Recent development of organic electron transport materials

This article reviews the recent development of organic electron transport materials applied in the fields of organic photoconductors, light-emitting diodes, field-effect transistors and solar cells. Several technologies for charge carrier mobility measurement are summarized and compared, and a series of basic principles for designing high-performance organic electron transport materials are suggested as well.     

Initial organic geochemical investigation on Late Neoproterozoic-Early Cambrian sediments in the Yangtze region, China

Totally 19 samples of typical Upper Proterozoic-Lower Cambrian sedimentary rocks were collected and analyzed for an organic geochemical investigation. Almost all these rocks have high TOCs, super-maturities and similar biomarker distribution. As an exception, however, the Sinian Nantuo Tillite shows much lower TOCs and little phytane and pristane in comparison with those in other strata, which implies a very faint photosynthetic process, and a restricted euphotic zone and quite limited sunlight within the sedimentary water column during the Sinian glaciation age in the western Yangtze region providing an evidence for palaeo-oceanic environment of the Neoproterozoic Snowball Earth age.     

Isotopic evolution of the terminal Neoproterozoic and early Cambrian carbon cycle on the northern Yangtze Platform, South China

Profound geotectonic, climatic and biological changes occur during the terminal Neoproterozoic and its transition into the early Cambrian. These are reflected in temporal variations of the chemical and isotopic composition of seawater. We are studying a sequence of sedimentary rocks at the Shatan section, northern Yangtze Platform, Sichuan Province of China. This succession comprises, in ascending stratigraphic order, predominantly calcareous sediments of the Sinian upper Dengying Formation and black shales of the lower Cambrian Guojiaba Formation (time equivalent of Niutitang Fm.). Paleoenvironmental setting represents shallow-water shelf deposits. The objective of our study is to provide temporal records for the isotopic compositions of organic and carbonate carbon throughout this time interval. Organic carbon isotope values display a range between -35.8‰ and -30.1‰ with clear stratigraphic variations. Carbonate carbon isotope data vary between -3.5‰ and +0.5‰. These secular variations are interpreted to reflect perturbations of the global carbon cycle, specifically changes in the fractional burial of organic carbon. However, local conditions have further affected the isotopic signals.     

含PPV结构的电致发光材料

评述了含PPV(聚苯乙炔)结构的高分子型电致发光材料近几年来的研究进展工作,并对这类材料的分子设计做了简要展望.介绍和引用了有代表性的文献31篇.     

二维磁性纳米结构材料的Monte Carlo模拟

运用Monte Carlo模拟方法，通过分折系统自旋序参数与温度的变化关系了解纳米结构材料磁性的特征．计算模拟结果表明，磁性纳米材料具有比同等大小和平均密度的单晶低的居里温度，且在相变过程中往往会出现一些亚稳态．研究结果提供了一种解析金属纳米结构材料特性的重要方法．     

H2在金属钾修饰碳纳米管上的吸附与储存

利用高压容积法、辅以卸压升温脱附排水法,测定金属钾修饰多壁碳纳米管(K~0-MWCNTs)对H_2的吸附储存容量。结果表明,在室温(～25℃)、～7.25MPa实验条件下其对氢的吸附储存容量可达3.80％(质量百分数);室温下卸至常压的脱附氢量为3.36％(占总吸附氢量的～89％),后续升温(升至673K)的脱附氢量为0.41％(占总吸附氢量的～11％)。     

纳米结构V2O5薄膜的溶胶凝胶制备与特性研究

采用溶胶 -凝胶技术 ,以V2 O5粉末为原材料制备了纳米结构的V2 O5薄膜 .使用椭偏仪、X射线衍射仪(XRD)、红外分光光度计 (FTIR)、电化学分析、原子力显微镜 (AFM)等方法研究了V2 O5薄膜的特性 .实验结果表明 :薄膜具有纳米多孔结构 ;热处理使得薄膜致密 ,折射率提高 ,薄膜结晶 .红外吸收测量揭示了刚制备的薄膜中钒以 4价离子为主 ,高温热处理后形成 5价钒离子 ,相应出现了V2 O5特征吸收峰 .这种结构的薄膜具有很好的锂离子注入 /退出可逆性和很高的离子注入容量 ,可用作锂离子电池的高性能阴极材料 .     

透水基层材料渗透系数测试

通过查阅国内外资料和进行大量室内试验 ,确定了级配 型沥青碎石和级配 型水泥碎石两种透水基层材料的配合比。并通过自制的沥青处治碎石渗透系数测试仪和水泥处治碎石渗透系数测试仪 ,分别测定了上述两种透水基层材料的渗透系数。     

淤泥类软土的应变特征与沉降计算

根据淤泥类软土的压缩模量随深度变化的事实，在理论和实例两方面，探讨分析了现行沉降分层总和法修正系数偏高的原因。     

纳米双相钕铁硼永磁合金的织构及磁畴

为开发纳米复合永磁材料高磁能积的潜力,用熔体快淬法制备各向异性的纳米双相快淬带。X光衍射结果表明,Nd9Fe85-xNbxB6(x=0,0.5,1.0)快淬带中存在垂直于带面的Nd2Fe14B[00L]织构,其自由面上的织构强于贴辊面。x=1.0时,在15m.s-1的快淬速度下的择优取向度为94%。磁力显微镜观察表明晶粒间存在强烈的交换耦合作用。x=0.5时的快淬带具有较强交换耦合作用及高织构度,因此具有最佳磁性能。其剩余磁极化强度为1.130T,内禀矫顽力为519.8kA.m-1,最大磁能积为121.2kJ.m-3。