一种高分子电阻型湿度传感器的制备及研究

以苯乙烯-马来酸酐共聚物钠盐(Na-SMA)为湿敏材料,采用浸涂的方法,在小型叉指金电极上成膜,制备了高分子电阻型湿度传感器.研究了浸涂液组成对传感器响应特性的影响.研究表明,随着浸涂液中Na-SMA浓度的提高,元件的电阻、湿滞降低;而随着浸涂液中聚乙烯醇(PVA)浓度的提高,元件的电阻降低,湿滞增加.     

LF钢水成分与温度控制模型

以钢水、渣、包衬为研究体系,建立了钢水成分与温度控制模型。温度控制精度在±3℃以内,在补加系数法的基础上考虑了合金的收得率,推导出合金添加计算公式,使计算精度进一步提高。     

煤灰熔融温度多项式模型的偏回归函数分析

为了考察煤灰中的化学组分对熔融特性温度的贡献，借助我国69种重要的商业用煤的灰熔融特性温度和灰中SiO2和Al2O3等6种主要化学组分的测试数据，利用多项式模型的偏回归函数分析方法，对煤灰的熔融特性温度进行一至四阶多项式模型回归分析，获得了各化学组分的偏回归函数。研究结果表明：各化学组分的偏回归函数能够表现熔融温度对应于该组分变化的趋势；同一组分偏回归函数不同，该组分对变形温度、软化温度和熔融温度的影响存在较大的差异；CaO和TiO2的偏回归函数反映熔融温度变化趋势的可信度最高。实验为进一步研究煤灰熔融特性温度的数学模型和参数选择提供参考。     

摔跤训练器主体与模拟人连接机构的分析与改进

阐述了摔跤训练器的基本机构,利用齐次坐标变换建立了摔跤训练器主体机构与模拟人连结部分的运动关系;根据理论推导的结果,分析了此机构的特点,提出了改进方案。该方案克服了训练器在滚桥动作中的一些不足之处。     

论互动式写作教学模式的构建

“人”“”合一的写作教学新理念，预示着以人为本、注重学生写作主体性、开放性、体验性、生成性和创造性的现代写作教学新思维的唤醒及其价值回归。写作教学新理念和现代教学理论是构建互动式写作教学模式的指导思想和理论基础，互动式写作教学模式有其独特的特征及对教师角色地位要求，开放型、交流型、激励型、评价型的写作教学成为互动模式结构的主要成分，其实施目的和要求应体现在更深层次的人取向上。     

关于Wolliam Kruskal猜想

对Wolliam Kruskal猜想进行了研究，得到了一些结果。     

井冈山自然保护区甜槠群落物种多样性分析

以甜槠群落6个样地调查资料为基础,对该群落的区系组成和不同样地、不同层次的物种多样性进行了分析,结果表明:(1)甜槠群落中有维管植物59科85属116种(含变种);属的地理成分以热带成分占优势,温带成分占有一定的比例。(2)乔木层、灌木层和草本层的各项物种多样性指标在群落各样地间均有一定的差异;在群落垂直结构中,灌木层的多样性指数最大,乔木层次之,草本层最小。     

C－isotope composition and significance of the Sinian on the Tarim plate

102 samples of limestones,mudrocks shales and tillites from the Sinian in Kuluketage have been analyzed ,Four formations in the Sinian belong to glacial deposits in which the differences in δ^13C are distinct (-14.7‰- 4.2‰),Distinctly negative δ^13C excursions for three times support the viwe of three glacial deposits in this area suggested by previous authors,except for the durations of them ,δ^13C values are generally positive in the Beiyixi Formation of lower part of the Lower Sinian ,representing probably the rock records of a continental rift related to break-up of the Rodinian supercontinent,There are three times of distinct excursions of δ^13C curve in all strata,The first one is from positive values at the bottom to about -5‰ at the top of the Beiyixi Formation ,The second one,from 0‰-3‰ in the Arletonggou Formation of upper part of the Lower Sinian to -3.4‰---14.4‰ in the Teruiaiken Formation.The third one,from positive values in the Zhamoketi Formation of lower part of the Upper Sinian to negative values in glacial varves at the top of the Hankeerqiaoke Formation.     

Inorganic chemical composition and source signature of PM2.5 in Beijing during ACE-Asia period

Aerosol samples for PM2.5 were collected in Beijing for 38 consecutive days from March to April 2001 using an IMPROVE Sampler. Concentrations of 20 elements in PM2.5 were determined using a PIXE method. Results show that the average mineral dust concentration of PM2.5 was 14.6 Ilg/m3 during the observation period. On the sand-dust event days of March 21 and April 10, dust PM2.5 mass concentrations were 62.4 and 54.1 μg/m^3, respectively.These demonstrate that fine particle pollution by dust event in Beijing was very severe. The enrichment factors of S and Cu reached minimums on the dusty days and were high on the non-dusty days. It is considered that enrichment factors of elements in PM2.5, which are associated with human activities, can probably provide an effective method to distinguish local sources from external sources of dust. Factor analysis on the chemical composition in PM2.5 shows that sources of crustal matters, anthropogenic emission, and oil combustion contributed to PM2.5 levels in air in the springtime of 2001 in Beijing.     

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.