纯粘土矿物甲烷吸附研究及吸附模型评价

粘土矿物在页岩储层无机矿物中占有重要的比例,其是页岩气吸附的重要场所。由于不同页岩储层成藏条件差异,粘土矿物相对含量有较大差异,因此也影响页岩气的吸附能力。以XRD,低压氮气吸附实验以及甲烷等温吸附实验为主要研究手段。XRD结果表明四种样品(伊利石,蒙脱石,绿泥石,高岭石)纯度较高,均大于94%。低压氮气吸附结果表明：蒙脱石以微孔与中孔为主,孔隙形态主要为四边都开口的平行板状、狭缝状等,含有墨水瓶状的孔;伊利石主要发育有中孔与大孔,绿泥石主要发育有微孔和大孔,高岭石主要发育有中孔和大孔,它们的孔隙形态同样都平行板状、狭缝状等为主;比表面积与孔隙体积的大小顺序为：高岭石>伊利石>蒙脱石>绿泥石,两者呈正相关。在61 ℃,压力为0~25 MPa条件下进行五组甲烷等温吸附试验,包括四组纯粘土矿物及一组由四种纯矿物等质量混合的矿物。纯粘土矿物甲烷吸附量大小顺序为：高岭石>伊利石>蒙脱石>绿泥石,粘土矿物的比表面积越大,其甲烷吸附量也越大。对等温吸附实验数据进行拟合发现：Langmuir, Toth以及Langmuir-Freundlich吸附模型对于不同矿物总体拟合效果都极好,对粘土矿物吸附模型精确选择具有一定意义。     

纯黏土矿物甲烷吸附研究及吸附模型评价

黏土矿物在页岩储层无机矿物中占有重要的比例,其是页岩气吸附的重要场所。由于不同页岩储层成藏条件不同,黏土矿物相对含量存在较大差异,因此也影响页岩气的吸附能力。以X射线衍射(XRD)、低压氮气吸附实验及甲烷等温吸附实验为主要研究手段,XRD结果表明:4种样品(伊利石,蒙脱石,绿泥石,高岭石)纯度较高,均大于94%。低压氮气吸附结果表明:蒙脱石以微孔与中孔为主,孔隙形态主要为四边都开口的平行板状、狭缝状等,含有墨水瓶状的孔;伊利石主要发育有中孔与大孔,绿泥石主要发育有微孔和大孔,高岭石主要发育有中孔和大孔,其的孔隙形态同样都平行板状、狭缝状等为主;比表面积与孔隙体积的依次为高岭石伊利石蒙脱石绿泥石,且两者呈正相关。在61℃,压力为0～25 MPa条件下进行5组甲烷等温吸附试验,包括4组纯黏土矿物及1组由4种纯矿物等质量混合的矿物。纯黏土矿物甲烷吸附量依次为高岭石伊利石蒙脱石绿泥石,黏土矿物的比表面积越大,其甲烷吸附量也越大。对等温吸附实验数据进行拟合发现:Langmuir、Toth及Langmuir-Freundlich吸附模型对于不同矿物总体拟合效果都极好,对黏土矿物吸附模型精确选择具有一定意义。     

配合物Eu（P—MOBA）3bpy的晶体结构

在乙醇溶液中合成了对甲氧基苯甲酸－２，２′－联吡啶铕配合物的晶体，用ｘ－射线衍射方法测定了配合物的单晶结构，其结构式为Ｅｕ２（Ｐ－ＭＯＢＡ）６（ｂｐｙ）２Ｃ２Ｈ５ＯＨ（Ｐ－ＭＯＢＡ：对甲氧基苯甲酸根离子；ｂｐｙ；２，２′联吡啶），属三斜晶系ＰＴ空间群，晶胞参数；ａ＝１４８２（３）ｎｍ，ｂ＝１．３９０１（２）ｎｍ，ｃ＝１．０９４８（２）ｎｍ；α＝１０３．６３（１）＾０，β＝９２．６７（２）６０，γ＝     

