Fe3O4/纳米级Fe0去除水中Cr(VI)的研究

本文考察了Fe3O4/纳米级Fe0对污染水中Cr(VI)的去除效果,以及Fe3O4投加量、腐殖酸投加量、温度对Fe3O4/纳米级Fe0去除水中Cr(VI)的影响。结果表明：Fe3O4/纳米级Fe0对水中Cr(VI)的去除效果很好,在2min时Cr(VI)的去除率就能够达到91.4%,这个值比纳米级Fe0单独作用120min时对 Cr(VI)的去除率还要高;Fe3O4与纳米级Fe0的配比为7.5:1时,Fe3O4/纳米级Fe0对Cr(VI)的去除效果最好。温度的升高加速了Fe3O4/纳米级Fe0对水中Cr(VI)还原降解反应的进行。     

Fe3O4/纳米级Fe0去除水中Cr（Ⅵ）的研究

考察了Fe3O4/纳米级Fe0对污染水中Cr(Ⅵ)的去除效果,以及Fe3O4投加量、腐殖酸投加量、温度对Fe3O4/纳米级Fe0去除水中Cr(Ⅵ)的影响。结果表明:Fe3O4/纳米级Fe0对水中Cr(Ⅵ)的去除效果很好,在2 min时Cr(Ⅵ)的去除率就能够达到91.4%;这个值比纳米级Fe0单独作用120 min时对Cr(Ⅵ)的去除率还要高。Fe3O4与纳米级Fe0的配比为7.5:1时,Fe3O4/纳米级Fe0对Cr(Ⅵ)的去除效果最好。温度的升高加速了Fe3O4/纳米级Fe0对水中Cr(Ⅵ)还原降解反应的进行。     

以硫酸钴或硫酸铁为催化剂快速测定化学耗氧量

以CoSO4或Fe2(SO4)3代替Ag2SO4,对模拟废水及实际废水进行COD测定,获得了与国家标准法相近的测定结果.分别考察了微波消解时间、硫酸用量和催化剂投加量等对COD测定结果的影响.结果表明:在CoSO4的投加量为0.10 g或Fe2(SO4)3的投加量为0.09 g、硫酸用量5 mL、消解时间5 min时,分析结果达到最佳.确立的方法测定结果准确、可靠,可以用作废水COD的测定.采用廉价的CoSO4或Fe2(SO4)3代替昂贵的Ag2SO4作催化剂,能大大降低分析成本.     

基于普鲁士蓝纳米粒子的形成利用共振瑞利散射技术测定盐酸土霉素

在pH值为1.4的盐酸溶液中,盐酸土霉素将Fe3+还原成Fe2+,Fe2+能与[Fe(CN)6]3-反应生成Fe3[Fe(CN)6]2络合物,并进一步聚集形成普鲁士蓝纳米粒子.该纳米粒子的形成导致共振瑞利散射强度显著增强,最大散射波长位于380nm,RRS的增强值(ΔIRRS)在一定范围内与盐酸土霉素的质量浓度成正比.同时,该方法操作简单、快速,具有较宽的线性范围和高的灵敏度,线性范围为0.05~1.5mg/L,检出限为8.62μg/L.据此,基于普鲁士蓝纳米粒子的形成,建立了利用共振瑞利散射技术测定盐酸土霉素的新方法.研究了这一反应体系的RRS光谱,探究了最佳反应条件并考察了干扰物质的影响.同时,将该方法用于盐酸土霉素实际样品的检测,得到了满意的结果.此外,还初步探讨了该体系的反应机理和RRS增强的原因.     

流动注射化学发光测定盐酸多巴酚丁胺

基于盐酸多巴酚丁胺对高锰酸钾氧化鲁米诺产生的化学发光的增强作用建立了一种测定盐酸多巴酚丁胺的新方法.在优化的实验条件下,测定盐酸多巴酚丁胺的线性范围为1 0×10-3～0 5μg/mL,检出限(3σ)为5 0×10-4μg/mL,对浓度为0 4μg/mL的盐酸多巴酚丁胺进行11次平行测定,其相对标准偏差(RSD)为3 39%.将本法用于注射液、血样以及尿样中盐酸多巴酚丁胺的测定,结果令人满意.     

