n维Oppenheim不等式及其应用

设ａ＿ｉ（ｉ＝１，２，３）为三角形ΔＡ＿１Ａ＿２Ａ＿３的边长，Ｓ为ΔＡ＿１Ａ＿２Ａ＿３的面积，λ＿ｊ（ｊ＝１，２，３）为任一组正数．作者将Ｏｐｌｓｏｎｂｅｉｍ三角形不等式推广到ｎ维欧氏空间Ｅ￣ｎ中的ｎ维单形，从而获得了ｎ维单形的Ｏｐｐｅｎｂｅｉｍ不等式这里Ｖ是ｎ维单形Ａ＿１Ａ＿２…Ａ＿（ｎ＋１）的体积，Ｖ＿ｉ为顶点Ａ＿ｉ所对之侧面的面积，λ＿ｉ为任意一组正数．     

时间序列引出的数学问题(Ⅱ)

Ｘ′＝（ｘ１，ｘ２…，ｘｎ），问在∑ｎｉ＝１ｘ２ｉ≤１条件下，ａ３＝∑ｎ－２ｉ＝１ｘｉｘｉ＋２，ａ５＝∑ｎ－１ｉ＝１ｘｉｘｉ＋１，当Ｘ取遍∑ｎｉ＝１ｘ２ｉ≤１上的点，（ａ３，ａ５）在平面上构成怎样的图形？该文对ｎ＝４给出解析解     

时间序列引出的数学问题（三）

若Ｘ′＝（ｘ１,ｘ２,…,ｘｎ）,问在ｎｉ＝１ｘ２ｉ≤１条件下,ａ３＝ｎ－２ｉ＝１ｘｉｘｉ＋２,ａ５＝ｎ－１ｉ＝１ｘｉｘｉ＋１,当ｘ取遍ｎｉ＝１ｘ２ｉ≤１的点,（ａ３,ａ５）在平面上构成怎样的图形．该文对ｎ＝５给出解析解．     

一类食饵具有常数存放率的n次Kolmogorov系统的极限环

本文讨论一类食饵具有常数存放率的ｎ次Ｋｏｌｍｏｇｏｒｏｖ微分系统其中ａ＿０，ａ＿２，ｂ＿１，和ｂ＿２是正常数；Ｆ是负常数；ａ＿１和ａ＿３不定号，得到下列结论：ｌ：当Ａ＿１－２Ａ＿３＋ｍ＞０时，系统（１）在第一象限存在唯一稳定的极限环２：当Ａ＿１－２Ａ＿３≤０时，系统（１）在第一象限全局稳定     

时间序列引出的数学问题（II）

Ｘ＇＝（ｘ１，ｘ２，…，ｘｎ），问在Σｉ＝１↑ｎｘｉ＾２≤１条件下，ａ３＝Σｉ＝１↑ｎ－２ｘｉｘｉ＋２，ａ５＝Σｉ＝１↑ｎ＝１ｘｉｘｉ＋１，当Ｘ取遍Σｉ＝１↑ｎｘｉ＾２≤上的点，（ａ３，ａ５）在平面上构成怎样的图形？该文对ｎ＝４给出解析解。     

分担两个值的亚纯函数

该文主要证明如下的定理１ 　设ｆ 和ｇ 为非常数亚纯函数,ａ１ , …,ａｎ 为互异复数,若（ｉ） ｆ 和ｇ ＣＭ 分担ａ１ ,ａ１ ,（ｉｉ） δ（ ∞,ｆ）＝ δ（ ∞,ｇ） ＝１ ,（ｉｉｉ） ａ３ ,…,ａｎ 为ｆ 的亏值,满足ｎｊ＝３δ（ａｊ ,ｆ） ＞ ｎ － ２ｎ ,则（ａ） 当ｎ ＝ ３ 时,有ｆ ≡ｇ 或（ｆ － ａ３）（ｇ ＋ ａ３ － ａ１ － ａ２） ≡（ａ３ － ａ１）（ａ２ － ａ３）且有δ（ ａ３ , ｆ） ＝ １, δ（ａ１ ＋ ａ２ － ａ３ , ｇ） ＝ １,（ｂ） 当ｎ ＞ ３ 时,有ｆ ≡ｇ 。     

