995 resultados para Mo(v)
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A new compound, (CH5N2)(3)(PMo12O40CH4N23H2O)-C-.-H-. (1), was synthesized and structurally characterized by elemental analyses, IR spectra, UV spectra, NMR spectra and ESR spectra. This is, to our knowledge, the first example of an imidazole-polyoxometalate species. The compound was recrystallized from N,N-dimethylformamide (DMF), and then black block-like crystals of (C3H5N2)(4)((PMoMo11O40)-Mo-V-O-VI)(.)4C(3)H(7)NO(.) 2H(2)O (2), were obtained. It crystallizes in a triclinic space group P (1) over bar with n=12.423(3) Angstrom, b=12.666(3) Angstrom, c=13.341(3) Angstrom, alpha=70.56(3)degrees, beta=71.16(3)degrees, gamma=64.18(3)degrees, V= 1742.3(6) Angstrom(3), Z=1, R1 = 0.0585, wR2 = 0.1885. An X-ray crystallographic study showed that the crystal structure is constructed by electrostatic attractions and hydrogen bonds between a dodecamolybdophosphoric anion and an imidazole. The imidazole and DMF molecules occupy cavities in a polyoxometalate lattice ordered along a c-axis. The structure of (2) is similar to that of (1) from a comparison of both IR spectra and TGA Curves.
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In this paper, we will report the preparation of a mixed-valence polyoxometalate compound (Bu4N)(4)[PMo12O40].2DMF.H2O (TBA = tetrabutylammonium; DMF = N,N-dimethyl formamide). The title compound has been photochemically synthesized and characterized by using elemental analysis, IR, solid diffusion reflectance electronic spectra, ESR spectra, XPS, CV and X-ray single-crystal analysis. The crystal lographic data are as follows: monoclinic, P2(1)/c, a = 14.124(3), b = 17.481(4), c = 22.744(5) Angstrom, beta = 101.66(3)degrees, V = 5500(2) Angstrom(3), C70H160Mo12N6O43P, M-r = 2956.29, Z = 2, D-c = 1.785 g/cm(3), F(000) = 2970 and mu(MoKalpha) = 1.412 mm(-1). The structure has been refined to R = 0.0638 and wR = 0.1975 by full-matrix least-squares methods. The title compound is composed of four tetrabutylammonium cations, one [(PMoMo11O40)-Mo-V](4-) heteropoly anion, two N,N-dimethyl formamide and one H2O molecule.
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[NH3CH2CH2CH2NH2][NH3CH2CH2CH2NH3](2)[(As2AsMo8V4O40)-As-III-Mo-V-O-IV].3H(2)O was hydrothermally synthesized and structurally characterized by single crystal X-ray diffraction. Crystal data: monoclinic, C2/c, a = 45.375(9) Angstrom, b = 11.774(2) Angstrom, c = 23.438(5) Angstrom, beta = 96.62(3)degrees. X-ray crystallographic study showed that the crystal structure was constructed by bicapped alpha-Keggin fragments [(As2AsMo8V4O40)-As-III-Mo-V-O-IV](5-) polyoxoanion. The title compound had a high catalytic activity for the oxidation of benzaldehyde to benzoic acid using H2O2 as oxidant in a liquid-solid biphase system.
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A compact non-stoichiometric molybdenum (VI, V) oxide of blue film was grown on carbon fiber (CF) microelectrode surface be cycling the potential between + 0.2V and - 0.70V in a freshly prepared Na2MoO4 solution containing 5 x 10(-3) mol/L H2SO4. The quantity-of the oxide is controlled by the charge passing the electrode. The electrochemical pretreatment of CF microelectrode not only mises the deposition velocity of molybdenum oxide on CF surface, but also improves greatly the cyclic voltammetric behavior of the molybdenum oxide film prior to the electrodeposition. The cathodic processes are believed to yield the hydrogen molybdenum oxide bronzes HxMoO3(0 < x < 2), or substoichiometric lower molybdenum oxides with the formula MoO3-y(0 < y < 1). The anodic response results from the reversible oxidation of molybdenum bronze/Mo(V) centers [or perhaps Mo(IV) in more reduced coatings], to Mo(VI). Further information was gained about the chemical composition and valent state of Mo from XPS and SEM.