铁离子对曼尼希碱型盐酸缓蚀剂(FHS-A)缓蚀性能的影响

采用单因素实验,运用静态失重法考察Fe3+含量对曼尼希碱型盐酸缓蚀剂(FHS-A)缓蚀性能的影响.还考察了N80钢片在具有Fe3+的HCl溶液中的腐蚀速率随盐酸质量浓度和缓蚀剂质量分数的变化规律.结果表明:Fe3+对曼尼希碱型盐酸缓蚀剂(FHS-A)有一定的影响,随着Fe3+含量的增大腐蚀速率增大;随着缓蚀剂质量分数的增大腐蚀速率减小;随着盐酸质量浓度的增大腐蚀速率增大.根据实验结果,初步探讨了Fe3+对曼尼希碱型盐酸缓蚀剂(FHS-A)缓蚀性能的影响机理.通过电镜扫描和能谱分析,证实了Fe3对曼尼希碱型盐酸缓蚀剂(FHS-A)缓蚀性能的影响.     

邻氯苯基荧光酮-溴十六烷基三甲铵光度法测定微量锆

在表面活性剂存在下,水杨基荧光酮,对羟基苯基荧光酮光度法等测定锆已有报道.邻氯苯基荧光酮(o-CPF)由于邻位强吸电子基氯的影响,与锆的反应灵敏度更高,可在更强的酸性介质中反应,选择性更好,实验证明:在0.4mol·L~(-1)盐酸介质中,锆与粼氯苯基荧光酮和溴化十六烷基三甲铵形成橙红色络合物,该络合物,络合物5分钟内显色完全,40分钟内基本不变,组成比在,0～12μg/25ml锆浓度范围内符合比尔定律。由于体系在较强的酸性介质中进行,大量的SO_4~(2-)、NO_3~-、Ca(Ⅱ)、Cu(Ⅱ)等不干扰测定,Fe(Ⅲ)及少量Ti(Ⅳ)、Mo(Ⅵ)干扰测定,可根据显色快慢消除Ti影响,用盐酸羟胺及抗坏血酸混用消除Fe(Ⅲ)及Mo(Ⅵ)影响。此法灵敏度高、选择性好,方法简单快速,可用于钢铁中微量锆的直接测定。     

分光光度法催化动力学分析痕量铝

根据AI 3 对KIO4氧化次甲基蓝褪色的催化行为,建立了测定痕量铝的催化动力学分析法,本法线性测定范围为0～720μg/L,检测限为1.1×10-8g/L,除Fe 3 外其余离子不影响测定,Fe 3 的干扰可用铜铁试剂-氯仿溶液萃取除去,利用本法测定水样中的铝含量,结果满意.     

复合纳米Fe2O3/TiO2的制备、表征及光催化活性

采用将TiO2 加入Fe(OH ) 3 胶体中的方法制得复合的Fe2 O3 /TiO2 纳米粒子 .以光催化降解甲胺磷研究其光催化活性 ,并通过XRD、TEM、DRS等分析方法 ,探讨了影响其光催化活性的原因 .结果表明 ,Fe2 O3 的复合量对Fe2 O3 /TiO2 的活性影响很大 ,当n(Fe)∶n(Ti) <0 .3%时 ,复合物Fe2 O3 /TiO2 的光催化活性大于TiO2 ,最佳的复合量为0 .2 % .当复合量大于 0 .5 %时 ,复合物Fe2 O3 /TiO2 的光催化活性低于TiO2 .锻烧温度及锻烧时间对复合物Fe2 O3 /TiO2 光催化活性均有影响 .用XRD确定掺杂前后TiO2 的晶型均为锐钛矿型 ,当复合量大于 0 .7%时才能看到Fe2 O3 的衍射峰 .TEM照片表明 ,由于复合量小 ,复合前后颗粒直径和晶粒直径基本一致 .反射率光谱图表明 ,在 36 0～ 6 5 0nm范围内复合物Fe2 O3 /TiO2 吸收光的性能比TiO2 好 ,亦即增强了对可见光的吸收     

水中痕量铁测定方法的研究

基于Fe3+对KIO4氧化紫脲酸胺 (MX)褪色的催化效应 ,建立了一个催化动力学光度法测定水中痕量Fe3+的新体系 ;该方法具有较好稳定性和选择性 ,Fe3+的浓度在 4× 1 0 - 9～ 3.2×1 0 - 7g/ml范围内与体系的褪色效应成良好线性相关 ,检出限为 1 .0× 1 0 - 9g/mlFe3+;RSD≤ 2 .1% (c=5× 1 0 - 8g/ml,n =1 1 ) ;该方法用于化学试剂和水样中Fe3+测定效果比较满意     

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