新环状势的狄拉克与薛定谔方程束缚态解

本文提出了一种新的环状非球谐振子势V(r,θ)=K/2r2+A/r2+β/(r2sin2θ)+(γcos2θ)/(r2sin2θ.在标量势与矢量势相等的条件下,给出了Dirac方程和薛定谔方程的束缚态波函数解u(β′r)=1/Γ(L+3/2)(√2β′·Γ(Nr+L+3/2))/(nr!)·(β′r)(L+1),e(B...     

非球谐环形振子势的Schrdinger方程的解析解

量子力学中除了无限深势阱、一维线性谐振子、库仑势和三维各向同性谐振子势外,绝大部分Schrdinger方程是没有精确解的,这给具体问题的深入研究带来了很大的障碍。本文从求解Schrdinger方程的NU Method方法出发,求解了非球谐环形振子势V(r,θ)=μω2r2/2 h-2α/(2μr2) -h2βcosθ/(2μr2sin2θ)的本征方程的角向方程,获得解析解,将求解的过程大大简化;同时用特殊函数的方法求解了非球谐环形振子势的Schrdinger方程的径向方程,借以拓宽对Schrdinger方程求解方法的研究。     

非球谐环形振子势的Schrdinger方程的解析解

量子力学中除了无限深势阱、一维线性谐振子、库仑势和三维各向同性谐振子势外，绝大部分Schrodinger方程是没有精确解的，这给具体问题的深入研究带来了很大的障碍。本文从求解Schrodinger方程的NU Method方法出发，求解了非球谐环形振子势V（r，θ）=μω^2r^2／2＋h^2α／（2μr^2）＋h^2βcosθ／（2μr^2sinθ）的本征方程的角向方程，获得解析解，将求解的过程大大简化；同时用特殊函数的方法求解了非球谐环形振子势的Schodinger方程的径向方程，借以拓宽对Schrodinger方程求解方法的研究。     

Asymptotic Approximations of Jacobi Polynomials and Their Zeros with Error Bounds

IntroductionUniform asymptotic expansions and error boundsof the (α,β>- 1 ) two- term approximations of theJacobi polynomials P(α,β)n ( cosθ) were obtained[1] .Their result wassin θ2α cosθ2βP(α,β)n ( cosθ) =Γ( n +α + 1 )n!θsinθ1/ 2 Jα( Nθ)Nα +θB0 (θ) Jα+1( Nθ)Nα+1+σ2 ,|σ2 |≤ E2 θ2 +αN -2 ,　 0≤θ≤ π2 ,where E2 is a construct.Baratella and Gatteschiused the first two terms of this expansion[2 ] toconstructa more accurate one- term approximation:x(θ)x′(θ)…     

用阿基米德滚刀加工渐开线齿形的原理误差计算

分析了阿基米德滚刀加工渐开线齿形的原理误差,推导出滚刀切削刃连续位置的包络线方程及齿形误差的计算式:θ=(nβ)/(Hcos αcos λ)r2sin2α+2r2ha+ha2-((ρnβ)/(Hcos αcos λ))2-1+cos-1((H)/(ρnβ)cos αcos λ)-α△fF=ρ{[(1)/(cos α)((nβ)/(Hcos λ)-(1)/(r2))r22sin2α+2r2ha+ha2]-[((ρnβ)/(Hcos αcos λ))2-1-((ρ)/(r2cos α))2-1]+[cos-1((H)/(ρnβ)cos αcos λ)-cos-1((r2cos α)/(ρ))]}所用的方法,也可用于其它齿形的范成法.     

具第二类Chebyshev节点的拟和扩充Hermite-Fejer插值算子的逼近度

设U_n(x)=(sin(n 1)θ)/(sinθ)(x=cosθ)是第二类Chebyshev多项式,b_k=b_k~(n)=cos((kπ)/(n 1))(k=1,2,……n)是U_n(x)的零点,以{-1,b_1……,b_n,1}为基点的2n 1次拟Hermite-Fejer插值多项式是     

调幅波平均功率的讨论

本文通过积分证明了调幅波 u(t)=V_0.(1+m_a cos(aπ)/(T_n)t)cos((2π)/(T_0))t的平均功率P_调=(V_0~2)/(2R_1)(1+(1/2)m~2).指出了文献[3]中的错误之处.最后,用帕斯瓦尔定理对调幅波的平均功率做了进一步的简明解释.     

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))     

締合勒让德函数的展开及公式P_l~m(cosθ)=(-1)~m(l+m)!/(l-m)!P_l~(-m)(cosθ)的直接証明

在量子力学中讨论有心力场时,一开始就要遇到球谐函数Y_l,m的归一化问题。解决的办法这一涉及要证明P_l~m(cosθ)=(-1)~ml[(l+m)!/(l-m)!]P_l~(-m)(cosθ)这一公式。由于P_l~m(cosθ)与P_l~(-m)(cosθ)完全用cosθ表示时,很难进行展开,因而不能将二者直接比较。故一般对上述公式的证明都不采用展开比较的办法。作者在教学中常遇到同学们希     

缔合勒让德函数的展开及公式P_l~m(cosθ)=(-1)~m((l+m)！/(l-m！))-P_l~(-m)(cosθ)的直接证明

在量子力学中讨论有心力场时,一开始就要遇到球谐函数Y_l,m的归一化问题。解决的办法之一涉及要证明P_l~m(cosθ)=(-1)~m((l+m)!/(l-m!))-P_l~(-m)(cosθ)这一公式。由于P_l~m(cosθ)与P_l~(-m)(cosθ)完全用cosθ表示时,很难进行展开,因而不能将二者直接比较。故一般对上述公式的证明都不采用展开比较的办法。作者在教学中常遇到同学们希     

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.