Authigenic sulfide minerals and their sulfur isotopes in sediments of the northern continental slope of the South China Sea and their implications for methane flux and gas hydrate formation

This is a report of the study of the authigenic sulfide minerals and their sulfur isotopes in a sediment core (NH-1) collected on the northern continental slope of the South China Sea, where other geo-physical and geochemical evidence seems to suggest gas hydrate formation in the sediments. The study has led to the findings: (1) the pyrite content in sediments was relatively high and its grain size relatively large compared with that in normal pelagic or hemipelagic sediments; (2) the shallowest depth of the acid volatile sulfide (AVS) content maximum was at 437.5 cm (>2 μmol/g), which was deeper than that of the authigenic pyrite content maximum (at 141.5-380.5 cm); (3) δ 34S of authigenic pyrite was positive (maximum: 15‰) at depth interval of 250-380 cm; (4) the positive δ 34S coincided with pyrite enrichment. Compared with the results obtained from the Black Sea sediments by Jorgen-sen and coworkers, these observations indicated that at the NH-1 site, the depth of the sulfate-methane interface (SMI) would be or once was at about 437.5-547.5 cm and the relatively shallow SMI depth suggested high upward methane fluxes. This was in good agreement with the results obtained from pore water sulfate gradients and core head-space methane concentrations in sediment cores collected in the area. All available evidence suggested that methane gas hydrate formation may exist or may have existed in the underlying sediments.     

铜镍硫化物矿床特征与成矿机制综述

综述了近几年来的研究成果,介绍与铜镍硫化物矿床有关的镁铁质-超镁铁质岩体特征、部分地球化学参数,总结岩浆重力分异、同化混染、热液成矿作用等成矿理论。     

柴油深度加氢脱硫过程中硫化物转化规律的研究

采用气相色谱-脉冲火焰光度计检测器(GC-PFPD)对催化柴油中的硫化物及其形态分布进行了分析,发现催化柴油中硫化物的类型主要为苯并噻吩类(BTs)和二苯并噻吩类(DBTs)。研究表明,苯并噻吩类硫化物比较容易被脱除,而当催化柴油中总硫含量在500×10-6时其主要硫化物形态为二苯并噻吩类;不同烷基取代的DBTs的加氢脱硫(HDS)转化率不同,其被加氢脱除由易到难顺序为:C1DBT→C2DBT→C3DBT;而单个硫化物被加氢脱除由易到难顺序为:DBT→4-MDBT→2,4,6-TMDBT→4,6-DMDBT。实验发现,加氢柴油中的硫化氢可以被氧化成元素硫,从而影响总硫分析结果。采用GC-PFPD可以有效地对最低硫含量在(5~20)×10-6的超低硫柴油中硫化物以及元素硫进行分析鉴定,为加氢催化剂和加氢工艺的筛选提供必要的依据。     

亚硝酸盐氮对硫化物测定的干扰及消除

对氨基二甲基苯胺光度法和碘量法测定硫化物过程中,高浓度的亚硝酸盐氮(NO2--N)会对分析测定产生明显干扰,在CNO2--N=150mg/L左右、S2-加标量为100mg/L时,两种测定方法的加标回收率分别为68.27%和58.21%。实验证明,在用碘量法测定硫化物时,若将无CO2水重复冲洗滤纸3次,其加标回收率可达103.84%。     

S-烷基异硫脲盐作为硫醇替代物经环氧开环反应合成β-羟基硫化物

S-烷基异硫脲盐作为一种无毒、无味、易于制备的硫醇替代物，在碱性水介质中、室温下与多种环氧化合物发生环氧开环反应，区域选择性、高收率地合成了一系列β-羟基硫化物。     

褪色光度法测定微量硫化物的研究

根据Ｓ＾２－对４－（对磺酸基苯基）－卟啉（ＴＳＰＰ）与铅显色反应的褪色干扰作用，建立了一种测定Ｓ＾２－的新方法，该方法对Ｓ＾２－的检出限为１０μｇ／Ｌ，选择性较好，用于含硫废水中痕量Ｓ＾２－的测定，结果令人满意。     

硫含量对中碳非调质钢中硫化物及组织的影响

利用真空感应炉冶炼了不同硫含量的中碳非调质钢,研究了S含量对非调质钢中硫化物形态分布及显微组织的影响.结果表明：在0.025%~0.065%范围内,随S质量分数的增加,非调质钢中硫化物的数量增多,偏聚分布现象加重;晶内铁素体比例随之升高,组织得到细化.通过热力学计算及相图信息研究了硫化物的类型转变. S含量增加时第Ⅲ类MnS在凝固末期以离异共晶形式较早析出,剩余液相中的S在凝固结束时以共晶形式析出为第Ⅱ类MnS.单独MnS以及MnS- V( C, N)复合硫化物均可作为晶内铁素体的有效形核核心,促进铁素体的生成.     

Ⅱ-Ⅵ族化合物半导体超微粒子光谱性质的研究:Ⅰ硫化物

本文报道了锌、镉、汞、铅硫化物半导体极超微粒子的制备以及它们的光谱性质,比较了它们的粗、细粒子的吸收光谱和荧光光谱的差异,用量子化粒径效应解释了当超微粒子的粒径减小时出现的能级分裂.同时讨论了上述物质的极超微粒子在老化过程中的行为及其原因.     

一类新的红色荧光粉MY2S4:Er3+(M=Sr2+,Ba2+)的合成与表征

Eu2 激活的CaS: Eu[1],Eu3 激活的硫氧化物[2],Pr3 激活的Ca0.8Zn0.2TiO3[3]以及Eu2 和Mn2 掺杂的SrY2S4[4]都是重要的红色发光材料.