用具有变ω值通用对应态方程计算正烷烃类饱和蒸汽压

作者曾建议了一个通用对应态方程。本文认为偏心因子ω随对比温度T_r应该是变化的,并建立了ω与T_r的关联。文中使用具有变ω值的通用对应态方程计算了正烷烃C_1～C_(20)20种流体的饱和蒸汽压,总平均绝对偏差为0.48%,它大大小于由其它方程计算得到的偏差。     

~(14)NH自由基基态与第一激发单重态的结构与势能函数

使用QCISD(T)/6-311++G(3df,2pd)和SAC-CI/D95(d)方法分别对14NH自由基的基态与第一激发单重态进行几何优化和离解能的计算,并进行了单点能扫描,同时用正规方程组拟合Murrell-Sorbie函数.利用得到的势能函数计算了与基态、第一激发单重态相对应的力常数(f2,f3,f4)和光谱数据(ωe,Be,eα,ωeχe),结果与实验数据符合的很好.     

BeH分子第一激发双重态A~2Π的结构与势能函数

使用“对称性匹配簇-组态相互作用”方法,6-311++G(3df,2pd)基组对BeH分子的第一激发双重态A2Π进行几何优化和离解能的计算,并进行了单点能扫描,同时用正规方程组拟合Murrell-Sorbie函数.利用得到的势能函数计算了与第一激发双重态相对应的力常数(f2,f3,f4)和光谱数据(eω,Be,eα,ωeχe),结果与实验数据符合的非常好.     

切削测力仪动力学分析与切削力动态测量误差确定

本文从分析具有普遍性意义的测力仪双自由度振动模式出发，采用复变函数方法求解了与振动模式对应的微分方程组，给出了频率响虚特性ψ(ω)、幅频特性|ψ(ω)|和相频特性φ(ω)的准确表达式。本文还给出了测力仪动态测动态测尾误差的计算方法，证实了压电式压力仪测力仪测量误差δ压电远远小于位移型测力测量误差δ位移的原因。     

范畴内部算子中的开态射

给出范畴内部算子的一些结果,通过一般拓扑学中连续开映射的等价刻画,定义了范畴内部算子中的开态射,并研究了它们的性质.设Ω是一个范畴,ω是Ω上的一类单态射使得(ε,ω)是一个恰当的保持的分解系统.IN(Ω,ω),CL(Ω,ω)和NO(Ω,ω)分别记为范畴Ω相对应ω的范畴内部算子、范畴闭包算子和范畴邻域算子的全体.当满足一定条件和适当的序关系给IN(Ω,ω),CL(Ω,ω)和NO(Ω,ω),可以证明它们彼此是完备类之间的同构.     

OT,DT分子基态(X~2Π)的结构与势能函数

采用密度泛函方法(B3LYP)和二次组态相互作用方法(QCISD(T))优化计算了OT,DT分子基态(X2Π)的平衡结构、振动频率和离解能.根据原子分子反应静力学原理,导出了OT,DT分子基态(X2Π)的合理离解极限,采用最小二乘法拟合Murrell-Sorbie函数得到了相应的势能函数和与该基态相对应的光谱常数(Be,eα,eω和ωeχe),计算结果与实验数据符合得相当好.     

BeO分子X~1Σ~+,a~3Π和b~3Σ~+电子态的光谱性质

使用内收缩多参考组态相互作用方法和相关一致基aug-cc-p Vn Z(n=Q,5)对Be O分子的光谱性质开展研究.计算了Be O分子X1Σ+,a3Π和b3Σ+态的势能曲线,并将3个态的能量外推至完全基组极限.对分子能量进行相对论效应及核价相关效应修正计算.相对论修正计算采用cc-p V5Z相对论收缩基,核价相关修正计算使用的基组是aug-cc-p CVQZ基.拟合能量修正的外推势能曲线,得到3个态的光谱常数(Te,Re,ωe,ωexe,Be,αe和De).这些结果与实验结果符合很好.详细讨论了基组、核价相关修正和相对论修正对Be O分子的能量及光谱常数的影响.通过求解双原子分子核运动的振-转Schrdinger方程,找到了J=0时Be O分子3个态的全部振动态及与每一振动态对应的振动能级和惯性转动常数等分子常数.它们与实验结果一致.     

