有穷下级整函数的奇异方向

对于λ(0<λ<∞)级整函数f(z),杨乐、张广厚获得:若f(z)的Borel方向总数q有穷。则f(z)的有穷亏值总数P<2λ。本文类似[1]的证明方法得到:整函数f(z)的下级μ有穷,设q为f(z)至少μ级Borel方向总数,若q<+∞,则f(z)的有穷亏值数p<2μ。其中f(z)至少μ级Borel方向指由原点发出的半直线B:argz-θ_0(0≤θ_0<2π),对于任意正数ε和每个复数a都有 (?)(logn(r,θ.,ε,f=a)/logr≥μ (*)至多除去两个例外的复数。     

具有有穷条Julia方向的整函数

本文主要证明了下述结论: 定理设f(z)是整函数,其下级μ(f)<,若f(z)仅有有穷条julia方向,则f(z)的Nevanlinna亏量在坐标平移下不变,即任取a∈C,z_0∈C,均有δ(a,f(z)=δ(a,f(z+z_0)).     

亚纯函数及其导函数的渐近值

定理设f(z)是下级μ有穷的亚纯函数,P_i是f~((i))(z)的非零有穷亏值数,而f~((0))(z)=f(z);当i为负整数时,f~((i))(z)为f(z)的(i)次原函数(若存在的话)。若对某一正整数k, sum from n=a to δ(a,f~((k)))=2,和 sum from i=-∞ to ∞ P_i=μ。则f~((i))(z)(i=0,±1,±2,…)的所有有穷非零亏值都分别为它们的渐近值。     

具有极值亏量和的整函数

设 f(z)是一个下级为μ的整函数,记 f(z)的有穷亏值数目为 p,判别有穷渐近值数目为 l.本文证明了如下结果:假设 f(z)的亏量总和Δ(f)(?)=(a,f)=2,δ(a,f)>0,则有 p+l≤2μ.     

亚纯函数及其导函数的渐近值

定理设f(z)是下级μ有穷的亚纯函数,P_4是f~(i)(z)的非零有穷亏值数,而f~(0)(z)=f(z);当i为负整数时,f~(i)(z)为f(z)的(i)次原函数(若存在的话).若对某一正整数k, ??和?? 则f~((i))(z)(i=0,±1,±2,…)的所有有穷非零亏值都分别为它们的渐近值.     

亚纯函数及其各级导数的线性组合的辐角分布

本文考虑了亚纯函数结合其导数的线性组合涉及重值的辐角分布方面的问题,证明了: 定理 设f(z)是λ级亚纯函数,0<λ<∞,则存在一条由原点出发的半直线B:argz=θ_0(0≤θ_0≤2π),使得对于任意正数ε,一切有穷复数a与一切有穷非零复数b有;其中F(z)=a_0f~((m))(z)+a_1f~((m-1))(z)+…+a_m(f(z)(a_0≠0)而k,l是满足(m+1)/k+1/l<1的正整数。     

偶次幂为非拟素的有穷级素整函数的存在性

本文解决了[1]中提出的一个问题,即证明了:存在有穷级的素整函数F(z),使得E(z)~2是非拟素的。同时进一步证明:若F(z)是拟素的超越整函数,而F(z)~2可分解为F~2=f(g),这里f,g为超越整函数,则g(z)=cosα(z),以及F(z)=sinα(z)h(cosα(z)),这里α(z),h(w)是整函数。     

偶次幂为非拟素的有穷级素整函数的存在性

本文解决了[1]中提出的一个问题,即证明了:存在有穷级的素整函数F(z),使得可(z)~2是非拟素的。同时进一步证明:若F(z)是拟素的超越整函数,而F(z)~2可分解为F~2=f(g),这里f,g为超越整函数,则g(z)=cosα(z),以及F(z)=sinα(z)h(cogα(z)),这里α(z),h(w)是整函数。     

关于有穷级亏函数的Nevanlinna逆问题

本文证明了任给亚纯函数集合{a_j(z)}_j~N=1,N≤ ∞;若它的级有界,那么存在有穷级亚纯函数F(z)使{a_j(z)}_j~N=1是F(z)的亏函数序列。若{a_j(z)}_j~N=1是整函数序列,本文得到更好的结果。     

分担值和全纯函数族的正规性

应用Zalcman引理研究了与导数有分担值的全纯函数族的正规族,把分担值减弱为单项分担值,得到了如下的结论:设F是区域D内的一族全纯函数,a,b是非零有穷复数,若对于每个f(z)∈F,若F满足:(1)f(z)=0=f′(z)=a,f′(z)=a=f′′(z)=b则F在D内正规;(2)k≥2为一整数,b为一正数f(z)=0=f′(z)=a,f′(z)=a=f(k)(z)≤b则F在D内正规.     

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.     

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.     

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.