标量张量暴胀宇宙学

推广的引力理论 ( generalized gravity theory)早就被用来建立拓广暴胀模型 ( extend inflationarymodel) .不过 ,引力的基本理论仍然是 Einstein的广义相对论 ,推广的引力理论只是用来改变引力常数 G的值 ,以调节宇宙膨胀的速度而解决优良出口问题 .我们的标量张量暴胀宇宙学则是以标量张量引力理论为基础 ,并且以引力标量场ψ作为暴胀场 ( inflaton)来建立暴胀宇宙模型 .我们所用的作用量为 :A =∫d4x - g[-ψR - ωψ ψ .ψ - 2ψλ(ψ) - Γ ( u .ψ) 21 -ψ + 1 6πLm],其中 Lm为物质的拉氏密度 ,ψ .ψ≡ψ,σψ,σ,u .ψ≡ uμ…     

一种标——张量引力理论的引力波辐射

本文通过一种单位变换导出了文献[4]提出的标—张量引力理论方案的另一种表述形式,由此得到的引力场张量方程和守恒律完全类似广义相对论的Einstein方程和守恒律;变换后的标量场视为“物质场”,在张量方程中起着一种“引力源”的作用。应用变换后的理论表述研究引力辐射问题,其结果是引力场的总辐射强度为引力张量场和引力标量场的辐射强度之和。求出了引力张量场和引力标量场的辐射强度公式,详细地讨论了双星的引力波辐射。     

旋量算法及其应用

介绍了旋量算法技术及其应用.这个技术与螺旋度振幅、色分解、对偶性、KLT关系等技术相结合,可以在微扰论的树图和圈图水平上,对非阿贝尔规范理论、超对称、弦理论及引力-规范理论对偶等方面的研究发挥重要作用.     

狄拉克旋量场的二重化及其与二重复阿西特卡引力场的耦合

将二重复函数理论运用阿西特卡自对遇引力理论,通过引入二重时空流形,二重γ矩阵以及二重狄拉克旋量,将狄拉克旋量场的作用量二重化,进而研究狄拉克旋量场与阿持卡引力场的二重耦合问题,得到二重自对偶耦合作用量,并且能用它统一地描述罗伦兹引力和欧几里德引力。     

引力场方程的新标架形式及定域化的引力场能量动量张量

本文通过引入标架空间定叉了引力场场强张量和引力场拉格朗日密度,根据最小作用量原理导出了引力场运动方程的一种新的半度规形式(或称标架形式)及具有标架空间和坐标空间的双重协变的引力场能量动量张量.我们用这种定域化的能量表达式和球对称真空外部场席瓦兹希德解(当β1+β2=0,B3=0时)计算出在r≥R区域中的球对称引力场的总能量为E=MC2 1-√1-2GM/C2R/1+√1-2GM/C2R.它把爱因斯坦引力理论作为一个特例(满足条件β1=β2=β3=0)包含其中,是对爱因斯坦度规引力理论的重大发展.本文通过求解球对称真空外部场解得到以下结论:满足条件β1+β2=0,β3=0时的球对称真空外部场解就是席瓦兹希德外部解,基于球对称真空外部场解的任何检验Einstein引力场方程的实验验证都无法确定Einstein引力场方程是唯一正确的.最后根据粒子在引力场中的运动方程确定了待定常数的值为β1=2β,β2=β3=0.本文得到的引力理论与平移引力理论具有相同的形式.本文建立的引力理论采用的几何是黎曼几何,没有采用平移引力理论中的weitzenbock几何,并且对其中的能量问题和待定常数问题作了更深入的讨论.     

一种新的标量—张量引力理论

本文提出了一种新的标量-张量引力理论.在弱场近似中,得到与Fujii模同样的一种Yukawa型的中程引力,这一理论完全是经典的.     

爱因斯坦引力理论和狄拉克电子理论之间的矛盾

本文通过联合考虑爱因斯坦引力理论和狄拉克电子理论,发现在爱因斯坦引力理论和狄拉克电子理论之间关于电子场的能量动量运动存在着一个矛盾。这个矛盾表明爱因斯坦引力理论不能描述带半整数自旋的粒子的引力作用。如果假设狄拉克电子理论是正确的,我们必须修改爱因斯坦引力理论。     

从Poincaré丛及其配丛作用量得到的引力规范场方程

对Poincars仿射标架丛P(M)及其配丛E提供的作用量.应用变分原理.得到一种属Poinca引力(PG)的引力规范场方程,即与文献得到推广的Einstein—杨振宁方程类似的但属PG的另一种推广的Einstein—杨振宁方程.     

变化的引力常数G和行星轨道运动

变化的引力常数Ｇ引起对牛顿万有引力定律的修改．计算角速度和轨道半径的相对时变率．结果与引力协变理论相一致．     

Riemann－CartanR＋R~2引力场方程和能量动量张量

给出一有挠Ｒ＋Ｒ２型引力理论的Ｅｉｎｓｔｅｉｎ方程和Ｃａｒｔａｎ方程．由广义位移交换下引力场作用量的不变性导出能量动量的协变守恒律，并求得了引力场的能量动量张量和超势．     

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.