投射群环

设R是一个环,G是一个有限群,本文定义了一个R上带因子组f的投射群环RG_f,证明了如果RG_f是R的Galois扩张带由G导出的内Galois群G,使得R的中心C是R的C-直和项,则CG_f是C上中心Galois代数;还将F.R.DeMeyer关于Azumaya投射群代数的刻划推广到投射群环RG_f。     

关于Galois扩张理论中F.R.DeMeyer的一个定理

本文证明了Galois 扩张理论中F.R.DeMeyer 的一个定理的逆定理;并从证明的过程中可见,条件R~G 在C~G上是Azumaya 的可以换为交叉积Δ(R,G)在C~G 上是Azumaya 的.另外,还获得了C[U_1,…,U_n]的可分子代数的某种结构,这里的{U_i}是Δ(R,G)的标准自由基。     

交叉积的中心与环的Galois扩张

本文对交换环R 与其自同构群G 的交叉积Δ(R,G)的中心的元素,给出一个具体的表示形式,然后在Δ(R,G)是可分的(?)一代数的假设下(R~G 是G 的不动环),给出Galois 扩张的一个判别准则;还对R 对G 的中心的元素的幂等Galois 扩张进行讨论,并取得了一些结果.     

F.C群在任意环上的局部群环

给出了F.C群在任意环上的群环成为局部环的充分与必要条件,即证明了若G是F.C群,则群环R[G]是局部环当且仅当R是局部环,G是局部有限P-群且p∈J(R),其中J(R)是环R的Jacobson根.此结果推广了W.K.Nicholson关于Abel群的群环的相应结论.     

子群c-正规性对群结构的影响

群G的一个子群H称为在G中c-正规，如果存在一个正规子群K，使得G＝HK且H∩G≤HG，其中HG＝CoreG(H)=∩x∈GH^x是包含在H中的G的最大正规子群。该文利用子群c－正规性给出一个群为可群解的一些条件，主要定理有：1）设G为群， 若存在P∈Syl2（G），P为c－正规于G，则G可解；2）设N为群G的非单位正规子群，则N可解当且仅当G的任意不包含N物极大子群M为c－正规于G。     

*-代数上强保持新积的映射

设R是有单位元的*-代数,若R包含非平凡对称幂等元P满足:(1)若ARP={0},则A=0;(2)若AR(I-P)={0},则A=0。设φ:R→R是满射,则φ强保持新积当且仅当存在Z∈Z_S(R)且Z²=I,使得对所有X∈R, 有φ(X)=ZX。作为应用,在没有I₁型的中心直和项的von Neumann代数上和素*-环上得到相似的结果。     

关于顺从Banach代数

1.引言 Johnson([3])引入了顺从Banach代数.证明了群代数L′(G)是顺从的当且公当G是顺从的,其中G是一个拓扑群。J.W.Bunce([7]、[8])给出了顺从C(?)—代数的特征描述: 设A是一个具单位元的C(?)代数,则下面三个命题等价: (a)A是顺从的 (b)存在一个线性算子T:(AA)→C={f∈(AA):af=fa,(?) a∈A}使得T在C上的限制是单位映射,且T(aof)=aoT(f),T(foa)=T(f)·a     

因子von Neumann代数上ξ-*-Lie同构的特征

设H和K是复Hilbert空间,A和B分别是H和K上的维数大于1的因子von Neumann代数。设Φ:A→B是双射且满足条件Φ(A*B-ξB*A)=Φ(A)*Φ(B)-ξΦ(B)*Φ(A),?A、B∈A。证明了以下三个结论:(1)当ξ=0时,Φ是线性或共轭线性*-同构;(2)当ξ∈R/{0,1,-1}时,若Φ保单位元,则Φ是线性或共轭线性*-同构;(3)当ξ∈C/R,若Φ保单位元,则Φ是线性*-同构。     

一类算子的换位代数的K-群

Hilbert空间X上的有界线性算子K称为紧算子,若K(B1)的闭包—↑K（B1）在X中是紧集,其中B1是X中的单位球,得到了若X上的有界线性算子S的换位代数d′(S)=CI R,(其中：C是复数域;I是R上的单位算子;R是所有与S可交换的对角线为0的紧上三角有界线性算子的集合),则K0(d′(S))同构于整数群Z。     

强π-正则斜群环的一些性质

设R是有单位元的结合环.设x∈R,若存在y∈R和正整数n,使得x~n=yx~(n+2)(x~n=x~(n+1)y),则称x是左(右)π-正则元.如果x既是左π-正则元又是右π-正则元,则称x是强π-正则元.若环R中的每一个元素都是强π-正则元,则称R是强π-正则环.给出了R*_θG是强π-正则的充分或必要条件,其中θ是群G到由R的自同构所构成的群Aut(R)的群同态.     

Markedness and its Interpretation in Language Use

Language markedness is a common phenomenon in languages, and is reflected from hearing, vision and sense, i.e. the variation in the three aspects such as phonology, morphology and semantics. This paper focuses on the interpretation of markedness in language use following the three perspectives, i.e. pragmatic interpretation, psychological interpretation and cognitive interpretation, with an aim to define the function of markedness.     