次Hermite矩阵的次正定性

若ｎ阶次Ｈｅｒｍｉｔｅ矩阵Ａ，对任意非零向量Ｘ＇＝（ｘ＿１，ｘ＿２，…ｘ＿ｎ）∈Ｒ￣ｎ，有ＡＸ＞０，则称次Ｈｅｒｍｉｔｅ矩阵Ａ是次正定的．给出了判定次Ｈｅｒｍｉｔｅ矩阵次正定的几个充要条件：定理ｎ阶次Ｈｅｒｍｉｔｅ矩阵Ａ是次正定的，当且仅当下列条件之一成立：（ｌ）Ｈｅｒｍｉｔｅ矩阵ＪＡ是正定的；（２）存在ｎ阶可逆复矩阵Ｐ，使ＡＰ＝Ｊ；（３）次Ｈｅｒｍｉｔｅ矩阵Ａ的４ｋ阶，４ｋ十互阶下次主子式为正，４ｋ＋２阶，４ｋ＋３阶下次主子式为负；（４）存在ｎ阶可逆复矩阵Ｐ，使其中λ＿ｉ＞０，ｉ＝１，２，…，ｎ。     

两分子饱和反应系统的极限环的存在性与唯一性

陈兰荪等在第二届中国生物数学学术会议上提出了生物动力学系统中研究的１１个问题。作者所研究的是第１１个问题，生物化学中两分子饱和反应。其数学模型为ｘ＝Ｊ＿１（１＋ｘ＋ｙ＋Ａｘ￣２）－ｘ（１＋ｘ＋ｙ＋Ａｘ￣２）－Ｂｘｙ；ｙ＝Ｊ＿２（１＋ｘ＋ｙ＋Ａｘ￣２）－Ｂｘｙ．其中：Ｊ＿１、Ｊ＿２、Ａ、Ｂ为非负常数，当Ｊ＿１－３Ｊ＿２＜－［１＋Ｂｘ＋（Ｂ＋１）ｙ］／（１＋Ａｘ）时，该模型在第一象限内至少存在一个极限环；当Ｊ＿１＜Ｊ．ｘ＜ｙ，Ｂ＞ｌ且ｘ＞ａ时，该模型在第一象限内存在唯一的极限环。其中ａ＜０为方程ｐ（ｘ＝）＝０的最大负实根．     

图的圈长分布和圈长分布唯一的图

阶为ｎ的图Ｇ的圈长分布是指序列（ｃ１，ｃ２，…，ｃｎ），其中ｃｉ是Ｇ中长为ｉ的圈数．若不存在，使Ｇ’与Ｇ有相同的圈长分布，则称图Ｇ是圈长分布唯一图．本文确定了Ｋｎ－Ａ（｜Ａ｜＝ｊ，ｎ≥｜Ａ｜＋３）的最小、最大的４圈和５圈数．证明了当ｎ≥９时，Ｋｎ－Ａ（｜Ａ｜＝４）以及当ｎ≥１４时，Ｋｎ－Ａ（｜Ａ｜＝５）都是圈长分布唯一图．     

关于n~(1/2)∫_0~(π/2)(sin~nxdx(n→∞))渐近级数展开计算

运用文献［１］的结果建立了如下的渐进展开式：ｎ∫π／２０ｓｉｎｎｘｄｘ～π２∞ｉ＝０ａｉｎｉ其中，ａｌ由下面的递推公式所决定：ｌｉ＝０ａｉｂｌ－ｉ＝（－１）ｌ１／２（１／２－１）…（１／２－ｌ＋１）ｌ！，ａ０＝１，ｌ＝１，２，３式中：ｂ０＝１，ｂ１＝ａ１，ｂｉ＋１＝ａ１＋ｉ１！ａ２＋ｉ（ｉ－１）２！ａ３＋…＋ｉ（ｉ－１）…（ｉ－ｉ＋２）（ｉ－１）！ａｉ＋ｉ！ｉ！ａｉ＋１，ｉ＞１这个新递推公式的作用是简化了系数计算的复杂性。此外，还给出了有关的Ｗａｌｉｓ公式渐进性的应用。     

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