两参数混合型S.D.E 解的性质

设 M={Mz,Z∈R2 },A分别是两参数连续鞅和适应增过程,Y={Yz,Z∈R2 },为Poisson单,∧是Y的特征测度且N=Y-∧. 本文考虑如下混合型S.D.E: X2=X0 ∫R2f1(ξ,Xξ)dMξ ∫R2f2(ξ,Xξ)dAξ ∫Rzf3(ξ,Xξ)dNξ ∫Rzf4(ξ,Xξ)∧(dξ)其中z∈R2 .在方程系数fi,i=1,2,3,4满足一定假设条件下,得到了方程解的性质.     

多自由度振动系统的同相振动性

采用反射函数法研究了多自由度振动系统x′=p(t)x, 当p(t)=diag(A(t),B(t))时,给出其等价系统y′=A(t)y, z′=B(t)z同相振动的充分必要条件,其中A(t)=(aij(t))2×2, B(t)=(bij(t))2×2, y=(y1,y2)T, z=(z1,z2)T, p(t+2ω)=p(t), ω>0, t∈R, x∈R4, p(t)为连续可微的矩阵函数.     

Villat公式的两个简单证明及其在n连通圆界区域内的推广

本文利用Schwarz积分和Poisson积分的性质及核函数的下列表示式: K_1(z,ξ_1)=(ξ_1 z)/(ξ_1-z) sum from k=1 to ∞ ((ξ_1 q~(2k)z)/(ξ_1-q~(2k)z) (ξ_1 q(-2k)z/(ξ_1-q~(-2k)z)),ξ_1=e~(iθ) K_2(z,ξ_2)=(ξ_2 z)/(ξ_2-z)-sum from k=1 to ∞ ((ξ_2 q~(2k)z)/(ξ_2-q~(2k)z) (ξ_2 q(-2k)z/(ξ_2-q~(-2k)z)),ξ_2=qe~(iθ) 给出圆环内解析函数的Villat公式的两个十分简单的证明。并进而把它推广到任意有限连通的圆界区域中去。后一结果此“美国数学评论”34卷＃6047(1967)介绍的Dunducenko的结果要早,我们的工作完成于1964年。     

随机单调条件下带Poisson跳的倒向随机微分方程解的存在唯一性

讨论了带跳的BSDE:Yt=ξ ∫Ttf(s,Ys,Zs)ds-∫TtZsdMs,0≤t≤T,其中驱动过程Mt=(Wt,Qt)T,Wt=(W1(t),W2(t),…,Wr(t))是一个r维的标准Winner过程,令Nt=(N1(t),N2(t),…,Nd-r(t))T是一族相互独立的Poisson过程,且W和N相互独立,λ=(λ1,λ2,…,λd-r)T为其参数,定义Qt=(Q1(t),Q2(t),…,Qd-r(t))T为一族补偿Poisson过程,其中Qi(t)=λ-(1)/(2)i[Ni(t)-λit],0≤t≤T,i=1,2,…,d-r.通过构造函数逼近序列的方法,证明了飘移系数f关于y满足随机单调,关于z满足随机Lipschitz条件下,上述方程适应解的存在唯一性问题,并对文[9]中常系数线性增长条件作了改进.     

工业过程的数学模型由离散时间域向连续时间域的转换方法

工业过程在离散时间域上的数学模型HG(z)与其在连续时间域上的数学模型G(S)之间存在着如下的关系式: HG(z)=(1-z~(-1))z[G(S)/S]. 若由辨识所获得的HG(z)为和则与之对应的连续时间域上的数学模型为和文中所提出的各个公式可用来计算K、τ_d、τ、τ_1、τ_2、τ_0、ζ和T.     

亚纯函数及其线性微分多项式的唯一性

设f(z)是开平面上的亚纯函数,N(r,f)为f(z)在圆|z|≤r上极点的计数函数,m(r,f)为逼近函数.T(r,f)=m(r,f) N(r,f),T(r,f)称为f(z)的特征函数.F(z)=(fn)(z) a1(z)f(n-1)(z) … an(z)f(z)是f(z)的线性微分多项式,其中n是正整数,a1(z),a2(z),…,an(z)均是f(z)的小函数.研究f(z)和F(z)的唯一性问题.证明了:f(z)为满足N(r,f)≤1f(z)的两个相互判别的小函数,若f(z)和F(x)几乎CM分担a(z)和b(z),则f(z)≡F(z).     

