(B(H))上保交换零积的可加映射

讨论了B(H)上保交换零积的可加映射,其中B(H)是由Hilbert空间H上的有界线性算子全体组成的Banach代数。首先给出了在有限维情形下,若Φ是保交换零积的可加满射,使得Φ(I)=I,并且对每个一秩幂等算子P∈Mn都有Φ(FΦ)FΦ(P),则Φ是一个自同构或反自同构。进一步给出了无限维情形下,若Φ是保交换零积可加满射,则Φ是非零数乘一个环同构或一个环反同构。     

标准算子代数上保Jordan零积的可加映射

设A和B分别是无限维的实或复Banach空间X和Y上的标准算子代数,F(X)是X上的所有有限秩算子组成的代数。设Φ:A→B是一个保单位的可加满射。文章在对Φ的值域range(Φ)附加条件比较弱的假设下证明了映射Φ单边保Jordan零积(AB+BA=0→Φ(A)Φ(B)+Φ(B)Φ(A)=0),则要么Φ|F(X)=0,要么Φ是下面四种形式之一:代数同构,共轭代数同构,代数反同构,以及共轭代数反同构。     

弱δθ-可加空间的逆极限

主要证明了如下两个结果:设X=lim←{Xσ,πσρ,σ},并且每个πσ是开满映射,(1) 如果X是|Σ|-仿紧的且每个Xσ是正规弱δθ-可加的,则X是正规弱δθ-可加的;(2) 如果X是遗传|Σ|-仿紧的且每个Xσ是遗传正规的遗传弱δθ-可加空间,则X是遗传正规的遗传弱δθ-可加空间.     

自伴算子空间上满足[φ(A~2),A]+[A~2,φ(A)]=0的可加映射

运用算子论的方法,研究了自伴算子空间上满足[φ(A2),A]+[A2,φ(A)]=0的可加映射。如果可加映射φ:Bs(H)→Bs(H)满足对所有A∈Bs(H)有[φ(A2),A]+[A2,φ(A)]=0,那么存在λ∈R,可加映射f:Bs(H)→R,以及算子K∈Bs(H),使得对所有A∈Bs(H)有φ(A)=iAK-iKA+λA+f(A)I。即自伴算子空间上满足[φ(A2),A]+[A2,φ(A)]=0的可加映射是导子与可交换映射之和。     

正规弱θ-可加细空间的无限乘积

主要证明了如下结果(1)如果是X=∏σ∈Xσ是||-仿紧空间, 则X是正规弱θ-可加细空间当且仅当F∈[]＜ω,∏σ∈F Xσ是正规弱θ-可加细空间.(2)设X=∏i∈ωXi 是可数仿紧的, 则下列3条等价X是正规弱θ-可加细的;F∈[ω]＜ω,∏ i∈FXi是正规弱θ-可加细的;n∈ω ,∏i≤n Xi是正规弱θ-可加细的.     

正规弱-可加细空间的无限乘积

主要证明了如下结果 :(1)如果是X =∏σ∈ Xσ 是 | |-仿紧空间 ,则X是正规弱θ -可加细空间当且仅当 F∈ [ ]<ω,∏σ∈FXσ 是正规弱θ -可加细空间 .(2 )设X =∏i∈ωXi 是可数仿紧的 ,则下列 3条等价 :X是正规弱θ -可加细的 ; F∈ [ω]<ω,∏i∈FXi 是正规弱θ -可加细的 ; n∈ω ,∏i≤nXi 是正规弱θ -可加细的 .     

B(X)上的(m,n)-Lie中心化子

设X是实数域或复数域F上维数大于1的Banach空间，Ф:B(X)→B(X)是一个可加映射。证明了如果存在正整数m,n使得(m+n)Ф([A,B])=m[Ф(A),B]+n[A,Ф(B)]对任意A,B∈B(X)且AB=P（其中P∈B(X)是一个固定的非平凡幂等元）成立，则存在λ∈F及在AB=P的换位子上为零的可加映射h:B(X)→F使得对任意A∈B(X),有Ф(A)=λA+h(A)I.     