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本文采用苯甲酰苯胲(BPHA)-甲基异丁基酮(MIBK)溶剂萃取方法将钢中基体元素Fe,Ti,Mo,V等大量非稀土元素萃入有机相中,稀土元素留于水溶液中.由电感耦合等离子体原子发射光谱(ICP-AES)仪直接测定水溶液中的微量稀土元素La,Ce,Pr,Nd.Sm,Y和Gd,实验结果与推荐值基本相符,方法的回收率为96%~108%,相对标准偏差低于5%.
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In this paper the electrochemical properties of isopolymolybdic anion thin film modified carbon fibre (CF) microelectrode prepared by simple dip coating have been described. The modified electrode shows three couples of surface redox waves between + 0.70 and - 0.1 V vs. sce in 2 M H2SO4 solution with good stability and reversibility. The pH of solution has a marked effect on the electrochemical behaviour and stability of the film, the stronger the acidity of electrolyte solution is, the better the stability and reversibility of isopolymolybdic anion film CF microelectrode will be. The scanning potential range strongly influences on the electrochemical behaviour of the film. The isopolymolybdic anion film prepared by the dip coating resulting a monolayer with estimated surface concentration (F) 2.8 x 10(-11) mol cm-2. From the half-peak widths and peak areas of the surface redox waves of the film electrode, the first three surface waves are corresponding to two-electron processes. The electron energy spectra show the products by six electrons reduction are a mixture of Mo(VI) and Mo(V) species. The electrochemical reaction of the isopolymolybdic anion monolayer can be expressed as Mo8O264- + mH+ + 2ne half arrow right over half arrow left [HmMo8-2n(VI)Mo2n(V)O26](4,2n-m)-n = 1, 2, 3; m = 2, 5, 7.
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本文用控制阴极电位电解还原方法,制得了以Si为杂原子的Keggin结构二电子、四电子杂多蓝K_2H_4[SiMo_2~ⅤMo_(10)~ⅥO_(40)]·12H_20(Ⅰ)和K_3H_5[SiMo_4~ⅤMo_8~ⅥO_(40)]·12H_2O(Ⅱ).通过IR,UV,极谱,XPS,ESR及单晶X射线衍射对所合成的杂多蓝进行了表征,确定了被还原的Mo(V)位置位于不同的边共用三金属簇内,测定结果表明,Keggin结构杂多阴离子还原后,八面体结构有轻微畸变,畸变程度随还原程度增大而增大。
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研究了以Cu~(2+)为催化剂的Mo(V)-SCN~--ERB~+-PVA超高灵敏新显色体系及钼的分光光度测定条件。缔合物的吸收峰在580nm处,表观摩尔吸光系数ε=5.6×10~6L·mol~(-1)·cm~(-1)。Mo(Ⅵ)含量在0~0.3μg/25mL范围内符合比耳定律。初步研讨了显色反应的机理。结合离子交换分离,本法可成功地用于水样及麦饭石浸出液中痕量钼的测定。
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采用低温技术,用 X 射线单晶衍射法测定了标题化合物的结构.晶体属 P4/mnc 空间群,a=12.515(3),c=17.636(7),Z=2.用788个独立可观测反射精修所有结构参数得 R=0.061.钼钒磷杂多酸阴离子中,PO_4四面体是无序的,P—O 键长1.54.M(Mo,V)是6配位,M—O 键长1.62—2.48.K 是7配位,K—O 键长2.84—3.10.