Lower Paleozoic oil relationships within Williston Basin, Canada

The Williston Basin is a significant petroleum province, containing oil production zones that include the Middle Cambrian to Lower Ordovician, Upper Ordovician, Middle Devonian, Upper Devonian and Mississippian and within the Jurassic and Cretaceous. The oils of the Williston Basin exhibit a wide range of geochemical characteristics defined as "oil families", although the geochemical signature of the Cambrian Deadwood Formation and Lower Ordovician Winnipeg reservoired oils does not match any "oil family". Despite their close stratigraphic proximity, it is evident that the oils of the Lower Palaeozoic within the Williston Basin are distinct. This suggests the presence of a new "oil family" within the Williston Basin. Diagnostic geochemical signatures occur in the gasoline range chromatograms, within saturate fraction gas chromatograms and biomarker fingerprints. However, some of the established criteria and cross-plots that are currently used to segregate oils into distinct genetic families within the basin do not always meet with success, particularly when applied to the Lower Palaeozoic oils of the Deadwood and Winnipeg Formation.     

An Analysis of Catherine＇s Character——Wuthering Heights

Wuthering Heights, Emily Bronte＇s only novel, was published in December of 1847 under the pseudonym Ellis Bell. The book did not gain immediate success, but it is now thought one of the finest novels in the English language. Catherine is the key character of this masterpiece, because everybody and everything center on her though she had a short life. We can understand this masterpiece better if we know Catherine well.     

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.     

Features of Women's language

Language is a means of verbal communication. People use language to communicate with each other. In the society, no two speakers are exactly alike in the way of speaking. Some differences are due to age, gender, statue and personality. Above all, gender is one of the obvious reasons. The writer of this paper tries to describe the features of women＇s language from these perspectives： pronunciation, intonation, diction, subjects, grammar and discourse. From the discussion of the features of women＇s language, more attention should be paid to language use in social context. What＇s more, the linguistic phenomena in a speaking community can be understood more thoroughly.     

Design and analysis of generic LBS application developing platform

Location based services is promising due to its novel working style and contents.A software platform is proposed to provide application programs of typical location based services and support new applications developing efficiently. The analysis shows that this scheme is easy implemented, low cost and adapt to all kinds of mobile nework system.     

橡胶颗粒沥青混合料低温抗裂性试验研究

以AC-13级配为基础,将橡胶颗粒代替部分集料掺入混合料中,以低温弯曲试验为评价方法对不同橡胶颗粒掺量下沥青混合料的低温抗裂性进行研究,并引入应变能密度值对混合料的低温抗裂性进行综合评价.试验结果表明:橡胶颗粒沥青混合料试件的破坏微应变均超过2 300,满足冬寒区的技术指标;无论是否掺加橡胶颗粒,随着温度的下降,沥青混合料破坏时的最大弯拉强度增大,弯拉应变降低,劲度模量增大;弯曲应变能密度在胶粒掺量为1%左右时具有较大的弯曲应变能密度值,此时橡胶颗粒沥青混合料具有较好的低温抗裂性.     

A computer generator for randomly layered structures

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

低渗透非均质砂岩油藏启动压力梯度研究

理论推导与室内实验相结合,建立了低渗透非均质砂岩油藏启动压力梯度确定方法。首先借助油藏流场与电场相似的原理,推导了非均质砂岩油藏启动压力梯度计算公式。其次基于稳定流实验方法,建立了非均质砂岩油藏启动压力梯度测试方法。结果表明:低渗透非均质砂岩油藏的启动压力梯度确定遵循两个等效原则。平面非均质油藏的启动压力梯度等于各级渗透率段的启动压力梯度关于长度的加权平均;纵向非均质油藏的启动压力梯度等于各渗透率层的启动压力梯度关于渗透率与渗流面积乘积的加权平均。研究成果可用于有效指导低渗透非均质砂岩油藏的合理井距确定,促进该类油藏的高效开发。     

Quantitative trait loci （QTLs） for quality traits related to protein and starch in wheat

Quality traits in wheat （Triticum aestirum L.） were studied by quantitative trait locus （QTL） analysis in a recombinant inbred line （RIL） population, a set of 131 lines derived from Chuan 35050 × Shannong 483 cross （ChSh）. Grains from RILs were assayed for 21 quality traits related to protein and starch. A total of 35 putative QTLs for 19 traits with a single QTL explaining 7.99-40.52% of phenotypic variations were detected on 10 chromosomes, 1D, 2A, 2D, 3B, 3D, 5A, 6A, 6B, 6D, and 7B. The additive effects of 30 QTLs were positive, contributed by Chuan 35050, the remaining 5 QTLs were negative with the additive effect contributed by Shannong 483. For protein traits, 15 QTLs were obtained and most of them were located on chromosomes 1 D, 3B and 6D, while 20 QTLs for starch traits were detected and most of them were located on chromosomes 3D, 6B and 7B. Only 7 QTLs for protein and starch traits were co-located in three regions on chromosomes 1D, 2A and 2D. These protein and starch trait QTLs showed a distinct distribution pattern in certain regions and chromosomes. Twenty-two QTLs were clustered in 6 regions of 5 chromosomes. Two QTL clusters for protein traits were located on chromosomes 1D and 3B, respectively, three clusters for starch traits on chromosomes 3D, 6B and 7B, and one cluster including protein and starch traits on chromosome 1D.