推广后的复合Poisson-Geometric过程的风险模型下的破产概率

对索赔到达为复合Poisson-Geometric过程的风险模型进行了推广,考虑保单到达为参数α的Poisson过程,运用鞅论的方法得出了破产概率满足的Lundberg不等式和一般公式．     

关于P叶函数的一个子类

本文利用Rusheweyh导数引进函数类T(α+p—1,β)={f(z)|f(z)∈A(p),Re(D~(α+p)f)/(D~(α+p-1)f>β}。当0≤β≤1/2时,证明了T(α+p,β)(?)T(α+p-1,β)。还讨论了由积分算子定义的函数F(z)=(p+c)·z~(-(?))integral from n=0 to z t~((?)-1)f(t)dt,(|z|<1)的映射性质。推广了某些文献中的一些结果。     

关于丢番图方程Ax4+Bx2y2+Cy4=z2的解

证明了丢番图方程4x4-6x2y2 3y4=z2,(x,y)=1的全部正整数解为(x,y,z)=(x0／2,ab,(3a4 b4)／4), (Xn,2yn,2zn),认为仅有正整数解(x,y,z)=(1,1,1)是不妥的,它漏掉了(xn,2yn,2zn)及(x0／2,ab,(3a4 b4)／ 4);丢番图方程x4-6x2y2 12y4=z2,(x,y)=1的全部正整数解为(x,y,z)=(x0,ab,(3a4 b4)／2),(xn,yn, zn),认为仅有正整数解(xn,yn,zn),则漏掉了(x0,ab,(3a4 b4)／2)。     

二阶线性周期微分方程的解和小函数的关系

研究了二阶线性周期微分方程$f^{\prime\prime}+[P_1(e^{z})+P_2(e^{-z})]f^{\prime}+[Q_1(e^{z})+Q_2(e^{-z})]f=0$和$f^{\prime\prime}+[P_1(e^{z})+P_2(e^{-z})]f^{\prime}+[Q_1(e^{z})+Q_2(e^{-z})]f=R_1(e^{z})+R_2(e^{-z})$的解以及它们的一阶导数、二阶导数、微分多项式与小函数之间的关系, 其中$P_j(z)$和$Q_j(z)$及$R_j(z)$(j=1,2)是关于z的多项式.     

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.     

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.     

A computer generator for randomly layered structures

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

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.     

Achieving Unusual States of Matter Under High Pressure

正The periodicity of the elements and the non-reactivity of the inner-shell electrons are two related principles of chemistry,rooted in the atomic shell structure.Within compounds,Group I elements,for example,invariably assume the+1 oxidation state,and their chemical properties differ completely from those of the p-block elements.These general rules govern our understanding of chemical structures and reactions.Using first principles calcula-     

Exchange-Correlation and Electronic Excitation Energies from Pairing Matrix Fluctuations

We have developed an adiabatic connection to formulate the ground-state exchange-correlation energy in terms of pairing matrix linear fluctuations.This formulation of the exchange-correlation energy opens a new channel for density functional approximations based on the many-body perturbation theory.We illustrate the potential of such approaches with an approximation based on the particle-particle Random Phase Approximation(pp-RPA).This re-     

Density Functional Theory for the Response of Periodic Systems to Electric Fields Based on the Vector Potential Approach

正The electronic and nuclear(structural/vibrational)response of 1D-3D nanoscale systems to electric fields gives rise to a host of optical,mechanical,spectral,etc.properties that are of high theoretical and applied interest.Due to the computational difficulty of treating such large systems it is convenient to model them as infinite and periodic(at least,in first approximation).The fundamental theoretical/computational problem in doing so is that     

On the Thermodynamic Limit for Responses to Static Electromagnetic Fields

For molecular systems,the quantum-mechanical treatment of their responses to static electromagnetic fields usually employs a scalar-potential treatment of the electric field and a vector-potential treatment of the magnetic field.Although the potential for each field separately is associated with the choice of an(unphysical)origin,the precise choice of the origin for the electrostatic field has little consequences for the results.This is different for the