吸附溶出伏安法同时测定水中痕量锌和镉

报道了同时测定痕量锌和镉的新方法 .在 0 .0 1mol/LHAc - 0 .0 1mol/LNaAc- 1.2× 10 - 5mol/L乙醛酸缩氨基硫脲 (GATSC)中 ,Zn -GATSC和Cd -GATSC均产生非常灵敏的吸附波 ,峰电位分别是 - 0 .82V和 - 0 .4 3V(vs·SCE) ,峰电流和锌、镉的浓度分别在 3.0× 10 - 8～ 8.0× 10 - 7mol/L和 1.0× 10 - 8～ 6 .0× 10 - 7mol/L范围内成直线关系 ,检测限分别是 8.0× 10 - 9和 3.0× 10 - 9mol/L .该方法用于测定水中痕量锌和镉 ,结果令人满意     

TASPAP分光光度法测定水中镉（Ⅱ）离子

用分光光度法研究了新试剂2-(2-噻唑偶氮)-5-磺丙氨基苯酚(TASPAP)与镉(Ⅱ)的显色反应性能.在pH =8的Clark-Lubs缓冲溶液中,TASPAP与镉(Ⅱ)形成配合物,该配合物的最大吸收峰位于550 nm波长处,镉(Ⅱ)的量在0～60 μg范围内符合郎伯-比尔定律, 表观摩尔吸光系数为3.30×104(L·mol-1·cm-1),灵敏度较高,该方法用于镉离子的测定,结果令人满意.     

镉与锡、锆、铁和铈的浮选分离研究

研究了四丁基溴化铵-碘化钾体系分离镉的行为及与其他金属离子分离的条件.实验结果表明, 在水溶液中, Cd(Ⅱ)与四丁基溴化铵和碘化钾形成不溶于水的三元缔合物[CdI4][TBAB]2,此三元缔合物沉淀浮于水相上层形成界面清晰的液-固两相.当四丁基溴化铵和碘化钾的浓度分别为5.0×10-4 mol·L-1和8.0×10-3 mol·L-1, 且缓冲溶液为pH 2.0时, 该体系对Cd(Ⅱ)的浮选率在99.2 %以上.Sn(Ⅳ)、Zr(Ⅳ)、Fe(Ⅱ) 和Ce(Ⅲ)等离子在该体系不被浮选,实现了Cd(Ⅱ)与这些金属离子的定量分离.对合成水样中Cd(Ⅱ)的分离和测定,结果满意.该方法具有简便、快速等特点,在微量镉的分离和富集分析中有一定的实用价值.     

新试剂3-[3-(4-苯基-2-噻唑基)三氮烯基]苯磺酸与阳离子表面活性剂显色反应的研究

研究新试剂3-[3-(4-苯基-2-噻唑基)三氮烯基1苯磺酸(PTTBSA)与阳离子表面活性剂溴化十六烷基三甲铵(CTMAB)的显色反应,在pH 12.4的缓冲介质中,试剂与CTMAB发生显色反应,形成深红色离子缔合物,最大吸收波长555nm,试剂与CTMAB的缔合比为1:3,其表观摩尔吸光系数为1.04×104L·mol-1·cm-1,CTMAB量在0.1×10-5～3.0×10-5mol/L范围内服从比尔定律,该方法直接用于水中微量CTMAB的测定,结果满意.     

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 .     

1-(5,7-二溴-8-喹啉)-3-(偶氮苯)-三氮烯的合成及作为镉的光度分析试剂

合成了新显色剂1-(5,7-二溴-8喹啉)-3(偶氮苯)-三氮烯(DBQABT),其结构由红外光谱和元素分析确证.研究了DBQABT与镉的显色反应在.pH9.8～10.5的硼酸盐缓冲介质中,镉与该试剂形成1:2的橙红色络合物,其最大吸收波长位于525 nm处,表观摩尔吸光系数为2.10×105L·mol-1·cm-1,镉的浓度在0～20μg/25 mL范围内符合比尔定律在掩蔽剂存在下,常见离子基本不干扰.用于工业废水中微量镉的测定,结果与原子吸收法一致.     

镉超高灵敏显色反应的研究

本文研究了高灵敏测定镉的光度法,在阿拉伯胶存在下,在0.02—0.16mol/L硫酸介质中,镉与碘化物和罗丹明6G生成离子缔合物。该缔合物最大吸收波长为525mn,表观摩尔吸收系数ε525为1.6×106L·mo1-1·cm-1,镉浓度在0—2μg/25ml符合比耳定律。考察了共存离子的干扰影响,该法可用于测定水中痕量镉。     

镉(Ⅱ)—碘化钾—丁基罗丹明B显色反应的研究

本文研究了在聚乙烯醇和Tritonx—100存在下,镉(Ⅱ)—碘化钾—丁基罗丹明B离子缔合物显色反应的条件。络合物最大吸收峰在600nm,摩尔吸光系数为2.2×10~5l·mol~(-1)·cm~(-1)。镉量在0.5-4.0μg/25ml范围内服从比尔定律。试验了若干种离子的干扰,此法已用于自来水中微量Cd~(2+)的测定。     

试剂DBNPDAPT与十六烷基二甲基苄基氯化铵显色反应的研究

研究2，6-二溴-4-硝基苯基重氮氨基-4-苯基-2-噻唑（DBNPDAPT）与阳离子表面活性剂十六烷基二甲基苄基氯化铵（HDBAC）的显色反应.建立分光光度测定阳离子表面活性剂HDBAC的新方法.结果表明，在NaOH碱性介质中，试剂DBNPDAPT与HDBAC形成蓝色离子缔合物.其最大吸收波长为615 nm，试剂DBNP?DAPT与HDBAC的缔合比为1：2，其表观摩尔吸光系数为1.37×104 L·mol-1·cm-1，HDBAC量在0～2.0×10-5 mol/L范围内服从比尔定律.该方法直接用于合成水样中微量HDBAC的测定，结果满意.     

DNA/CTC双向捕集离子液体浮选分离测定废水中痕量Ni(Ⅱ)

在一定条件下,Ni(Ⅱ)在溶液中能够被脱氧核糖核酸(DNA)和金霉素(CTC)双向捕集,形成Ni-CTC-DNA三元缔合物.该缔合物具有良好的疏水性,利用离子液体[bmim]BF_4浮选体系可以将其从混合溶液中分离提取出来.研究了缔合物形成和离子液体浮选过程的影响因素,得到了三元缔合物生成和浮选分离的最优条件.线性回归方程为A=8.03×10⁵C-0.000 3,线性范围为4.7×105C-0.000 3,线性范围为4.7×10^(-8)(-8)⁶.5×106.5×10^(-3)mol/L,摩尔吸光率为8.03×10(-3)mol/L,摩尔吸光率为8.03×10⁵L·mol5L·mol^(-1)·cm(-1)·cm^(-1),检出限为1.8×10(-1),检出限为1.8×10^(-8)mol/L.该方法可用于工业废水中重金属镍离子的快速检测分析.     

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.     

Features of Women's language

Language is a means of verbal communication. People use language to communicate with each other. In the society, no two speakers are exactly alike in the way of speaking. Some differences are due to age, gender, statue and personality. Above all, gender is one of the obvious reasons. The writer of this paper tries to describe the features of women＇s language from these perspectives： pronunciation, intonation, diction, subjects, grammar and discourse. From the discussion of the features of women＇s language, more attention should be paid to language use in social context. What＇s more, the linguistic phenomena in a speaking community can be understood more thoroughly.     

A computer generator for randomly layered structures

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

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。     

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.     

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。     

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.     

《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