Developmental modes of the Neoproterozoic-Lower Paleozoic marine hydrocarbon source rocks in China

Based on the researches on rock type, the mode of occurrence, diagnostic minerals and creatures, the sedimentary geochemistry and organic facies of Chinese marine source rocks from wells and outcrops, and on the research findings of developmental modes of foreign marine source rock, the authors consider that it is impossible to objectively make clear the formation mechanism of hydrocarbon source rock with high organic matter abundance by either single mode of preservation or high organic matter productivity. According to the Chinese geological features, the formation mechanism of the Neoproterozoic-Lower Paleozoic marine source rock is generalized into four modes, namely, thermal water activity-upwelling flow-anoxic; carbonate gentle slope-upwelling flow; xerothermic climate-brine euxinic milieu; and humid climate-retained euxinic milieu; as the Lower Cambrian undercompensation basin organic facies （the Tarim Basin, South China and southwestern margin of North China）, carbonate gentle lime mud bound organic facies （the Upper Ordovician in Tazhong region of the Tarim Basin and the Lower Silurian in the Upper Yangtze Platform）, the Middle Cambrian evaporation laggon organic facies （the Tarim Basin and the Upper Yangtze Platform）, enclosed undercompensation terrigenous bay organic facies （the Middle-Upper Ordovician in the west of the Tarim Basin, the Lower Silurian Long- maxi Formation in the Upper Yangtze platform）. Chinese marine sedimentations with lower organic matter abundance are generalized into two modes of consumption-dilution mode of open epicontinental sea and depletion-dilution mode of supercompensation basin.     

The controlling factors and distribution prediction of H2S formation in marine carbonate gas reservoir, China

Generally, there are some anhydrites in carbonate reservoir, as H2S is also familiar in carbonate oil and gas reservoirs. Nowadays, natural gas with high H2S concentration is usually considered as TSR origin, so there is close relationship between H2S and anhydrite. On the contrary, some carbonate rocks with anhydrite do not contain H2S. Recently, researches show that H2S is only a necessary condition of H2S formation. The reservoir porosity, sulfate ion content within formation water, reservoir temperature, oil/gas and water interface, hydrocarbon and some elements of reservoir rock have great controlling effects on the TSR occurrence. TSR deoxidizes hydrocarbon into the acidic gas such as H2S and CO2, and the H2S formation is controlled by TSR occurrence, so the relationship among reaction room, the contact chance of sulfate ion and hydrocarbon, the reservoir temperature has great influence on the TSR reaction. H2S has relatively active chemical quality, so it is still controlled by the content of heavy metal ion. Good conditions of TSR reaction and H2S preservation are the prerequisite of H2S distribu- tion prediction. This paper builds a predictive model based on the characteristic of natural gas reservoir with high H2S-bearing. In the porosity reservoir with anhydrite, the formation water is rich in sulfate and poor in heavy metal ion. Oil and gas fill and accumulate in the gas reservoir with good preservation conditions, and they suffered high temperature later, which indicates the profitable area of natural gas with high H2S-bearing.     

纳米CaCO3/丙烯酸树脂浆液的流变性

制备了纳米CaCO3/丙烯酸树脂浆液,当浆液(48 gZ-26、50g纳米CaCO3和83.3 g二甲苯)中分散剂添加量为3 g时,Casson屈服应力τc值最小,浆液的稳定性最好,与工艺条件优化时所得到的一致.纳米CaCO3/丙烯酸树脂浆液的流变性研究表明:该体系的流动特性符合Casson模型,其屈服应力τC较小,稳定性较好;浆液的黏度随剪切速率增加而显著下降,具有明显的剪切稀化特性,且随着纳米CaCO3含量增加,其剪切稀化趋势增强;在所考察的低剪切速率范围内,纳米CaCO3浆液具有明显的触变性,且纳米CaCO3含量越大触变性越大.图10,表7,参8.     

