化学发光法测定痕量酚

基于在硫酸介质中 ,高锰酸钾与痕量酚之间反应能产生较强的化学发光的实验事实 ,建立了测定酚类的化学发光分析新方法 .该法线性范围为 8.0× 10 - 6- 2 .0× 10 - 4mol/L ;检出限为 1.2×10 - 6mol/L ;对 5.0× 10 - 5mol/L的苯酚进行连续 11次平行测定 ,相对标准偏差为 3.4 % .将该法应用于环境水样中酚含量的测定 ,结果良好 .     

催化动力学分光光度法测定镨和钐

在盐酸介质中,痕量稀土元素镨和钐催化双氧水氧化碘化钾生成单质碘,单质碘可使次甲基蓝褪色,基于此建立了催化动力学分光光度法测定稀土元素镨和钐的新方法.方法的线性范围分别为5.1×10-6mol/L～5.1×10-5mol/L、5.1×10-6mol/L～5.1×10-5mol/L,检出限分别为2.75×10-6mol/L和2.44×10-6mol/L.该方法用于含稀土的纳米材料中镨和钐的分析测定,结果满意.     

Ru(phen)_3~(2+)-SO_3~(2-)-Ce(IV)体系化学发光法测定葡萄酒中的亚硫酸盐总量

提出了Ru(phen) 3 2 + -SO3 2 --Ce(IV)体系化学发光法测定溶液中亚硫酸盐的方法 SO3 2 -浓度与化学发光强度在 1 0× 10 -7～ 1 0× 10 -4mol/L范围内成正比 ,检出限为 1 97× 10 -7mol/L(S/N =3) ,1 0× 10 -4mol/LSO3 2 -溶液重复 6次测定结果的相对标准偏差为 4 9% 该方法用于测定白葡萄酒中亚硫酸盐总含量为 4 0 0 6× 10 -5mol/L ,加标回收结果令人满意     

流动注射化学发光增强法测定酪氨酸

在Na2CO3-NaHCO3介质中,酪氨酸对Luminol-K3Fe(CN)6化学发光体系有很强的增敏作用.据此建立了流动注射化学发光增强法测定酪氨酸的方法.发光信号的增强值(ΔI)与酪氨酸的浓度在5.0×10-5～4.0×10-7mol/L的范围内呈良好的线性关系,检出限为1×10-7mol/L(S/N=3),对于1.0×10-6mol/L的酪氨酸测定相对标准偏差为2.4%(N=11).该法用于测定医用氨基酸注射液中的酪氨酸,结果令人满意.     

催化动力学光度法测定啤酒中的乙醇

基于乙醇对过硫酸钾与亮绿间的氧化褪色反应的负催化作用 ,建立了一种定量乙醇的新方法 .该法的线性范围为 4.0× 10 -5～ 2 .0× 10 -3 mol/L ;检出限为 7.6× 10 -6mol/L .用于实际啤酒样品中乙醇含量的测定 ,结果良好     

Ru(phen)32+-SO32--Ce(Ⅳ)体系化学发光法测定葡萄酒中的亚硫酸盐总量

提出了Ru(phen)32+-SO32+-Ce(Ⅳ)体系化学发光法测定溶液中亚硫酸盐的方法.SO32-浓度与化学发光强度在1.0×10-7～1.0×10-4mol/L范围内成正比,检出限为1.97×10-7mol/L(S/N=3),1.0×10-4mol/LSO32溶液重复6次测定结果的相对标准偏差为4.9%.该方法用于测定白葡萄酒中亚硫酸盐总含量为4.006×10-5mol/L,加标回收结果令人满意.     

呋喃妥因的伏安法测定

应用循环伏安法、微分脉冲伏安法对呋喃妥因在玻碳电极上的伏安行为及其测定进行了研究 .实验发现 ,在 0 .10 mol/ L的 HCl底液中 ,对其进行微分脉冲阴极溶出伏安扫描 ,于 - 0 .0 7V(vs.SCE)产生一还原峰可用于呋喃妥因的定量测定 .该还原峰的微分脉冲伏安峰电流与呋喃妥因的浓度在 5.0 0× 10 -7～ 3.0 0× 10 -5mol/ L范围内呈良好的线性关系 .对 1.0 0× 10 -5mol/ L的呋喃妥因溶液中进行 10次实验 ,该峰的峰电流相对标准偏差为 2 .6 8% .本方法检测限为 2× 10 -8mol/ L.     

蒙脱石修饰电极伏安法同时测定人血中的铅、镉

报道了一种快速同时测定人血中痕量铅、镉的电分析方法 ,在pH 4.0 0的磷酸盐缓冲溶液中 ,铅、镉在钠型蒙脱石修饰玻碳电极上通过离子交换有十分灵敏的阳极溶出峰 ,由此可同时测定痕量的铅、镉离子 ,且相互间的影响较小 .优化了各种试验条件 ,如支持电解质的选择、pH值的影响、修饰剂的用量、富集电位及时间、以及扫描速度 .利用该方法测定铅、镉时线性范围分别为 4× 10 -9到 8× 10 -6mol/L和 4× 10 -9到 2× 10 -6mol/L ,检出限分别是 5× 10 -10 mol/L和 8× 10 -9mol/L .该方法简便、快速 ,灵敏度高 .用此修饰电极测定了血样中的铅、镉离子 ,结果令人满意 .     

微量锗的分析方法

以HClO4为支持电解质,没食子酸为络合剂,在示波极谱仪上对锗进行了测定.实验确定的最佳测定体系是0.1 mol/LHClO4加5.0×10-4mol/L没食子酸的体系.锗测定的线性范围是2.0×10-6～5.0×10-5 mol/L.通过一系列实验证明了该体系形成的极谱波为配合吸附波.经实验测定,其配合物的配合比为12,电极反应转移电子数为3.9.     

流动注射化学发光抑制法测定2,5-二巯基-1,3,4-噻二唑

利用在氨性条件下2,5-二巯基-1,3,4-噻二唑对焦性没食子酸-H2O2-Co(II)体系的化学发光具有抑制作用,从而建立了测定2,5-二巯基-1,3,4-噻二唑的流动注射分析方法,该法线性范围为1.0×10-3-1.0×10-4mol/L;相对标准偏差为3.6%;检出限为5.8×10-6mol/L.     

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。     

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

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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     

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