CO、N2在金属Y表面的吸附行为

对Y原子采用相对论有效原子实势(RECP/SDD),C、O、N原子采用6-311 G**基函数,利用B3LYP方法计算了YCO和YN2分子的微观结构以及不同温度下的热力学函数.以气态分子总能量中的振动能EV代替该分子处于固态时的振动能量,以电子运动和振动运动熵SEV代替分子处于固态的熵的近似方法,计算了不同温度下金属Y与CO、N2反应的ΔHΘ、ΔSΘ、ΔGΘ及反应平衡压力,导出了反应平衡压力与温度的关系.计算得出在标准条件下,YCO(s)的生成焓为-69.88 kJ.mol-1,YN2的生成焓为-46.34 kJ.mol-1.比较YCO(s)、YN2(s)和YH2(s)的G ibbs自由能ΔGΘ,可得到在常压及298.15~998.15 K温度条件下,吸附平衡压力pH2Kp(CO)>Kp(N2).比较YCO(s)和PdCO(s)的G ibbs自由能ΔGΘ以及YN2(s)和PdN2(s)的Gibbs自由能ΔGΘ,得到在常压及298.15~998.15 K温度条件下,Y对CO和N2的吸附弱于Pd对CO和N2的吸附.由此,可以认为在纯钯中加入钇,一方面增强了H2在合金膜表面的吸附,另一方面减弱了杂质气体CO和N2的吸附,从而有效提高了渗氢速率.     

CH3SH与O(3P)反应的密度泛函理论研究

用量子化学密度泛函理论(DFT)方法,对CH3SH与O(3P)的反应进行了理论研究.在B3LYP/6-31G*,B3LYP/6-311 G**水平上,优化了反应势能面上各驻点(反应物、产物、中间体和过渡态)的几何构型,在B3LYP/6-311 G**水平上通过内禀反应坐标(IRC)计算和振动分析,对过渡态进行了确认.在CCSD(T)/6-311 G**水平上进行了单点能量计算,并确定了反应机理.研究结果表明,反应主要产物为CH3SOH.     

HONO与HCl反应的量子化学研究

用量子化学密度泛函理论(DFT)和四次组态相互作用(QCISD(T)),对HONO与HCl的反应进行了研究.在B3LYP/6-311G**计算水平上,优化了反应势能面上各驻点的几何结构.在QCISD(T)/6-311G**水平上计算了单点能量.确定了反应机理,HONO与HCl反应主要生成产物为ClNO H2O.     

DFT研究大气环境中HCNO与Cl反应的产物通道

用密度泛函理论研究了大气环境中Cl与雷酸(HCNO)分子反应的机理.在6-311++G**和6-311G**基组水平上,优化得到了反应物、过渡态、中间体和产物的几何构型;在B3LYP/6-311++G**优化的构型基础上,利用CCSD(T)/6-311++G**方法对各驻点的单点能量进行校正;通过振动分析对过渡态和中间体构型进行了确认.计算结果表明:Cl与HCNO分子的反应通过Cl对HCNO分子中O或C原子进攻的多步反应得到了三种产物.其中,Cl加成到HCNO分子中O原子上消去OCl基团的反应是主反应通道,P1(HCN+OCl)为主要产物.     

S4分子结构和振动光谱的从头算

利用量子化学的从头算方法, 在6-311+G^**基组下, 分别应用HF, MP2, BLYP, B3LYP方法优化各种可能的S₄分子构型, 计算 各构型的振动光谱, 并在HF/6-311+G^**优化的几何结构基础上, 分别在MP4/6-311+G ^**和QCISD(T)/6-311+G^**水平上考虑相关能修正对总能量的影响. 比较各 种方法计算的几何结构的差别和各构型的相对稳定性, 得出顺式平面C_2v对称 构型为基态的结论. 计算表明, 确定该类分子的基态构型必须考虑电子关联效应的影响, B3LYP是计算该类分子既经济又实用的方法.     

HCNO与F反应机理的理论研究

利用量子化学计算方法,采用密度泛函理论(DFT)研究了大气环境中F与雷酸(HCNO)分子反应的机理.在6-311++G**和6-311G**基组水平上,优化得到了反应物、过渡态、中间体和产物的几何构型;在B3LYP/6-311++G**优化的构型基础上,利用CCSD(T)/6-311++G**方法对各驻点的单点能量进行校正;通过振动分析对过渡态和中间体构型进行了确认.计算结果表明:F与HCNO分子的反应有两种不同的反应机制.其中,F加成到HCNO分子中O原子上消去OF基团的反应是主要反应通道,P1(HCN+OF)为主要产物.     