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贵州早寒武世的黑色岩系属中国南方该时期缺氧事件沉积的一部分,为一套沉积速率低的海侵体系域沉积.主要为黑色页岩,发育水平纹理,主要含浮游生物,其中产钼、钒等矿床.其具有独特的元素地球化学特征:SiO2、TiO2、Al2O3的含量相对较高;富集Mo、V、Ba、Ag、Au、U等元素,而Co、Sr、Ta等元素却亏损;稀土总量不高,为130×10-5~226×10-6,稀土配分曲线形态近于水平或略向右倾,具弱的负Ce异常和正Eu异常.地层特征、元素地球化学特征及特征元素比值所反映的是早寒武世黑色岩系形成于缺氧的还原环境,而缺氧沉积中有热水沉积的加入.
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氧化还原敏感元素硒的地球化学循环非常复杂, 它的循环主要受氧化还原势、酸碱度、温度、压力等条件的控制。长期以来,关于硒的主要研究集中在环境生物地球化学领域。对于硒的地质地球化学行为的研究,学者们认为硒不可能独立形成矿床,它主要以伴生元素的形式赋存于一些热液矿床(如,拉尔玛硒-金热液矿床等)。 二十世纪末, 我国学者开始关注硒的矿床地球化学行为, 发现了目前唯一的渔塘坝沉积型的独立硒矿床。另外,下寒武统底部黑色岩系(如,遵义牛蹄塘组)处于地球发展演化的关键时期且富集了众多的有用金属元素, 因此它引起了全世界广大地质学家的普遍关注和重视。这些黑色岩系的共同特点是含有大量的有机质和丰富的金属元素(PGE,Cu,Ni,Mo,Au,U,V,Mn,Fe,Co,Bi,Cr,Se等)。但遵义牛蹄塘组中Ni-Mo多金属层的成因一直争论不休。 本文以拉尔玛硒-金热液矿床、渔塘坝独立硒矿床、遵义黄家湾含Ni-Mo-Se多金属层剖面为研究对象,主要通过硒稳定同位素的测试和不同化学形态的分析结合其他的地球化学参数(如,C-S-Fe体系,氧化还原敏感元素),示踪富硒地层的沉积环境,研究不同地质体系中硒稳定同位素的组成,进而完善硒同位素的理论体系,探讨硒富集过程中的形态迁移途径,并为矿床的形成提供更完善的地球化学证据。通过一系列的研究工作,我们取得了以下几点认识: (1) 通过不同的消解方法准确测定了低硒,高硒样品的总硒含量,相对标准偏差小于10%,而且不同的消解方法测得同样的结果, 满足了地质样品中微量元素的测试要求。由于不同消解方式存在自身的优缺点,我们建议根据不同的样品类型,不同的研究目的选取合适的消解方法。 (2) 通过巯基棉吸附装置达到了纯化富集样品硒的目的, 硒的回收率一般大于90%, 满足同位素测试的需要。应用自制的氢化物发生器与Nu-MC-ICP-MS联用,实现了在线气体进样测试硒稳定同位素的目的。 采用标准样品匹配测试方法校正仪器测试过程中的质量分馏。 硒稳定同位素的测试精度为2δ=0.30‰, 标准NIST SRM 3149采用与样品同样的处理方法,没有发现前处理过程的同位素分馏。 (3) 传统地球化学参数对沉积环境的指示意义。通过氧化还原敏感微量元素及其与TOC的关系和C-S-Fe体系的分析,对渔塘坝独立硒矿床的多元素富集及沉积环境, 遵义黑色岩系沉积环境进行了详细的解释。TS-TFe的关系表明样品中有过量的硫存在,可能为有机硫或为其他亲硫元素提供有利的沉淀条件。C-S-Fe体系及微量元素指数V/(V + Ni) 说明渔塘坝矿区的硅质岩和页岩的沉积环境为缺氧到静海环境, Ni/Co、V/Cr几乎不能作为该区缺氧环境的指示参数, 后者可能由于Cr的外源输入(碎屑、热液等)所致。 C-S-Fe体系及微量元素指数V/(V + Ni)体系指示遵义黑色岩系的沉积环境为微含氧到缺氧的条件, 但对于Ni-Mo矿而言, V/(V + Ni)体系指示其为含氧条件沉积,这可能与Ni-Mo多金属层的成因有关。但铁的硫化度可以指示Ni-Mo多金属层极端的缺氧还原环境。 (4) 硒的形态对古氧化还原条件和矿物质来源的示踪意义。黑色岩系的硒形态分布不同于海洋沉积物,体现了成岩作用对硒形态分布的改变。