Oxidative Treatment of Some Reactive Dyes by Fenton Reagent

Nine kinds of reactive dye solutions: Reactive K-2RL, H-E2R, X-6B1Y, HE-4G, X-3B, K-2R,H-E7B, X-4RN and S-F3B were treated by usingFenton reagent. While the concentration of dye is 400mg/L, the FeSO_4 dosage 100-180 mg/L, H_2O_2 240～540 mg/L, that is the stoichiometric numbers of Fe~(2+)and H_2O_2. are between 1: 9～1: 12, pH=3, reaction     

西部人力资源开发问题研究

人力资源开发是西部大开发的客观要求 ,是促进西部地区产业结构调整的关键环节 ,是解决西部地区诸多社会问题的重要途径。只有以观念更新为前提 ,以优化环境为基础 ,以教育优先为关键 ,以政府作用为保障 ,才能有效地解决西部地区人力资源开发方面存在的诸多问题 ,保证西部大开发战略的顺利实施。     

从果子狸谈起——从SARS的流行省思人与自然的关系

果子狸是SARS病毒的宿主之一 ,野生动物是人类SARS的毒源。人工驯养野生动物 ,让人造的化学成分进入了大自然本来的生物过程 ,其产生的危害给世人带来了生态性的灾难。人类要善待自然 ,慎用科技 ,让人的自然体在大自然中正常生息才能达致人与自然的和谐。     

《广西民族学院学报(哲社版)》引文分析

运用文献计量学方法 ,对 1 995～ 2 0 0 2年度《广西民族学院学报 (哲社版 )》全部论文的引文量、引文类型、引文语种、引文年代等进行统计分析 ,揭示该刊论文著者利用科技文献的规律。     

在硅基材料上用Sol-gel法制备涂层测定氧扩散系数研究

提出一种测定氧扩散系数新方法。用Sol-gel法制备了Y2O3/SiO2均匀致密的薄膜,能成功解决其它方法无法得到的冶炼所得到的熔体,光学椭偏测定氧化层的膜厚。探讨了氧在薄膜中的扩散,在Wagner理论基础上,用数学方法表达在掺杂SiO2薄膜氧扩散系数与氧化层膜厚的关系。     

硫酸浓度对纳米级SO4^2-／TiO2固体超强酸的影响

用锐钛型纳米TiO2制备了纳米级SO4^2-／TiO2固体超强酸，分析了硫酸浓度不同时其比表面积、失重率、红外光谱及催化活性的不同。当硫酸浓度为1．0mol／L时，它在450～900℃的失重率为3．3％，比表面积为105．2m^2／g，对乙酸和丁醇酯化反应的酯化率达到98．4％。玻璃球负载纳米级SO4^2-／TiO2固体超强酸的重复使用性能好，在乙酸和丁醇的酯化反应中重复使用9次后的酯化率才由初次的99．3％变为84．9％。     

在硅基材料上用Sol-gel法制备涂层测定氧扩散系数研究

提出一种测定氧扩散系数新方法.用Sol-gel法制备了Y2O3/SiO2均匀致密的薄膜,能成功解决其它方法无法得到的冶炼所得到的熔体,光学椭偏测定氧化层的膜厚.探讨了氧在薄膜中的扩散,在Wagner理论基础上,用数学方法表达在掺杂SiO2薄膜氧扩散系数与氧化层膜厚的关系.     

Paleotemperature changes ver the past 3000 years in eastern Beijing, China:A reconstraction based on Mg/Sr records in a stalagmite

The Mg/Sr ratio in a stalagmite, which is directly proportional to DMg/Ca, the solid-liquid distribution coefficient of Mg, is proposed as a geochemical thermometer to estimate paleotemperature changes. The paleotemperature changein eastern Beijing over the past 3000 years has been reconstructed by using this thermometer in the stalagmite ZFFS-1 from Jingdong Cave. The records can be divided into two periods: 3000-2000 aBP, cool and wet, the air temperature averaging 9.8℃; and 2000 aBP-present, hot and dry, the air temperature being 1℃ higher than the mean value (11.7℃) of the past 3000 years. During 500-200 aBP, the air temperature was about 1.2℃ lower than that of the present, corresponding to the Little Ice Age in Europe. Like δ18O and δ13C, Mg/Sr (or DMg/Ca) reflects an obviously warming trend of the past 200 years. These results are supported by historic records.     

Impact of the closure of Indonesian seaway on climate: A numerical modeling study

Using a global OGCM and its relevant coupled ocean-atmosphere GCM with the contemporary, 6 MaBP and 14 MaBP oceanic topography, respectively, a series of numerical experiments are implemented in order to investigate the effect of the north shift of Australian continent on the tropical oceanic circulation, especially the formation of the western Pacific warm pool. The numerical experiments of the individual OGCM forced by the modern atmospheric circulation indicate that the closure of Indonesian passage results in warming in the tropical Pacific Ocean and cooling in the tropical Indian Ocean; furthermore, it also results in change in source of the Indonesian Through Flow (ITF) water, e.g. ITF mainly originates from the south Pacific at 14 MaBP, but it mainly originates from the north Pacific now. The coupled model shows similar results as the individual OGCM qualitatively.     

以[NEt4]3[Fe(CN)6]和[Mn(Ⅲ)(SB)S1S2]ClO4为单元的分子磁体的合成和表征

以[NEt4]3[Fe(CN)6]和[Mn(Ⅲ)(SB)S1S2]ClO4(SB,席夫碱＝5-CH3salophen (双水杨醛缩邻苯二胺)和5-CH3salen (双水杨醛缩乙二胺),S1和S2为H2O或CH3OH)为单元,室温下组装得到了新的化合物,并进行了相应的表征.结合元素分析、红外光谱分析、紫外-可见光谱分析和热分析结果,可以看出,席夫碱配体的空间位阻不同,化合物的结构也有很大变化.