B(X)上Lie中心化子的刻画

设X为实或复数域F上维数大于1的Banach空间, φ:B(X)→B(X)是一个可加映射。 证明了如果存在正整数m,n使得(m+n)φ(［A,B］)=m［φ(A),B］+n［A,φ(B)］对所有A,B∈B(X)成立, 则存在λ∈F及在换位子为零的可加映射h:B(X)→F使得对任意A∈B(X), 有φ(A)=λA+h(A)I。     

保持算子乘积部分等距的可加映射

设B(H)是复Hilbert空间H上的有界线性算子全体组成的Banach代数。证明B(H)上的可加满射Φ双边保持算子乘积是非零部分等距的充要条件是存在H上的酉算子或共轭酉算子U以及常数λ∈T,使得Φ(X)=λUXU~*,■X∈B(H),其中T表示复平面C上的单位圆周。同时,刻画了保持两个算子Jordan三乘积是非零部分等距的可加映射。     

Hilbert空间上的保内积映射和保距映射

本文给出Hilbert空间上保内积映射和保距映射的完全刻画.设H,K是实(或复)Hilbert空间,φ:H→为一映射,我们证明了φ为保内积映射的充要条件是φ为线性等距算子;φ为保距映射且φ0=0的充要条件是φ为线性等距算子;而φ为保距映射的充要条件是φ为一个平移映射与一个线性等距算子的复合.     

An Index mechanism for multi-scale view in spatial databases

There are numerous geometric objects stored in the spatial databases. An importance function in a spatial database is that users can browse the geometric objects as a map efficiently. Thus the spatial database should display the geometric objects users concern about swiftly onto the display window. This process includes two operations:retrieve data from database and then draw them onto screen. Accordingly, to improve the efficiency, we should try to reduce time of both retrieving object and displaying them. The former can be achieved with the aid of spatial index such as R-tree, the latter require to simplify the objects. Simplification means that objects are shown with sufficient but not with unnecessary detail which depend on the scale of browse. So the major problem is how to retrieve data at different detail level efficiently. This paper introduces the implementation of a multi-scale index in the spatial database SISP (Spatial Information Shared Platform) which is generalized from R-tree. The difference between the generalization and the R-tree lies on two facets: One is that every node and geometric object in the generalization is assigned with a importance value which denote the importance of them, and every vertex in the objects are assigned with a importance value,too. The importance value can be use to decide which data should be retrieve from disk in a query. The other difference is that geometric objects in the generalization are divided into one or more sub-blocks, and vertexes are total ordered by their importance value. With the help of the generalized R-tree, one can easily retrieve data at different detail levels.Some experiments are performed on real-life data to evaluate the performance of solutions that separately use normal spatial index and multi-scale spatial index. The results show that the solution using multi-scale index in SISP is satisfying.     

Characterization of Ordovician carbonate reservoirs, southeastern Saskatchewan, Canada

The discovery of the prolific Ordovician Red River reservoirs in 1995 in southeastern Saskatchewan was the catalyst for extensive exploration activity which resulted in the discovery of more than 15 new Red River pools. The best yields of Red River production to date have been from dolomite reservoirs. Understanding the processes of dolomitization is, therefore, crucial for the prediction of the connectivity, spatial distribution and heterogeneity of dolomite reservoirs.The Red River reservoirs in the Midale area consist of 3～4 thin dolomitized zones, with a total thickness of about 20 m, which occur at the top of the Yeoman Formation. Two types of replacement dolomite were recognized in the Red River reservoir: dolomitized burrow infills and dolomitized host matrix. The spatial distribution of dolomite suggests that burrowing organisms played an important role in facilitating the fluid flow in the backfilled sediments. This resulted in penecontemporaneous dolomitization of burrow infills by normal seawater. The dolomite in the host matrix is interpreted as having occurred at shallow burial by evaporitic seawater during precipitation of Lake Almar anhydrite that immediately overlies the Yeoman Formation. However, the low δ18O values of dolomited burrow infills (-5.9‰～ -7.8‰, PDB) and matrix dolomites (-6.6‰～ -8.1‰, avg. -7.4‰ PDB) compared to the estimated values for the late Ordovician marine dolomite could be attributed to modification and alteration of dolomite at higher temperatures during deeper burial, which could also be responsible for its 87Sr/86Sr ratios (0.7084～0.7088) that are higher than suggested for the late Ordovician seawaters (0.7078～0.7080). The trace amounts of saddle dolomite cement in the Red River carbonates are probably related to "cannibalization" of earlier replacement dolomite during the chemical compaction.     

