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。     

洞庭湖湿地小型节肢土壤动物群落组成及其特征

从2003年11月到2004年10月对洞庭湖湿地平原、丘岗、低山的4种生态系统中的小型节肢土壤动物群落的组成、多样性、相似性进行了比较研究。全年调查共获得小型节肢土壤动物27641个,隶属节肢动物门的6纲、24目。4个土壤动物群落中动物类群数和个体数均以针阔混交林>茶林>竹林>阔叶林;多样性指数(H')由大到小依次是针阔混交林>茶林>阔叶林>竹林,与群落均匀度的变化显著相关,而与群落的丰富度关系不密切;Jaccard系数、Gower系数和Pianka的α指数的分析结果表明,4种群落中共有的类群数极为相似,但群落中各类群的最大个体数和最小个体数的差值相差很大。     

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。     

聚氨酯泡沫复合夹层板抗爆特性分析

聚氨酯泡沫复合夹层板是一种可广泛应用于防护工程中的新结构形式 ,据此对聚氨酯泡沫材料夹层板进行了爆炸荷载下有限元分析 ,并与粘钢混凝土板及混凝土板两种板结构进行了比较 ,验证了聚氨酯泡沫夹层板良好的抗爆吸能性能     

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.     

Composition operators between p-Bloch space and q-Bloch space in the unit ball

Let B_n be the unit ball of C~n and φ= (φ_1,…,φ_n) a holomorphic self-map of B_n. The main purpose of this paper is todiscuss the boundedness and compactness of composition operator C_φ between p-Bloch space β~p(B_n) and q-Bloch space β~p(B_n), where p≥0 and q≥0.     

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.