拟相似算子本性谱的连通成分

设A和B是拟相似算子,△是Wolf本性谱σ_c(B)的任一个连通成分。本文证明了△∩σ_■(A)∩σ_■(B)≠φ及△∩(σ_■(A)∩σ_■(B))≠φ。并证明了若△σ_K(B)的一个连通成分,则△∩(σ_F(A)∩σ_F(B))≠φ等价于△∩(σ_■(A)∩σ_■(B))≠φ,进而给出△∩σ_■(A)∩σ_■(B)≠φ的充要条件,其中σ_K(T)=σ_■(T)∩σ_■(T),σ_■(T)=σ_K(T)\(P'_∞(T)~0∪P'_(∞∞)(T)~0),P'_∞(T)={λ∈C:v(T-λ)-μ(T-λ)=±∞},P_(∞∞)~'(T)={λ∈C:v(T-λ)=μ(T-λ)=∞}。     

算子的拟相似与Kato本质谱的连通分支

设算子A和B拟相似,τ是Kato本质谱σ_K(B)的连通分支,本文研究τ∩σ_K(A)≠φ的充分条件和必要条件以及τ与σ_B(A)的某些子集的相交关系。     

缺项算子矩阵的左谱

设A∈B(ye),B∈B(k),C∈(B)((k),(ye))给定,对X∈B((ye),(k))定义Mx=(AXCB)ye( )k→ye( )(k).在一定条件下刻画集合∩X∈B((k),(ye))σl(Mx)和∩X∈B((k),(ye))σl(Mx),其中σl(T)和σr(T)分别表示算子T的左谱和右谱.利用了算子矩阵的分块技巧和算子分块的几何结构.在C是闭值域的条件下,完全刻画了∩X∈B((k),(ye))σl(Mx)和∩X∈B((k),(ye))σl(Mx).此刻画在缺项算子矩阵的谱的研究中是新的结果,应用该刻画可以得到若干已知结论.     

两个算子乘积的{1,3,4}逆序律

利用算子分块矩阵的技巧,研究了两个算子乘积的{1,3,4}逆的广义逆序律,证明了当R(A)、R(B)以及R(AB)都闭时,(AB){1,3,4}=B{1,3,4}.A{1,3,4}当且仅当R(B)=R(A*AB),或者R(A*)R(B)且B*(R(B)∩N(A))=B+(R(B)∩N(A))。     

无穷维Hamilton算子纯虚谱的扰动

研究了Hilbert空间X⊕X中的无穷维Hamilton算子HC=[A C 0 -A*]和HF=[A F B -A*]的纯虚谱的扰动,其中R(B)是闭的.给定算子A,B,证明了∩C∈S(X)σi(HC)=σiπ(A),∪C∈S(X)σi(HC)=σi(A),∩F∈S(X)σi(HF)=σiπ(APR(B)⊥),∪F∈S(X)σi(HF)=σi(APR(B)⊥),其中σi(T),σiπ(T),PM和S(X)分别表示T的纯虚谱,纯虚近似谱,全空间到M的正交投影和X中的所有自伴算子所成之集.     

关于算子X→AX-XB和X→AXB-X

设A,B是Hilbert空间H上的算子,定义B(H)上的算子τ=τ(A,B),J=J(A,B)为τ(X)=AX-XB,J(X)=AXB-X。本文求得了算子J的近似点谱、剩余谱,给出了J的值域在B(H)中按范数拓扑稠密的充要条件,推广了Fialkow的结果。     

一类算子的谱理论(Ⅰ)——(AC)算子的基本性质

设X是复B-空间,B(X)是X上有界线性算子全体,C是复平面,F是C的一切闭子集类,我们引入一类算子,并研究它的谱理论,算子T∈B(X)称为(AC)算子,若T有性质(A)与(C),我们证明:(1)T∈B(X)是(AC)算子当且仅当对F到X的闭子空间类的同态X(·)满足下述条件:(ⅰ)(F_1∩F_2)=X(F_1)∩X(F_2);(ⅱ)X(φ)={0},X(C)=X;(ⅲ)TX(F)X(F);(ⅳ)σ(T|X(F))F;(ⅴ)对x∈X若存在解析函数x(λ):CF→X,使(λI-T)x(λ)=x,则x(λ)∈X(F),λ∈CF,(2)设T∈B(X)是(AC)算子,则对任何F∈F,有:(ⅰ)若X_T(F)≠{0},则F∩σ(T)≠φ;(ⅱ)若X_T(F)={0},则F∩σ_p(T)=φ,(3)设T∈B(X),σ(T)位于光滑Jordan曲线Γ上,又对每个z∈Γ,存在Γ邻域V上非零解析函数f(z),使 ‖f(z)R(λ,T)‖≤M_z,λ≠z,λ∈V,M_z>0,则T是(AC)算子。     

Banach空间上算子谱的精细划分

给出巴拿赫空间上算子谱的精细划分,证明了巴拿赫空间上的算子T有σ0p(T)＝ψ0(T)∩(T),σ(T)＝σB(T)∪σ0p(T)＝σW(T)∪(ψ0(T)∩σ(T)0)∪σ0p(T).     

上三角算子矩阵和广义Drazin谱的极限点

研究了上三角算子矩阵广义Drazin谱的极限点的填洞问题，并在此基础上给出了使得accσ_gD(M_C)=accσ_gD(A)∪accσ_gD(B)成立的充分条件，其中A∈B(X),B∈B(Y),C∈B(Y,X)且■     

广义Anderson定理

利用谱分解方法研究算子Φ(Χ)=AXB的不动点与值域的关系.证明了如果算子A,B*是压缩控制算子且Φ(S)=S,则对任意的算子X∈B(H)都有‖AXB-X+S‖≥‖S‖.     

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

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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