A computer generator for randomly layered structures

AcomputergeneratorforrandomlylayeredstructuresYUJia shun1,2,HEZhen hua2(1.TheInstituteofGeologicalandNuclearSciences,NewZealand;2.StateKeyLaboratoryofOilandGasReservoirGeologyandExploitation,ChengduUniversityofTechnology,China)Abstract:Analgorithmisintrod…     

Perspherical Approaches for Electrons in Atoms and Charged Excitons in Quantum Wells

Instead of following Fock’s expansion,we solve the Schrodinger equation for some quantum mechanical manybody systems such as electrons in atoms and charged excitons in quantum wells in a similar way in hyperspherical coordinates by expanding the wave functions into orthonormal complete basis sets of the hyperspherical hannonics(HHs)of hyperangles and generalized Laguerre polynomials(GLPs)of the hyperradius.This leads the equation to     

Advances in broadband wireless communications under high-mobility scenarios

Future mobile communication systems aim at providing very high data transmission rates, even in high-mobility scenarios such as high-speed wheel-track trains, maglev trains, highway vehicles, airplanes, guided missiles or spacecraft. A particularly important commercial application is the strong and increasing worldwide demand for high- speed broadband wireless communications （up to 574.8 km/ h test speeds or 380 km/h commercial speeds） in railways, providing data, voice and video services for applications such as onboard entertainment services to passengers, train control, train dispatch, train sensor status handling and sur- veillance. In such high-mobility scenarios, there are a number of communication challenges, including fast hand- over, location updating, high-speed channel modeling, estimation and equalization, anti-Doppler spreading tech- niques, fast power control, and dedicated network architec- ture. Because signal transmission in very high-speed scenarios will inevitably experience serious deterioration, it is imperative to develop key broadband mobile communi- cation techniques for such high-speed vehicles.     

Wuhan University Journal of Natural Sciences TOTAL CONTENTS

<正>~~     

海南岛地体及其毗邻陆缘晚中生代—新生代古地磁研究和构造演化

本文叙述了对海南岛及其毗邻大陆边缘白垩纪到第四纪地层岩石进行古地磁研究的全部工作过程。通过分析岩石中剩余磁矢量的磁偏角及磁倾角的变化,提出海南岛白垩纪以来经历的构造演化模式如下:早期伴随顺时针旋转而向南迁移,后期伴随逆时针转动并向北运移。联系该地区及邻区的地质、地球物理资料,对海南岛上述的构造地体运动提出以下认识:北部湾内早期有一拉张作用,主要是该作用使湾内地壳显著伸长减薄,形成北部湾盆地。从而导致了海南岛的早期构造运动,而海南岛后期的构造运动则主要是受南海海底扩张的影响。海南地体运动规律的阐明对于了解北部湾油气盆地的形成演化有重要的理论和实际意义。     

Scale-based spatial data model for GIS

Being the primary media of geographical information and the elementary objects manipulated, almost all of maps adopt the layer-based model to represent geographic information in the existent GIS. However, it is difficult to extend the map represented in layer-based model. Furthermore, in Web-Based GIS, It is slow to transmit the spatial data for map viewing. In this paper, for solving the questions above, we have proposed a new method for representing the spatial data. That is scale-based model. In this model we represent maps in three levels: scale-view, block, and spatial object, and organize the maps in a set of map layers, named Scale-View, which associates some given scales.Lastly, a prototype Web-Based GIS using the proposed spatial data representation is described briefly.     

Exciton Seebeck in Molecular Systems

Various applications relevant to the exciton dynamics,such as the organic solar cell,the large-area organic light-emitting diodes and the thermoelectricity,are operating under temperature gradient.The potential abnormal behavior of the exicton dynamics driven by the temperature difference may affect the efficiency and performance of the corresponding devices.In the above situations,the exciton dynamics under temperature difference is mixed with     

Achieving Unusual States of Matter Under High Pressure

The elongation method,originally proposed by Imamura was further developed for many years in our group.As a method towards O(N)with high efficiency and high accuracy for any dimensional systems.This treatment designed for one-dimensional(ID)polymers is now available for three-dimensional(3D)systems,but geometry optimization is now possible only for 1D-systems.As an approach toward post-Hartree-Fock,it was also extended to