局部紧Lindelf空间的序列覆盖映象

利用特定的覆盖性质,借助序列覆盖映射,建立局部紧L indelo。f空间和cs覆盖、sn覆盖、cs*覆盖之间的联系,以及局部紧L indelo。f空间的序列覆盖映象特征,得到并深化局部紧L indelo。f空间的一些相应结果,完善了局部紧L indelo。f空间的映射理论.     

局部紧LindelÖf空间的序列覆盖映象

利用特定的覆盖性质,借助序列覆盖映射,建立局部紧Lindelöf空间和cs覆盖、sn覆盖、cs*覆盖之间的联系,以及局部紧Lindelöf空间的序列覆盖映象特征,得到并深化局部紧Lindelöf空间的一些相应结果,完善了局部紧Lindelöf空间的映射理论.     

局部紧Lindel(o)f空间的序列覆盖映象

利用特定的覆盖性质,借助序列覆盖映射,建立局部紧Lindel(o)f空间和cs覆盖、sn覆盖、cs*覆盖之间的联系,以及局部紧Lindel(o)f空间的序列覆盖映象特征,得到并深化局部紧Lindel(o)f空间的一些相应结果,完善了局部紧Lindel(o)f空间的映射理论.     

仿紧局部可分空间的一些注记

研究了仿紧局部可分空间在一些L映射下象的性质后,文章继续讨论仿紧局部可分空间的映象问题。给出了点可数k覆盖与sL系之间的关系并进一步得到仿紧局部可分空间在一些紧覆盖映射下的象与k覆盖以及与sL系之间的关系,探讨了仿紧局部可分空间在2-序列覆盖L-映射下的象与序列开覆盖之间的联系,建立了仿紧局部可分空间的一些L-映象之间的联系。     

仿紧局部紧空间的L-映象

讨论了仿紧局部紧空间在一些特定L-映射(sL-映射)下象的性质,给出了仿紧局部紧空间在2-序列覆盖L-映象(sL-映象)的内在特征,建立了仿紧局部紧空间在一些L-映射(sL-映射)下象的联系．     

仿紧局部cosmic空间的一些注记

本文讨论了仿紧局部cosmic空间在一些特定L-映射下象的性质,给出了仿紧局部cosmic空间的2-序列覆盖L-映象的内在特征,建立了仿紧局部cosmic空间在一些L-映射下象的联系。     

仿紧局部Lindelof空间的一些映象

给出仿紧局部Ｌｉｎｄｅｌｏｆ空间的一个特征,建立这种空间的几类序列覆盖Ｌ映象和高映象的特征,证明了商ｓｓ映射保持仿紧局部Ｌｉｎｄｅｌｏｆ空间。     

仿紧局部Lindel(o)f空间的一些注记

文章在研究了仿紧局部Lindel(o)f空间在一些特定L映射下象的基础上,继续讨论仿紧局部Lindel(o)f空间的2-序列覆盖L-映象;建立了仿紧局部Lindel(o)f空间的一些L-映象之间的联系.     

仿紧局部Lindel(o)f空间的一些映象

给出仿紧局部Lindel f空间的一个特征 ,建立这种空间的几类序列覆盖L映象和商映象的特征 ,证明了商ss映射保持仿紧局部Lindel f空间 .     

局部可分度量空间的序列覆盖紧映像

该文借助点星网和具有不同性质的覆盖列来探讨局部可分度量空间中的各类序列覆盖紧映像,并得出了局部可分度量空间的序列覆盖紧映像、1-序列覆盖紧映像和2-序列覆盖紧映像的内在刻画,从而使得关于度量空间的紧映像的内在刻画更加趋于完善.     

一类包含σ紧空间和可分空间的拓扑空间

定义*σ紧空间的概念，讨论*σ紧空间的一些性质以及*σ紧性与*Lindelo(e)性。c，c，c与可分性之间的关系。结合点可数基讨论了一些空间的某些性质。     

强C*-代数值度量空间及其不动点定理

在C*-代数值度量空间基础上,给出强C*-代数值b-度量空间的概念,并证明了一个压缩条件下的不动点定理.做为应用,文中给出了某类算子方程中解的存在性及唯一性的判定.      

具有σ-局部可数cs* - 网的空间

利用ponomarrv's 方法及msss 映射的定义, 研究了广义度量空间中的点可数覆盖问题. 证明了具有σ-局部可数cs^* - 网的空间可以刻划成度量空间的序列覆盖映射和强序列覆盖映射下的象, 从而使关于对σ- 局部可数族的讨论趋于完整.     

