关于带权Hardy不等式

本文得到了Hardy算子Tf(x)=integral from n=0 to z(f(t)dt)从空间L~p(R+,vdx)到L~q(R+,Udx)有界的权函数对(u,v)的特征,其中1≤q相似文献   

关于第二积分中值定理

在数学分析中第二积分中值定理的基本形式是: 定理1 设f(x)在〔a,b〕(a〈b)上单调下降(即使广义的也可以),并且非负,则对〔a,b〕上的任意可积函数g(x),有integral from n=a to b (f(x)g(x)dx)=f(a) integral from n=a to b (g(x)dx) (1)其中ξ∈〔a,b〕。其证明可参见〔1〕、〔2〕、〔3〕。定理1仅告诉我们其中的ξ∈〔a,b〕,那么能否恰当地选取ξ,使之属于开的区间(a,b)呢?我们说,不一定!且看下面的例题。考虑〔0,(3/2)π〕上函数 f(x)=1与g(x)=cosx,显然它们满足定理1的条件,于是按照定理1,(1)式应该成立。然而     

介于欧拉和雅可比的一个结论

设Q(q)=multiply from n=1 to ∞((1-q~n)(|q|<1))欧拉的五边形数定理为 Q(q)=sum from n=0 to ∞((-1)~nq~(n(3n+1))/2)(1-q~(2n+1))雅可比得到Q(q)~3=sum from n=0 to ∞((-1)~n(2n+1)q~(n+1)/2)本文得到Q(q)~2=sum from n=0 to ∞((-1)~nq~(n(n+1)/2)(1-q~(2n+2))p_n(q))其中p_n~h(q)=sum from r=0 to n(q~r(n-r)) 证明:由[1;p.36,eq.(3.3.6)] sum from j=0 to N((Q)_v/(q)_1(q)_(n-j)(-1)~iZ~iq~(j(j-1)/2))=(z)_N. (1)及[1;p.19,Cor.2.3.α=b=0,i=q,c=q~(2r+1)]     

Bochner-Riesz平均带权的强性求和

设f∈L~p(R~n),1≤p≤2(n+1)/n+3,以及δ>n/p-(n+1)/2.本文证明了f在R~n上的Bochner-Riesz平均σR(f;x)满足关系式其中权函数w满足条件w(u)≥0以及1≤1/t integral from 0 to t(w(u)du≤C)(C为一绝对常数)。结论对周期情形也成立。     

Riemann可积函数的一个性质

大家知道,如果f(x)在〔a,b〕上非负连续且integral from a to b(f(x)dx=0),则f(x)在〔a,b〕上恒等于0.但若把条件减弱为“f(x)在〔a.b〕上非负可积且integral from a to ∞b(f(x)dx=0)”,是否还能作出“在〔a,b〕     

积分第一中值定理的一个简明的证明

本学报1979年第2期刊登了绍文同志《关于积分第一中值定理》一篇文篇,作者给出了定理的证明。本文就C∈(a,b)的问题再给出一个较为简明的证明,并给一个例子,说明连续的条件是必要的,即若f(x)在〔a,b〕上不连续时,则结论不再成立。这个定理是这样叙述的: 积分第一中值定理设在区间〔a,b〕上f(x)与g(x)都可积,且g(x)不变号,m≤f(x)≤M,则存在μ,m≤μ≤M,使下式成立 integral from n=a to b(f(x)g(x)dx)=μintegral from n=a to b(g(x)dx) (1)如果f(x)在〔a,b〕上连续,则可进一步证明,存在C∈(a,b),使 (?) (2) 为了叙述上的完整起见,把前一部分的证明也写上。证明:先证前一部分。由f(x)与g(x)在区间〔a,b〕上的可积性知(1)式左端的积分是存     

关于一些Hermite-Fejer算子逼近度的注记

本文研究以Jacobi多项式的J_n(x)=sin(2n+1)/2θ/sinθ/2(x=cosθ,0≤θ≤π)的零点为基点的Hermite-Fejer插值过程H_(2n-1)(f,x).对于Lipα(0<α<1)类中函数,改进了[1]的结果:得到了H_(2n-1)(f,x)逼近有界变差函数的阶估计. 设函数f(x)∈C〔-1,1〕,x=cosθ(0≤θ≤π),J_n(x)是n阶Jacobi多项式,x_k=x_k~(n)=cosθk=cos(2kπ)/(2n+1)(k=1,2,…,n)是J_n(x)的零点,以{x_1,x_2,…,x_n}为基点的Hermite-Fejer插值算子是(见文〔1〕(4))     

二阶线性常微分方程张力样条配置解的渐近表示及其外推

设u″(x)+p(x)u′(x)+q(x)u(x)=f(x) a≤x≤bu(a)=u_a u(b)=u_b (1)其中p(x),q(x)∈c~3[a,b],f(x)∈c~3[a,b],q(x)≤q_0<0或q(x)≥q_1>0,由常微分方程基本理论知存在唯一的u(x)∈c~5[a,b]满足(1).又设△是[a,b]的一个等距分划     

关于函数项级数的积分定理

文献〔1〕中对其中 f(x)为冪级数,即 f(x)=sum from n=0 to ∞(C_nx~n) ,在2≤ω<3(C_n 终规为正),ω=2(C_n 可正可负)和 f(x)为勒让特(切比晓夫)级数,f(x)=sun from n=0 to ∞(C_nP_n(x)在1≤ω<2(C_n 终规为正)情形下的存在性分别作了讨论。本文推广了文献〔1〕中的定理。     

一个二阶拟线性椭园型方程定解问题的奇摄动

我们考虑如下含有小参数的二阶拟线性椭园型方程的定解问题:L_ε〔w〕≡ε(■~2w)/(■y~2)+(■~2w)/(■x~2)-a(y)(■w)/(■y)+b(x,y,w)=0(1)〔(■w)/(■x)+λ_i(y)w〕x=σ_i(y)=(?)_i(y),(i=1,2)(2)w丨_(y=0)=(?)_1(x)(3)((?)w)/((?)y)_(y=1)=(?)_2(x)(4)其中0<ε《1,σ_1(y)<α<β<σ_2(y),σ_1(y),σ_2(y)在〔01〕上适当光滑,使得区域Ω={(x,y)丨σ_1≤x≤σ_2,0≤y≤1}在边界σ_1(y),σ_2(y)上每点满足内部球条件〔5〕。(-1)~iλ(y)>0,(?)_i(y)及(?)_i(x)均为它们所定义的那段边界上的连续可微函数,α(y)>0,b(x,     

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.     

《Chinese Science Bulletin》SUBJECT INDEX TO VOLUME 59(2014)

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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