容有m—维曲面族的QE（B^RP）流形的一些性质

本文拓广了ＱＥ流形，并研究了这类容有某种ｍ－维曲面族的Ｒｉｅｍａｎｎ流形的一些性质。进一步导出了在Ｒｉｃｃｉ对称及半对称条件下，这种拓广的ＱＥ流形为Ｅｉｎｓｔｅｉｎ或其法矢所满足的条件，以及一般情况下单位法矢为挠形场的必要条件。     

球面中子流形与特征P流形的谱间隙

给出了欧氏球面中子流形的两次Ｌａｐｌａｃｅ算子的谱间隙的一个新估计，同时讨论了特征Ｐ流形的两次Ｌａｐｌａｃｅ算子的谱间隙。     

Ricci曲率平行的黎曼流形的刚性定理

该文研究Ｒｉｃｃｉ曲率平行的黎曼流形，将文（６），（７）中Ｅｉｎｓｔｅｉｎ流形的一些刚性定理推广到Ｒｉｃｃｉ曲率平行的黎曼流形上。     

关于超曲面的几个结果

建立了黎曼流形中超曲面的Ｒｉｃｃｉ曲率和载面曲率之间的一个不等式，提到了用Ｒｉｃｃｉ曲率刻划的２个Ｐｉｎｃｈｉｎｇ定理。     

Riemannian流形上调和函数的一些注记

给出了高维旋转对称流形上Δｒ＝０的渐近Ｄｉｒｉｃｈｌｅｔ边值问题可解的一个曲率条件，且将Ｈａｒｄａｍａｒｄ三球定理推广到一般Ｒｉｅｍａｎｎｉａｎ流形上，并导出一个相应的Ｌｉｏｕｖｉｌｌｅ型结果，最后用Ｌ．Ｋａｒｐ的方法证明：在某个紧致集外满足曲率ｋ≥－１／ｒ＾２ｌｏｇｒ的二维流形上不存在有上界的非常值下调和函数。     

K(a)hler 流形上的典型线丛

讨论了Ｒｉｅｍａｎｎ流形上指标形式与共轭点的关系;证明了具非负Ｒｉｃｃｉ曲率的无共轭点Ｋａｈｌｅｒ流形上的典型线丛之曲率之零。     

Yamabe问题与紧致无边流形的第一特征值

根据Ｙａｍａｂｅ定理，任意ｎ维紧致无边黎曼流形（Ｍ，ｇ）上，存在共形度量ｇ，具有常数量曲率ｓｃａｌ（ｇ）。本文证明了这一流形上普拉斯算子的第一特征值满足λ１≥ｎＫ，     

具非负曲率的黎曼流形

利用沿测地线的Ｊａｃｏｂｉ场和指标形式，证明了具非负曲率的完备２维黎曼流形Ｍ＾２如果没有共轭点，必等距于Ｒ＾２。     

拟常曲率黎曼流形的紧致极小子流形

研究了拟常曲率黎曼流形中的紧致极小子流形问题，给出了Ｍ＾ｎ是全测地子流形的截面曲率不等式估计，推广了Ｓ．Ｔ．ａｕ研究的结果，并导出了有关数量曲率和Ｒｉｃｃ曲率的结论。     

关于对数Sobolev常数的估计

研究紧Ｒｉｅｍａｎｎ流形上可逆扩散过程对数Ｓｏｂｏｌｅｖ常数的估计，所获结果在一些有意义情形（特别是负曲率下界情形）优于Ｄｅｕｓｃｈｅｌ－Ｓｔｒｏｏｃｋ的估计，此外，对带边紧流形上的扩散过程，也给出了相同的估计。     

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.