Characterization of type<Emphasis Type="Italic">p</Emphasis> Banach spaces by the weak law of large numbers

For weighted sums of the form where {a _nj , 1 ⩽j⩽k _n ↑∞,n⩾1} is a real constant array and {X _aj , 1≤j≤k _{n, n}≥1} is a rowwise independent, zero mean, random element array in a real separable Banach space of typep, we establishL ^r convergence theorem and a general weak law of large numbers respectively, conversely, we characterize Banach spaces of typep in terms of convergence inr-th mean and probability for such weighted sums. Foundation item: Supported by the National Natural Science Foundation of China (No. 10071058) Biography: Gan Shi-xin (1939-), male, Professor, research direction: martingale theory, probability limiting theory and Banach space geometry theory.     

Synoptic-scale variation of δ18O in summer monsoon rainfall at Lijiang, China

Based on the daily δ~(18)O data in June―September 2003 at Lijiang and the daily mean NCEP/ NCAR reanalysis data, synoptic-scale variation of δ~(18)O in summer monsoon rainfall was investigated. The 'precipitation amount effect' is obvious for the daily δ~(18)O variation, whereas the 'temperature effect' is insignificant. Alternate occurrences of active phase and break phase of the southwest monsoon probably influence the synoptic-scale δ~(18)O variation prominently. Moreover, the isotopic composition in precipitation during the late monsoon months is presumably influenced significantly by recycling of monsoon precipitation. Both the above factors disturb the 'amount effect' of isotopic variation in the monsoon region. This study also indicates that the synoptic-scale rainfall δ~(18)O variation at Lijiang in summer is domi-nated by the Indian monsoon depression (low pressure) system at large scale. These results are important for further studying the 'amount effect' and reconstructing paleoclimate in the monsoon region.     

The concentration quenching characteristics of 5D3-7FJ and 5D4-7FJ (J=0―6) transitions of Tb3+ in YBO3:Tb3+ phosphor

The photoluminescence quenching behaviors of ^5D3-^7Fj and ^5D4-^7Fj （J = 0—6） transitions of Tb^3＋ in YBO3：Tb under 130—290 nm excitation were systematically investigated. The results revealed that the quenching concentrations of both ^5D3-^7Fj and ^5D4-^7Fj transitions of Tb^3＋ in YBO3：Tb were mainly dependent on excitation wavelength. Particularly, the quenching concentrations of ^5D4-^7Fj transitions of Tb^3＋ under 130—290 nm excitation were correlated with excitation bands of YBO3：Tb. The quenching concentrations of ^5D3-^7Fj transitions remained at low concentration （2%） under 186—290 nm excitation and then increased gradually with energy of incoming excitation photon when excited at 130—186 nm. This dependence should be involved in their excitation mechanisms and quenching pathway in particular excitation region.[第一段]     

Superconvergence for L2-projection in finite elements

Two classes of superconvergence points for L 2 projection u\-n in n degree finite elements on uniform grids are shown by element analysis method. Superconvergence points of u n are n+1 order Gauss point G n+1 for odd d≥1 (so the endpoint of each element is of superconvergent), and n+1 order pointset Z n+1 for even n ≥2 (which includes the endpoints and midpoint), respectively. Symmetry point is only an important part of them.     

A sufficient condition fork′(z)(k(z)∈H q,q≥1) to be ofH 1

We proved ifk(z)∈H ^q (q≥1),g(z) is analytic on |z|=1, , thenk′(z)∈H ¹, especially, ifq=1, thenk(z) is an analytic function on the closed unit disk |z|≤1. Peng Zhigang: born in June 1970, Ph. D     

Southwest monsoon changes indicated by oxygen isotope of ostracode shells from sediments in Qinghai Lake since the late Glacial

The δ 18O records of ostracode shells in sediments of core QH-2000 from Qinghai Lake can be used as a better proxy to reflect monsoon changes. Low monsoon precipitation between 17.5 and 11 cal. ka BP is indicated by positive δ 18O values averaging 2.37‰. A fast shift in δ 18O from positive at 11 cal. ka BP to negative at 10 cal. ka BP indicates sharp increase of monsoon precipitation. An interval of generally high monsoon precipitation is observed between 10 and 6 cal. ka BP with δ 18O values averaging -2.15‰. Decrease of monsoon precipitation between 6 and 2.5 cal. ka BP is indicated by positive δ 18O values. δ 18O keeps positive values averaging 3.0‰ between 2.5 and 0 cal. ka BP suggesting low high monsoon precipitation. The climatic changes indicated by δ 18O records of ostracode shells in sedi- ments of core QH-2000 from Qinghai Lake and our broader regional comparison show that the climate in Qinghai Lake since the late Glacial is probably controlled by southwest monsoon other than southeast monsoon.