多元向量值小波包的正交公式

引入对应于多元向量值正交尺度函数的多元向量值小波包的定义,运用代数学理论和积分变换进一步研究多元向量值小波包的性质,得到多元向量值小波包的一个新的正交公式.     

紧支撑多元向量值小波包的正交性

给出数量矩阵mIr(2≤m∈Z)伸缩的多元向量值小波包的定义及其构造方法.运用代数学理论,算子理论与时频分析方法,讨论多元向量值小波包的正交性,得到多元向量值小波包的正交公式.     

紧支撑向量值双正交小波包

研究向量值双正交小波包,给出一类紧支撑向量值双正交小波包的定义及其构造方法.讨论了这种向量值双正交小波包的性质.     

扩展矩阵伸缩的多元向量值双正交小波包

给出扩展矩阵伸缩的多元向量值双正交小波包的定义及其构造方法.运用积分变换与算子理论,讨论了它们的性质,得到了多元向量值小波包的双正交公式.     

具有整数伸缩因子的向量值正交小波的构建算法与性质

引进多尺度向量值正交小波与向量值小波包的概念.运用仿酉向量滤波器理论和矩阵理论,给出多尺度向量值正交小波存在的充要条件.提供紧支撑向量值正交的构建算法,给出相应的构建算例.利用时频分析方法与算子理论,刻画一类向量值正交小波包的性质.得到向量值小波包的正交公式.构造向量值函数空间L2 (R,Cn)的规范正交基.     

一类高维向量值双正交小波包

研究高维向量值双正交小波包的构造及性质.引进一类紧支撑高维向量值双正交小波包的概念.运用傅立叶变换、积分变换和算子理论,讨论了这种向量值双正交小波包的性质.     

矩阵伸缩的二元向量值双正交小波包

研究二元向量值双正交小波包的构造及性质.引进二元向量值双正交小波包的概念.运用时频分析方法,讨论它们的性质,得到向量值小波包的双正交公式与向量值函数空间的Riesz基.     

高维向量值正交小波包的性质

研究了高维向量值小波包的构造与性质,引进了数量矩阵伸缩的高维向量值小波包的概念.运用有限群理论和算子理论与积分变换,讨论了它们的性质,得到了高维向量值小波包的正交公式.利用高维向量值小波包的正交性,构造了空间L2(Rs,Cr)的新的正交基.     

一类多元双正交向量值小波包的构造

文章研究了一类多元双正交向量值小波包的构造及其性质。     

一类多重向量值双正交小波包的刻划

 研究向量值小波包.给出一类3尺度多重向量值双正交小波包的定义及构造.运用积分理论与算子理论,刻划了多重向量值双正交小波包的特征,得到多重向量值小波包的双正交公式.进而,得到向量值函数空间L²R,C^s×s)新的Riesz基.     

二元m带多重向量值双正交小波包的性质

给出二元多重向量值双正交小波包的定义及其构造方法.运用矩阵理论、积分变换与算子理论,讨论了热热二元m带多重向量值双正交小波包的性质,得到向量值函数空间L2(R2,Cn)的一个新的基底.     

Hardy空间上向量值极大算子的加权有界性

利用Hardy空间上的原子分解和Cauchy不等式证明了向量值极大算子在Hardy空间上的有界性,并推广到向量值极大算子的加权情形。     

向量值可测函数的连续性

本文给出了向量值可测函数等价类〔f〕的连续和弱连续的定义,并得到如下结果:如果〔f〕在〔a,b〕(?)R上(弱)连续,则必存在且唯一的g∈〔f〕使得g是〔a,b〕上的(弱)连续函数。以上定义及结论是A.C.Zaanen在文〔1〕中相应部分的推广。     

向量极小极大定理

本文在没有线性结构的G-凸空间(定义见后)上讨论向量极小极大定理．在G-凸空间上引进向量映射的真拟凸性概念，推广Ky Fan极小极大不等式、Li与Wang等的主要结果．     

算子空间L（lp,X）和K（lp,X）的序列弱完备性

建立了连续线性算子空间Ｌ（ｌｐ，Ｘ）及紧算子空间Ｋ（ｌｐ，Ｘ）和矢值序列空间ｌｐ〔Ｘ〕之间的等距同构关系。通过此关系，给出了算子空间Ｌ（ｌｐ，Ｘ）和Ｋ（ｌｐ，Ｘ）（１〈ｐ〈∞）是序列弱完备空间的特征。     

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.     

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…     

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。     

On Tragic Consciousness In The Works By Ernest Hemingway

As an American modern novelist who were famous in the literary world, Hemingway was not a person who always followed the trend but a sharp observer. At the same time, he was a tragedy maestro, he paid great attention on existence, fate and end-result. The dramatis personae's tragedy of his works was an extreme limit by all means tragedy on the meaning of fearless challenge that failed. The beauty of tragedy was not produced on the destruction of life, but now this kind of value was in the impact activity. They performed for the reader about the tragedy on challenging for the limit and the death.