加权环簇的轨形结构

环簇和轨形在数学和物理中具有广泛的联系.单纯环簇实际上就是一类具有良好结构的轨形.作者通过推广扇集和环簇之间的对应,定义了加权扇集和加权环簇,并给出了它们之间的对应.然后,作者讨论了加权环簇的性质,并证明了单纯加权环簇也具有轨形结构.     

轨形上的广群、丛束和周期磁单极定理

证明了每个平凡丛束都是可微广群,将流形上周期磁单极对应推广到轨形上,证 明 了 Ｇ 主轨丛的回路丛是ＦｒéｃｈｅｔＬＧ主丛,并且还在轨形上引入了 Ｃ× 广群、丛束的概念,从而推广了一些流形上的结论．      

四辊万能孔型中轨形件宽展的数值解

根据轨形件的形状特点和其在四辊万能孔型中变形特征，简化了其断面形状，并划分成７个区域．建立了各区的运动许可速度场，得到含５个变分参数总功率泛函表达式．由泛函极小化条件，用Ｐｏｗｅｌ算法，求解出轨形件头部和底部宽展的数值解．计算表明，头与底部宽展规律不同，理论值与实测值的吻合较好     

从卡-丘空间到轨形拓扑

当今弦理论最美妙的运用是卡－丘空间,但成千上万种的卡－丘空间也带来选择的困境,而类似的难题都能通过黎曼切口和轨形拓扑等数学思想,组织、纳入宏大而系统的三旋理论框架给予解决。     

轻轨CARD系统孔型设计模型

研究了轻轨ＣＡＲＤ系统孔型设计数学模型的建立方法,在总结和分析大量现场数据的基础上,用回归分析建立了轻轨ＣＡＲＤ系统轨形孔孔型设计模型,并成功的用在轻轨ＣＡＲＤ系统的开发中,经厂家试用效果很好。     

旧重轨轧制轻孔型系统的设计

从重轨和轻轨的断面特点了，在试验的基础上，提出了万能轧腰变形的方法、成功地解决了旧重轨轧制轻轨过程中压高变的难题。为此，设计了一套由轧腰孔型系统和轨形孔形系统组成的旧重轨轧制轻轨孔型系统，并获得符合标准的２４ｋｇ／ｍ轻轨实样。     

轨形与弦拓扑

轨形理论是近数十年来发展起来的一个交叉性数学课题,与许多不同的数学分支如代数几何、微分几何、拓扑、代数及弦理论相关。本书是关于这个理论的引论,给出了它的基本概念、主要结果以及来自代数几何、代数拓扑及几何学的基本技术,特别给出许多来自代数几何和弦理论的例子,核心内容是Chen．Ruan上同调的精细刻划,并且将统理论作为这个研究的一个主要动因。     

数字图书馆的概念与内涵的研究

简要介绍了数字图书馆的发展 ,对数字图书馆的定义进行了概括 ,指出了信息资源数据库群建设的重要性和方法 ,肯定了数字图书馆的发展趋势 ,指出了数字图书馆建设是涵盖广泛学科及技术领域的漫长过程 ,提出了数字图书馆资源建设的必要性、重要作用及规范标准 ,设想了数字图书馆应当建设的一些数据库 ,拟出了国家支持建立无偿数据库的思路和行业自行建立有偿数据库的思路     

新型的门禁系统结构的设计

在屏弃了传统的通讯单一化,或者无网络单点刷卡门禁系统结构的同时,将射频网络、GSM网络及以太网引入到了门禁系统中,形成了2级网络结构,极大的增强了系统的适应性,提高了性价比。初级网络采用资源丰富的ATMEGA128L作为主控器,次级网络由ATMEGA16L负责控制,并采用了自动请求重传机制,保证通讯的可靠性。     

邓小平的实践与邓小平理论的形成

长期的革命实践中 ,邓小平树立了坚定不移的共产主义理想和信念 ,积累了丰富的治党治国治军经验 ,掌握了马克思主义的真谛。所有这一切 ,对于邓小平理论的形成产生了极其重大的影响     

Orbifold嵌入定理

证明了orbifold嵌入定理在高维的orbifold上成立，即对于一紧致复orbifold M，若其上有一个正定的线丛，则存在正整数N使得M可以拓扑嵌入到CPＮ.     

一类局部orbifold Gromov-Witten不变量的计算

Gromov-Witten不变量是研究辛几何、代数几何的重要工具.对于一般流形,它的Gromov-Witten不变量的计算则是一项艰巨的任务,现在常用的计算方式一是利用流形的退化及退化公式,一是利用局部化技巧,以及两种方法混合.本文作者利用维数分析和局部化技巧将所考虑的orbifold Calabi-Yau模型Ws={(x,y,z,w)×[p,q]∈C4 × P1 |x/z=w/y=p/q}/μr(1,-1,b,-b)上的3-点orbifold Gromov-Witten不变量的计算简化到一些特殊的不变量的计算,并计算了其中一类.     

Orbifold上的积分

Orbifold的研究源于SATAKE对V-manifold的讨论．作者通过orbifold在一点附近的性质导出了带边区域的定义，还具体的构造出orbifold上的外微分形式丛，最后证明了对orbifold上的紧支集外微分形式Stokes公式成立。     

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。