拟共形映照的双曲面积偏差

进一步研究拟共形映照f(z)=ρ(r,θ)eiφ(θ),z=reiθ,0相似文献   

拟共形映照的一个极值问题

本文证明:如果f(z)是拓广复平面到自身使得f(0)=0,f(1)=1和f(∞)=∞的一个Q拟共形映照。则对任何r,|z|≤r |f(z)|≤r,成立|f(z)-z|≤4/π rK(1/1+r)K(r/1+r)·logQ,其中K(t)=integral from n=0 to 1(dx/((1-x~2)(1-tx~2))~(1/2)。它是夏道行的一个定理的拓广。     

一个拟共形映照的极值问题

设f(z)是把|Z|<1映成|ω|<1的K-Q.C.,f(0)=0。对正整数n及实数θ,0<θ<(?),记(?),(?),有估值(?)当且仅当n=1时估值是准确的,     

一类单叶调和函数的拟共形性质

研究单位圆盘D={z||z|<1}上满足Re{αz［h″(z)+g″(z)］+h’(z)+g’(z)}>0,z∈D,α>0的单叶调和函数f(z)=h(z)+g(z)^-的拟共形性质,对复伸张w(z)=(g’(z))/(h’(z))的模给出最好的最小上界估计,进而给出该类函数到D的余集D^c上的拟共形延拓,并对其复伸张的模给出最好的最小上界估计,改进和推广了2004年Yalcin S等的研究成果.     

单叶调和函数的稳定性

对单叶调和函数f(z)=h(z) ■,z∈D={z||z|<1},研究F(z)=h(z) ■(|λ|<1)单叶性的稳定性问题,得出凸像调和拟共形映照以及一些单叶调和函数类具有稳定性.     

拟似共形映照的参数表示

§1 设 w=f(z)是单位圆|z|<1到|w|<1的 Q-拟似共形映照(限于保持定向的映照,定义见)而且适合就范化条件 f(0)=0,f(1)=1.这种映照的全体就做U_Q.设 p(z),θ(z)是单位圆上分布的一对特征,在本文中为方便起见引入一个复函数     

关于拟共形映照的一个偏离定理的证明

设w=f(z)是把|z|<1映照成|w|<1,且f(0)=0的k—拟共形映照,Mori定理表明,对这类拟共形映照,成立     

单位圆上K-拟共形映照的爆破性

在R.M.Porter和L.F.Resendis研究径向映照的爆破性的基础上,进一步研究单位圆到单位圆上的拟共形映照类具有形如f(z)=p(r,θ)eiφ(r,θ)的双曲面积问题,得到了此类拟共形映照为非爆破的条件,推广了已有的结果.     

单位圆上调和拟共形映照的复特征估计

设f(x)=exp[iγ(x)]为单位圆周D到自身上的保向同胚映照,w=P[f](z)是单位圆D到自身上的单叶调和函数,f(x)为边界值.研究边界函数f(x),得到Jw的一个良好估计.当w为调和拟共形映照时,对其复特征|w w|进行估计.     

Mori不等式的精确化

设W=f(z)是单位圆|z|<1到|W|<1的Q—拟似共形是映照,且f(0)=0,f(1)=1。这种映照的全体记为U_Q,对于U_Q中任一f(z)有著名的森(Mori)不等式 4~(-Q)|z|~Q<|f(z)|<4|z|~(1/Q)。 嗣后王传芳证明了     

关于拟共形映照的几个偏差定理

本文利用模估计的方法，通过对Ｋ—Ｑ、Ｃ、映射性质的研究，得出了关于Ｓ_Ｋ，Ｓ′_Ｋ，∑_Ｋ，∑′_Ｋ族函数的一些结果。     

关于Riemann流形的某些整体性质

本文运用拟共形曲率张量研究了Riemann流形上调和P—形式与Killing P—形式的不存在性,给出了拟共形平坦流形和拟常曲率流形上不存在非零调和P—形式与Kill-lug P—形式的条件.它们分别是K Yano,Bochner,Goldberg等相应结果的有趣推广.     

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.     

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.     

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.     

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。     

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.