正实数阶广义M集的外部结构

推广了Philip所提出的“区域分解”和“角度分解”方法,提出了等势线和色彩调配法,并利用这四种方法构造了一系列正实数阶广义M集的外部结构图·研究了广义M集外部结构的分形特征及演化过程,结果表明整数阶广义M集的外部区域具有分形特征,小数阶广义M集的外部区域出现了错动和断裂,且其演化过程依赖于相角主值范围的选取     

开关广义Mandelbrot集

基于开关复映射,阐述了开关广义Mandelbrot集(简称广义M集)的构造方法,并构造出一系列开关广义Mandelbrot集·在对开关映射作用下复C平面上初始点轨道的分析及开关广义M集构造算法研究的基础上,通过计算机实验,得出以下结论:①开关广义M集具有分形结构;②开关广义M集包含了构成开关映射的两个映射的部分稳定区;③开关广义M集的演化过程依赖于相角主值范围的选取     

平面蒸发薄液膜的稳定性分析

固体表面上形成的蒸发薄液膜，对微细空间内的传热有重要强化作用。论文对平面蒸发薄液膜的传热传质过程建立了物理模型，从汽－液界面上的边界条件得到无量纲液膜厚度随时间变化的发展方程。还探讨了液膜的稳定性特性。这种稳定性特性对热边界条件不敏感，但对工质扩散常数、界面温度梯度（Marangoni效应）的依赖较大。     

汾河下游三万年来沉积环境演化

根据汾河下游岩性特征、沉积物粒度、粘土矿物和孢粉分析，探讨了汾河下游3万年来环境演化规律。30－11Ka.B.P为晚更新世末次冰期盛冰期，气修干寒；11Ka以来，经历了3个气候旋回，变化周期为3.5Ka左右，黄河中游早期文明起源及人类生产活动，与本区气候关系有很好的耦合性。     

高增益MILO中辐射场的Landau-Ginzburg方程

推导出了描述MILO中非线性辐射场演化的积分方程,并表明在高增益情况下,这个方程可简化为Landau-Ginzburg方程.这提供了一个描述MILO中场演化的最简单动力学模型.     

论刘勰诗本体论诗体的规范与进化观

既强调诗体的规范又强调诗体的进化的诗的进化论，是刘勰诗本体论的重要组成部分，刘勰在诗歌的形式本体上的思想是既保守又激进的，他很重视文体，语言，体验和想象，刘勰诗的形式本体论的主要学说是“诗有恒裁”说：强调诗歌有体，诗人应该有自觉的文体意识，甚至认为四言为正体；又不反对诗体进化，主张“随性适分”、“质文代变”。     

Identification of protein superfamily from structurebased sequence motif

The structure-based sequence motif of the distant proteins in evolution, protein tyrosine phosphatases (PTP) Ⅰ and Ⅱ superfamilies, as an example, has been defined by the structural comparison, structure-based sequence alignment and analyses on substitution patterns of residues in common sequence conserved regions. And the phosphatases Ⅰ and Ⅱ can be correctly identified together by the structure-based PTP sequence motif from SWISS-PROT and TrEBML databases. The results show that the correct rates of identification are over 98%. This is the first time to identify PTP Ⅰ and Ⅱ together by this motif.     

Change of water use efficiency and its relation with root system growth in wheat evolution

Raising crop water use efficiency (WUE) is the physiological basis to implement crop high efficiently using water. The present soil column and field experiments are designed to investigate the change of wheat WUE (Triticum aestivum L.) at whole plant level and root system growth in evolution and the relationship between WUE and its root system growth using 10 wheat evolution genotypes with different ploidy chromosomes sets. Results show that in wheat evolution from 2n→6n, WUE at whole plant level increases with the increase of ploidy chromosomes, and root system growth (root weight, root length) and root/shoot ratio of wheat decrease with the increase of ploidy chromosomes under dry and irrigated conditions. WUE is negatively correlated with root weight and root/shoot ratio of wheat in evolution, significantly. Root system growth has an adverse redundancy for WUE in wheat evolution, and the root redundancy reduces with the increase of ploidy chromosomes, which result in the increase of wheat WUE at whole plant level.     

The ecological sequence of Hipparion fauna in the mid-dle reaches of the Yellow River during Neogene

The faunal ecological type and sequence in the Tertiary red clay indicate that Hipparion fauna during the period 7.4-6.1 Ma in the middle reaches of the Yellow River is composed mainly of dorcadoides and mixed types. This represents semiarid veld environment with small fluctuation. The fossil assemblages characterized by the abundance of gaudryi types and even the occurrence of some Hominoid and Chalicotherium indicate an obviously warm and humid period since 5.3 Ma. The fossil assemblages during 3.4 Ma show the typical steppe fauna representing dry climate. It is indicated by the changes of ecological sequence that the climatic conditions in Pliocene are drier than that in late Miocene. The clay-skin content of red clay, which has a synchronous change with faunal features, is a rather good replacing palaeoclimatic index.     

The ecological sequence of Hipparion fauna in the middle reaches of the Yellow River during Neogene

The faunal ecological type and sequence in the Tertiary red clay indicate that Hipparion fauna during the period 7.4–6.1 Ma in the middle reaches of the Yellow River is composed mainly of dorcadoides and mixed types. This represents semiarid veld environment with small fluctuation. The fossil assemblages characterized by the abundance of gaudryi types and even the occurrence of some Hominoid and Chalicotherium indicate an obviously warm and humi period since 5.3 Ma. The fossil assemblages during 3.4 Ma show the typical steppe fauna representing dry climate. It is indicated by the changes of ecological sequence that the climatic conditions in Pliocene are drier than that in late Miocene. The clay-skin content of red clay, which has a synchronous change with faunal features, is a rather good replacing palaeoclimatic index.