7Li2分子A1Σ+u态的平衡几何、离解能及其谐振频率

利用分子反应静力学的原理,确定了7Li2分子A1Σ 态的离解极限;利用SAC-CI方法、使用6-311G、6-311 G、6-311G(3df,3pd)、6-311 G(3df,3pd)、D95(3df,3pd)、D95、D95V、D95V(d,p)、cc-PVTZ和AUG-cc-PVTZ等基组,对7Li2分子A1Σu 态的平衡几何进行了优化计算,且将计算结果与精细的单点能扫描结果进行了比较.分析表明,由单点能扫描获得的平衡核间距应更为合理.同时也得出了AUG-cc-PVTZ基组为最优基组的结论.在0.14~1.5 nm范围内对该态进行了单点能扫描,并用最小二乘法拟合出了其解析势能函数.从得到的解析势能函数出发,计算了该态的力常数(f2、f3和f4)及谐振频率(ωe),进而计算了其他光谱常数(Be,αe和ωeχe),理论值与实验结果一致.同时为便于分析和比较,对基态X1Σg 也进行了相应的计算.     

亚硝酸钠光学性质的第一性原理研究

为了更好地理解亚硝酸钠在铁电相和顺电相间光学性质的差异，计算了它的介电虚部ε2(ω)、光吸收系数I(ω)及反射系数R(ω)．ε2(ω)、I(ω)和R(ω)的计算结果表明，亚硝酸钠是一种各向异性比较明显的材料，并且其光学性质在铁电相中要比在顺电相中具有更高的各向异性．     

SeBrn(n=0,+1,+2)基态及SeBr低激发态的势能函数及微观性质

采用6-311 G**基组、B3LYP方法对SeBrn(n=0, 1, 2)分子离子基态进行了结构优化和频率计算,用TDB3LYP/6-311 G**含时方法对激发态B12Ⅱ、B22Ⅱ进行了计算,得到SeBrn(n=0, 1, 2)分子离子基态和SeBr分子激发态B12Ⅱ、B22Ⅱ的平衡几何结构、电子状态、谐振频率、偶极矩、离解能De等相关性质,并在计算出来的一系列单点势能基础上,用正规方程组拟合Murrell-Sorbie(M-S)势能函数,得到相应态的解析势能函数,光谱参数Be、αe、ωe、和ωexe,由此计算对应的光谱参数和力学性质.理论计算值与相关文献值吻合较好,说明用B3LYP(TDB3LYP)/6-311 G**方法计算SeBrn(n=0, 1, 2)分子离子基态和激发态微观结构性质是可行的.     

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。     

A computer generator for randomly layered structures

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

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.     

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.     

海南岛地体及其毗邻陆缘晚中生代—新生代古地磁研究和构造演化

本文叙述了对海南岛及其毗邻大陆边缘白垩纪到第四纪地层岩石进行古地磁研究的全部工作过程。通过分析岩石中剩余磁矢量的磁偏角及磁倾角的变化,提出海南岛白垩纪以来经历的构造演化模式如下:早期伴随顺时针旋转而向南迁移,后期伴随逆时针转动并向北运移。联系该地区及邻区的地质、地球物理资料,对海南岛上述的构造地体运动提出以下认识:北部湾内早期有一拉张作用,主要是该作用使湾内地壳显著伸长减薄,形成北部湾盆地。从而导致了海南岛的早期构造运动,而海南岛后期的构造运动则主要是受南海海底扩张的影响。海南地体运动规律的阐明对于了解北部湾油气盆地的形成演化有重要的理论和实际意义。     

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