夹心结构杂多化合物N(CH3)4Na6[Na3{Co(H2O)}2WOH2O(AsW9O33)2]·35H2O的晶体结构及表征

在 p H≈ 6.5及稀土盐 Gd Cl3 · 6H2 O或 Ce( NO3 ) 3 · 6H2 O的存在下 ,Na2 WO4· 2 H2 O与Na As O2 及 Co( NO3 ) 2 · 6H2 O反应 ,得到了夹层型杂多钨酸盐 N( CH3 ) 4 Na6[Na3 {Co( H2 O) }2 WO( H2 O) ( As W9O3 3 ) 2 ]· 35 H2 O单晶 ,用 X射线单晶衍射法及元素分析确定了其结构 ,晶胞参数为 :a=1 .395 ( 1 8) nm,b=1 .90 ( 2 ) nm,c=2 .2 9( 3) nm,α=1 0 2 .3( 4 )°,β=94.7( 3)°,γ=1 0 5 .3( 3)°,V=5 .65 6( 1 2 5 ) nm3 ,Z=2 ,空间群 Pī,R1=0 .0 60 0 ,w R2 =0 .1 2 0 7( I>2σ)。[Na3 {Co( H2 O) }2 WO( H2 O) ( As W9O3 3 ) 2 ]7-具有 C2 v对称性 ,Co2 +的配位数均为 5 .对题示化合物进行了 IR,UV- Vis表征 ,讨论了其形成条件     

以联苯二胺和水为中心配体的三角三核钼原子簇合物的研究

以簇合物[Mo3O2(CH3COO)6(H2O)3]Br2·2H2O和联苯二胺为原料,在乙醇溶剂中通过置换反应合成出新的三角三核钼簇合物,经紫外光谱分析、红外光谱分析、核磁共振谱分析、元素分析确定该簇合物的组成为[Mo3O2(CH3COO)6(H2O)(NHC6H4C6H4NH2·2H+)2]Br4·10H2O,并确定了该簇合物的结构.     

缺位Keggin阴离子SiW9O10-34的酯基锡杂多配合物的合成及性质

利用酯基锡与缺位Keggin结构阴离子SiW9O10-34反应,合成了6种新的杂多阴离子有机金属配合物M4H3[(R'OOCCHR"CH2Sn)3(SiW9O37)]·xH2O(M=K+,(CH3)4N+;R'=CH3,CH3CH2;R"=H,CH3;x=6～12).通过元素分析、IR光谱、1H NMR、紫外电子光谱、循环伏安和TGA-DSC热分析等测试手段对标题配合物进行了表征和性质研究,确定该系列化合物为α-Keggin型三取代酯基锡杂多配合物.     

无机-有机杂化钼磷、钒钼磷多酸化合物的合成与结构

通过对V2 O5 ,Na2 MoO4·2H2 O ,HF ,Ni(NO3) 2 ·6H2 O ,H3PO4和吡啶体系水热反应的研究 ,合成并表征了无机 -有机杂多酸化合物 [C5 H6 N] 3[C5 H5 N][PMo12 O40 ] ( 1 ) ,[C5 H6 N] 4[PVMo11O40 ] ( 2 )和 [C5 H6 N] 4[HPV2 Mo10 O40 ] ( 3 ) .化合物( 1 )属单斜晶系 ,C/ 2c空间群 ,a =2 .1 867( 6)nm ,b =1 .3 978( 4)nm ,c =1 .663 3( 3 )nm ,β =1 0 5.73 ( 1 0 )°,V =4 .893nm3,R =0 .0 60 4 ,Z =4 ;化合物 ( 2 )属单斜晶系 ,C/ 2c空间群 ,a =2 .1 858( 4)nm ,b =1 .3 971 ( 3 )nm ,c =1 .663 5( 3 )nm ,β =1 0 5.83 ( 3 )°,V =4 .8873 ( 1 7)nm3,Z =4 ,R =0 .0 4 63 ;化合物 ( 3 )属单斜晶系 ,P2 1n空间群 ,a =1 .1 1 2 2 ( 2 )nm ,b =1 .94 1 2 ( 3 )nm ,c=1 .2 4 84 ( 3 )nm ,β =99.89( 3 )°,V =2 .6565( 9)nm3,Z =2 ,R =0 .0 690 .     

缺位Keggin阴离子SiW_9O_(34)~(10-)的酯基锡杂多配合物的合成及性质

利用酯基锡与缺位Keggin结构阴离子SiW9O10-34反应,合成了6种新的杂多阴离子有机金属配合物M4H3[(R′OOCCHR″CH2Sn)3(SiW9O37)]·xH2O(M=K+,(CH3)4N+;R′=CH3,CH3CH2;R″=H,CH3;x=6～12).通过元素分析、IR光谱、1HNMR、紫外电子光谱、循环伏安和TGA-DSC热分析等测试手段对标题配合物进行了表征和性质研究,确定该系列化合物为α-Keggin型三取代酯基锡杂多配合物.     

