB.P. During 600―400 aB.P., the environmental feature was the reflection of "Little Ice Age".