船舶自动化电站系统仿真

应用系统建模技术和计算机系统仿真技术，在研究了某大型船舶电力系统的基础上，运用MATLAB软件，结合船舶柴油机发电机组和异步电动机的特性，完成了船舶自动化电站系统的建模。实现的船舶自动化电站仿真器系统特性与实际系统特性接近。该系统对船舶轮机员技术培训和船舶电力系统的故障分析具有很高的价值。     

我国海水制盐业废渣处理利用现状

介绍了盐石膏的理化性质,综述了我国海盐工业废渣盐石膏在水泥、石膏建材等建筑领域以及对盐石膏的深加工等方面的综合利用研究现状,并指出利用盐石膏制备硫酸钙晶须具有广阔的发展前景。     

聚乙二醇对碳酸钙结晶的影响

在聚乙二醇（ＰＥＯ）存在下,ＣａＣｌ２和Ｎａ２ＣＯ３反应得多晶形碳酸钙沉淀,Ｘ－衍射显示主要为文石型结构,并随着ＰＥＯ／Ｃａ摩尔比的增大,晶体颗粒变小。结果表明,聚合物对碳酸钙晶核的形成和晶体的生长有很大影响。本文还对其形成机理进行了初步探讨。     

用强碱性阴离子交换树脂从碳酸盐溶液中回收铀的研究 2.U(Ⅵ)在溶液相与树脂相的化学状态

在过量碳酸盐存在的Ｕ（Ⅵ）溶液中,Ｕ（Ⅵ）的化学状态与溶液的ｐＨ值有关,当ｐＨ＞８时,Ｕ（Ⅵ）以［ＵＯ２（ＣＯ３）３］４－离子存在．吸附于树脂相的Ｕ（Ⅵ）的化学状态也与供吸附的料液的ｐＨ值有关,当ｐＨ＞９时,Ｕ（Ⅵ）才完全以［ＵＯ２（ＣＯ３）３］４－吸附于树脂相．当ｐＨ在６．５～８．０范围时,Ｕ（Ⅵ）在溶液中还可能以［ＵＯ２（ＣＯ３）２］２－或Ｈｎ［ＵＯ２（ＣＯ３）３］ｎ－４形式存在,而Ｕ（Ⅵ）以［ＵＯ２（ＣＯ３）２］２－形式吸附于树脂相的可能性很小,它主要以Ｕ２Ｏ２－７的形式吸附于树脂相．     

BF3催化碳酸二甲酯合成N-环己基氨基甲酸甲酯

对碳酸二甲酯与环己胺化合生成N-环己基氨基甲酸甲酯的反应进行了研究.考察了催化剂BF3的催化活性和相关反应条件.控制反应的较佳参数为：催化剂用量为n（环己胺）：n（BF3）=20：1;反应回流时间为20 h;反应温度控制在70℃;反应物配比n（DMC）：n（环己胺）=1.5：1.最高产率为49.05%,且反应后处理简单,对环境污染少.产品纯度高,达99.94%.     

柴达木盆地西部第三系碳酸盐岩层的古生物特征

柴达木盆地西部第三系的碳酸盐岩层中发现有藻类、介形虫、有孔虫、腹足类、多毛类等化石.除藻类外各种生物的数量都比较少.生物具有个体小,壳体构造简单,多样性低等特点.所有生物都属于广盐性生物.根据该区古生物特征分析和与其它地区的对比,认为当时该区生物生长于内陆半咸化湖至咸化湖环境,而不是海相或海陆过渡相环境.参11.     

海洋木栖真菌抗肿瘤活性及其营养条件的影响

对从厦门海沧及漳州浮宫的红树林生态区分离到的177株海洋木栖真菌用MTT法进行抗肿瘤活性的测定，获得具有抗肿瘤活性的菌株共44株，占总受试菌株的24．9％，其中对KB瘸株有抑制作用的有12株．对Raji瘤株有抑制作用的菌株有43株，对这两种肿瘤细胞均有抑制作用的菌株有11株．并且考察了其中6株海洋木栖真菌在纤维素、羧甲基纤维素钠、淀粉和蔗糖为碳源的生物量和抗肿瘤活性。结果表明海洋木栖真菌在不同营养条件下的菌体生物量及代谢产物的抗肿瘤活性均存在差异，部分菌株在纤维素为碳源时，有最高的生物量和抗肿瘤活性，PDB培养基不宜作为抗肿瘤活性测定或生产发酵的基质．