甘氨酸晶体结构和振动频率的密度泛函方法研究

用密度泛函理论(DFT)的BLYP、B3LYP、Hartree-Fock(HF)和MP2方法,在6-311 G**基组水平上,对甘氨酸的几何构型和红外光谱进行了研究,并与实验结果(晶体数据)作了比较,得出了以上方法在计算甘氨酸的几何参数和谐振频率与实验数据间的相关性:在优化几何参数方面,B3LYP方法优于其它方法;在计算振动频率方面,可以看出对HF方法,标度因子校正是必要的,在非校正的情况下,DFT方法优于MP2和HF方法.     

PuCO气态分子的结构与热力学稳定性研究

根据原子分子反应静力学和群论,确定PuCO的基电子状态为((X)7A").在相对论有效原子实势近似下,应用基函数6-311G*和密度泛函理论B3LYP方法,全电子计算了钚化物的能量E、定容热容CV和熵S.应用电子振动近似理论,即用单个分子PuCO中的电子和振动能量和熵近似代表它们处于固态时的能量和熵.计算所得到的PuCO气态分子的结构与不同温度下的热力学函数.根据热力学原理,计算得到PuCO气态分子在不同温度下的标准生成自由能变均为较大正值,据此说明,uCO气态分子不具有热力学稳定性.     

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.     

PuCO气态分子的结构与热力学稳定性研究

根据原子分子反应静力学和群论,确定PuCO的基电子状态为(7A)″。在相对论有效原子实势近似下,应用基函数6-311G4和密度泛函理论B3LYP方法,全电子计算了钚化物的能量E、定容热容Cv和熵S。应用电子振动近似理论,即用单个分子PuCO中的电子和振动能量和熵近似代表它们处于固态时的能量和熵.计算所得到的PuCO气态分子的结构与不同温度下的热力学函数。根据热力学原理,计算得到PuCO气态分子在不同温度下的标准生成自由能变均为较大正值,据此说明,PuCO气态分子不具有热力学稳定性。     

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.     

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.     

A computer generator for randomly layered structures

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

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。     

Exciton Seebeck in Molecular Systems

Various applications relevant to the exciton dynamics,such as the organic solar cell,the large-area organic light-emitting diodes and the thermoelectricity,are operating under temperature gradient.The potential abnormal behavior of the exicton dynamics driven by the temperature difference may affect the efficiency and performance of the corresponding devices.In the above situations,the exciton dynamics under temperature difference is mixed with     

Achieving Unusual States of Matter Under High Pressure

The elongation method,originally proposed by Imamura was further developed for many years in our group.As a method towards O(N)with high efficiency and high accuracy for any dimensional systems.This treatment designed for one-dimensional(ID)polymers is now available for three-dimensional(3D)systems,but geometry optimization is now possible only for 1D-systems.As an approach toward post-Hartree-Fock,it was also extended to     

《Chinese Science Bulletin》SUBJECT INDEX TO VOLUME 59(2014)

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An on-line scaling method for improving scalability of a database cluster

The explosive growth of the Internet and database applications has driven database to be more scalable and available, and able to support on-line scaling without interrupting service. To support more client's queries without downtime and degrading the response time, more nodes have to be scaled up while the database is running. This paper presents the overview of scalable and available database that satisfies the above characteristics. And we propose a novel on-line scaling method. Our method improves the existing on-line scaling method for fast response time and higher throughputs. Our proposed method reduces unnecessary network use, i.e. , we decrease the number of data copy by reusing the backup data. Also, our on-line scaling operation can be processed parallel by selecting adequate nodes as new node. Our performance study shows that our method results in significant reduction in data copy time.     

An improved R-tree based on childnode''s probability

R-Tree is a good structure for spatial searching. But in this indexing structure,either the sequence of nodes in the same level or sequence of traveling these nodes when queries are made is random. Since the possibility that the object appears in different MBR which have the same parents node is different, if we make the subnode who has the most possibility be traveled first, the time cost will be decreased in most of the cases. In some case, the possibility of a point belong to a rectangle will shows direct proportion with the size of the rectangle. But this conclusion is based on an assumption that the objects are symmetrically distributing in the area and this assumption is not always coming into existence. Now we found a more direct parameter to scale the possibility and made a little change on the structure of R-tree, to increase the possibility of founding the satisfying answer in the front sub trees. We names this structure probability based arranged R-tree (PBAR-tree).     

Wuhan University Journal of Natural Sciences TOTAL CONTENTS

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