稀土金属离子钇(Ⅲ)-氨基多羧酸配合物结构的研究

介绍了稀土金属离子YⅢ 与一系列氨基多羧酸类配体形成配合物的合成及分子结构和晶体结构 ,并讨论了这些配合物的配位规律及形成原因 .发现具有 0 .10 4nm离子半径和d0 电子结构的稀土金属YⅢ离子一般情况下与氨基多羧酸类配体形成九配位结构的配合物 ,如K3 [YⅢ(nta) 2 (H2 O) ]·6H2 O(nta =氨三乙酸 ) ,Na[YⅢ(edta) (H2 O) 3 ]·5H2 O(edta =乙二胺四乙酸 ) ,K2 [YⅢ(dtpa) (H2 O) ]·7H2 O(dtpa =二乙三胺五乙酸 ) ,K4[YⅢ2 (Httha) 2 ]·14H2 O(ttha =三乙四胺六乙酸 )和 (NH4) 2 [YⅢ(NH4ttha) ]·5H2 O等 ,但与具有一定刚性的环己烷环的cydta(=反式 1,2 环己二胺四乙酸 )配体却形成了八配位NH4[YⅢ(cydta)(H2 O) 2 ]·4 .5H2 O配合物 .另外 (NH4) 2 [YⅢ(NH4ttha) ]·5H2 O配合物中具有可用于修饰的未配位的自由羧酸基 ( CH2 COO-) .     

多金属氧酸盐纳米粒子修饰电极的制备及电催化研究

通过溶胶 -凝胶技术首次将有机 -无机杂化的多金属氧酸盐纳米粒子 [(CH3) 4 N] 6 P2 Mo18O6 2 ·9H2 O修饰在蜡浸石墨电极的表面 ,并研究了该纳米粒子修饰电极的电化学行为和电催化行为 .不仅探索了一种更好的多金属氧酸盐修饰剂 ,而且为研究其他纳米粒子的电化学行为提供了一种简单而实用的方法 .     

配位聚合物[Ni（4，4′-bpy）（H2O）4]·（SO4^2-）·（CH3OH）·（H2O）的合成与晶体结构

通过NiSO4·6H2O与4,4'-联吡啶在H2O-CH3OH混合溶液中反应,制备了配位聚合物[Ni(4,4′-bpy)(H2O)4]·(SO42-)·(CH3OH)·(H2O),并使用X射线单晶衍射技术对其结构进行了表征.此配合物含有三种分别沿[100]、[010]、[110]方向排列的无限长链,并通过其配位水分子与位于层间位置的SO42-形成氢键而连接成为超分子结构.     

稀土杂多化合物Ba4[Ce(Ⅳ)W10O33]·24H2O制备及纳米化

以TritonX-100/n-C10H21OH/H2O体系W/O微乳液为基础,分别以K8[Ce(Ⅳ)W10O33]·32H2O和Ba(NO3)2水溶液代替组分水制备W/O微乳液.然后将两种微乳液混和,得到淡黄色沉淀的Ba4[Ce(Ⅳ)W10O32]·24H2O纳米粒子.经电镜分析所得Ba4[Ce(Ⅳ)W10O33]·24H2O纳米粒子为粒径6 nm的圆球状颗粒.并用TG-DTA和Raman对该化合物进行了袁征.     

钴配合物的合成与晶体结构

由CoCl2 ·6H2 O与KSCN和六次甲基四胺 (HMTA)反应得到超分子化合物 [Co(NCS) 2 ·(H2 O) 2 ·(HMTA) 2 ][Co(NCS) 2 ·(H2 O) 4]·(H2 O) 2 ,并测定了其晶体结构 .该化合物由 [Co(NCS) 2 ·(H2 O) 2 ·(HMTA) 2 ]、[Co(NCS) 2 ·(H2 O) 4]和H2 O三部分组成 ,每一个HMTA配体中仅有一个N原子与Co配位 ,剩余的三个N原子分别与 [Co(NCS) 2 ·(H2 O) 4]中的水及结晶H2 O分子之间形成氢键 .[Co(NCS) 2 ·(H2 O) 2 ·(HMTA) 2 ]和 [Co(NCS) 2 ·(H2 O) 4]之间通过NHO氢键连接成无限延伸的线性长链 ,链与链之间、链与结晶水之间通过不同形式的氢键构成三维结构的超分子     

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).     

Integrating GIS Web services based on mediating architecture

The geographic information service is enabled by the advancements in general Web service technology and the focused efforts of the OGC in defining XML-based Web GIS service. Based on these models, this paper addresses the issue of services chaining,the process of combining or pipelining results from several interoperable GIS Web Services to create a customized solution. This paper presents a mediated chaining architecture in which a specific service takes responsibility for performing the process that describes a service chain. We designed the Spatial Information Process Language (SIPL) for dynamic modeling and describing the service chain, also a prototype of the Spatial Information Process Execution Engine (SIPEE) is implemented for executing processes written in SIPL. Discussion of measures to improve the functionality and performance of such system will be included.