〔Eu(NTO)_3(H_2O)_5〕5H_2O的合成和晶体结构

用３－硝基－１，２，４－三唑－５－酮（ＮＴＯ）的锂盐水溶液与Ｅｕ２Ｏ３的稀硝酸溶液反应，合成了ＮＴＯ的铕配合物，其单晶结构用Ｘ射线分析法进行了测定，确定了它的结构式为〔Ｅｕ（ＮＴＯ）３（Ｈ２Ｏ）５〕５Ｈ２Ｏ。其晶体属单斜晶系，空间群为Ｐ２１／ｎ，最终偏离因子Ｒ为０．０２３。晶胞参数如下：ａ１．８７２０（２）ｎｍ，ｂ０．６５４８（３），ｃ１．９３２３（３）ｎｍ，β９５．３３（１）°，Ｖ２．３５８３（５）ｎｍ３，Ｚ４，Ｄｃ２．０２６ｇｃｍ－３，μ２７．６７８ｃｍ－１，Ｆ（０００）１４３２。铕离子的配位数为８，其配位多面体为畸变的十二面体     

LASERINDUCEDDISSOCIATIONOFKETENE（CH2CO）AT355nm：PHOTOACOUSTICSTUDIES

用光声方法观测乙烯酮分子的激光诱导离解以及研究离解碎片ＣＨ２（Ｘ３Ｂ１）的动力学。实验结果说明在３５５ｎｍ强激光辐射下，乙烯酮的非线性吸收只能诱导乙烯酮母体分子和（或）离解碎片的多光子离子化，这是造成光声信号随激光能量升高而降低的原因，再化合过程ＣＨ２（Ｘ３Ｂ１）＋ＣＨ２（Ｘ３Ｂ１）—→Ｃ２Ｈ２＋２Ｈ的速率常数是２．３９×１０－１１ｃｍ３ｍｏｌｅｃｕｌｅ－１Ｓ－１ＣＨ２（Ｘ３Ｂ１）＋ＣＨ２ＣＯ—→ＣＨ３＋ＣＨＣＯ的反应速度常数估计是１０－１２ｃｍ３ｍｏｌｅｃｕｌｅ－１Ｓ－１．     

微区原位测温技术建立储层填隙物成岩演化序列——以鄂尔多斯盆地陇东地区长8为例

为研究长8储层填隙物的演化过程,通过铸体薄片、扫描电镜、碳氧同位素、激光拉曼、电子探针等分析技术,对陇东地区长8储层中的绿泥石、伊利石和碳酸盐胶结物3种填隙物进行了微区原位测温分析,确定出绿泥石、伊利石、碳酸盐胶结物的形成温度,定量地分析了长8储层填隙物成岩序列。研究表明：长8储层主要发育绿泥石、伊利石、高岭石、硅质及碳酸盐胶结物5种填隙物类型,填隙物含量存在明显差异性。陇东地区长8储层填隙物充填顺序为：Ⅰ期绿泥石环边→Ⅰ期碳酸盐胶结→Ⅰ期自生石英→高岭石+Ⅱ期自生石英→Ⅰ期伊利石→Ⅱ期绿泥石+Ⅱ期伊利石+Ⅱ期碳酸盐→Ⅲ期自生石英→Ⅲ期伊利石→Ⅲ期碳酸盐→Ⅲ期绿泥石。     

TmxY1—xAl3（BO3）4晶体生长和光谱特性

用Ｋ２Ｍｏ３Ｏ１０－Ｂ２Ｏ３作助熔剂，采用缓慢降温自发成核的方法，生长了稀土四硼酸盐晶体ＴｍｘＹ１－ｘＡｌ３（ＢＯ３）４（简称ＴＹＡＢ），晶体尺寸为８×６×５ｍｍ３．对所获得晶体进行Ｘ射线结构分析，表明ＴＹＡＢ晶体属三方晶系，晶胞参数ａ＝９．２３７，ｃ＝７．１９２．测定了该晶体室温下的红外光谱、反射光谱、激发光谱及荧光光谱，当用２６１ｎｍ波长激发时，可产生３４５ｎｍ（３Ｐ０→３Ｈ４）蓝紫色及４５０ｎｍ（１Ｄ２→３Ｈ４）蓝绿色的荧光发射     

（C_6H_5）_3PO·p－ClC_6H_4OCH_2COOH的晶体结构

合成了（Ｃ６Ｈ５）３ＰＯ·ｐ－ＣｌＣ６Ｈ４ＯＣＨ２ＣＯＯＨ并解析了其单晶体结构。结果表明该晶体属于正交晶系，空间群是Ｐｂｃａ，ａ＝１．７１２２（４）ｎｍ，ｂ＝２．３８０３（７）ｎｍ，ｃ＝１．１３２８（４）ｎｍ，该晶体由三苯基氧膦和对氯苯氧乙酸组成，但晶体中对氯苯氧乙酸同单独的对氯苯氧乙酸晶体结构比较，相应的键长和键角有明显的差异。     

长江口启东嘴潮滩黏土矿物沉积特征及环境意义

黏土矿物是认识沉积环境变化和示踪物质来源的重要环境指标。应用粉晶X射线衍射(XRD)方法对长江口启东嘴潮滩的岩芯沉积物的黏土矿物组成进行分析,结果表明:伊利石含量最高,均值为54.11%;其次为绿泥石和蒙脱石,均值分别为21.30%、16.21%;高岭石最低,均值为8.37%。组合类型多样,主要为Ⅰ型(伊利石+绿泥石+蒙脱石+高岭石)、Ⅱ型(伊利石+绿泥石+高岭石+蒙脱石)、Ⅲ型(伊利石+蒙脱石+绿泥石+高岭石)。物源分析结果显示,研究区沉积物与南黄海物质的关系最为密切。南黄海沉积物受到长江和黄河的共同影响,在长期的地质过程作用下具有混合源特征。沉积物来源的变化与沉积动力环境的变化密切相关。人类围垦活动造成分流角加大,接近90°,导致长江北支分流比急剧下降,河槽性质发生质的变化,涨潮流成为主要动力作用。来自口外南黄海的悬浮泥沙,在涨潮动力的携带下扩散倒灌成为研究区主要的物质来源。     

铒钇异核谷氨酸配合物的合成及晶体结构

在水溶液中合成了铒钇异核谷氨酸配合物［ＥｒＹ（Ｇｌｕ）２（Ｈ２Ｏ）８］·（ＣｌＯ４）４·２．７５Ｈ２Ｏ的单晶，并用Ｘ射线单晶衍射仪测定了其晶体结构。晶体属单斜晶系，Ｐ２１空间群。晶胞参数：α＝１．１０３９０（１０）ｎｍ，ｂ＝１．６４９３（２）ｎｍ，ｃ＝１．９９８６（３）ｎｍ，β＝１０３．６００（１０）０，Ｖ＝３．５３６７（８）ｎｍ３，Ｚ＝４，Ｄｃ＝２．１４１ｇ／ｃｍ３。最终偏差因子Ｒ＝０．０３１１。配合物为由双核联结成的网状分子。在每个双核结构单元中，２个金属离子被４个谷氨酸的４个羧基桥联，２个谷氨酸的远离氨基的羧基以三齿（螯合配位加上１个氧桥）与中心离子配位；每个中心离子还有４个水分子配位，因此，铒和钇离子的配位数为９，形成三角十四面体型配位多面体     

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.     

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.     

Tracking data management using topology of moving object database system for moving object constrained trajectory in LBS application

Advances in wireless technologies and positioning technologies and spread of wireless devices, an interest in LBS (Location Based Service) is arising. To provide location based service, tracking data should have been stored in moving object database management system (called MODBMS) with proper policies and managed efficiently. So the methods which acquire the location information at regular time intervals then, store and manage have been studied. In this paper, we suggest tracking data management techniques using topology that is corresponding to the moving path of moving object. In our techniques, we update the MODBMS when moving object arrived at a street intersection or a curved road which is represented as the node in topology and predict the location at past and future with attribute of topology and linear function. In this technique, location data that are corresponding to the node in topology are stored, thus reduce the number of update and amount of data. Also in case predicting the location,because topology are used as well as existing location information, accuracy for prediction is increased than applying linear function or spline function.