黑色岩系中硒的主要形态为有机结合态和硫化物/硒化物结合态。硫化物/硒化物结合态比例与铁的硫化程度(DOS)之间明显的相关关系说明在海洋环境中硒主要通过氧化还原反应富集在富有机质的沉积物与沉积岩中。这种相关关系与岩石类型没有关系,这使得将硫化物、硒化物结合的Se(-II)比例作为一个氧化还原条件示踪剂更加可行。DOS与硫化物/硒化物结合态硒的关系,及Se(IV)与Se(-II)的关系均说明遵义牛蹄塘组的K-斑脱岩形成于碱性的氧化环境,Ni-Mo多金属层沉积于微酸性的极端还原环境,而渔塘坝矿床形成于微碱性的还原缺氧环境。生物的同化作用与异化作用之间本身存在互补关系,但这种互补关系却存在不同的转化趋势。不同的转化趋势可能主要受氧化还原反应和酸碱度的控制,其他的地质作用也可能起着重要作用(如,硅酸盐、Fe(II)的含量,硫化物、有机质含量,风化程度等)。同时我们发现相同的氧化还原条件下可能存在不同的富集途径。Ni-Mo多金属层中极少的有机结合态硒暗示海洋同生沉积主要被生物异化还原控制,而沉积物从海洋富集硒的途径主要为直接由Se(VI)和Se(IV)到Se(-II)的还原途径,从高价态到元素态的还原途径可能偶有发生但强度很小。 (5) 硒稳定同位素对矿床成因及物质来源的示踪意义。热液或表生环境中,硒的再次活化迁移对硒同位素的大范围分馏是很重要的。较少的硫化物结合态硒和较大范围的硒同位素组成说明渔塘坝矿床形成时经历了多次氧化还原过程。干酪根硒同位素组成与全岩相似, 而且样品富集轻同位素暗示该矿床硒来的富集主要通过海洋硒的生物吸收同化异化还原与多次无机氧化还原实现。对于拉尔玛金硒矿床而言,未蚀变岩体的硫化物结合态硒富集轻同位素,而后期低温流体的蚀变作用导致蚀变岩体中硫化物结合态硒富集重同位素。干酪根的硒同位素组成暗示热液输入的硒为该矿床硒的主要来源,硒从热液直接进入干酪根的机制是一致的。随着硫含量的增加岩石和矿体中的硒逐渐富集重同位素, 说明海水对矿床富集的贡献是很有限的。遵义黑色岩系中硒同位素组成与Se(-II)之间的关系, 单质硒的缺乏,硒的富集与同位素的关系说明,热液为主要的硒来源,而早寒武世海水中的硒主要通过Se(VI)和Se(IV)到Se(-II)的直接生物还原实现。三个区域的S/Se比值综合说明硫与硒的共同沉降过程中不存在硒的同位素分馏。不同化学形态的分布与不同形态中硒稳定同位素的结合可能会更好的解释硒的全球地球化学循环。 (6) 根据目前硒的同位素分馏体系及所测得的数据,我们初步建立了不同时代、不同成因黑色岩系中硒稳定同位素的分馏模式。
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J Biol Inorg Chem. 2008 Jun;13(5):737-53. doi: 10.1007/s00775-008-0359-6
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Iron, aluminium and mixed iron aluminium pillared clays have been prepared by partial hydrolysis method and doped with IO% Mo, V and Cr. The samples have been characterised by XRD, FTIR and surface area and pore Volume measurements. The surface acid site distribution has been determined by temperature programmed desorption of ammonia. Vanadia incorporated systems show maximum acidity. Benzylation of o-xylene has been done as probe reaction to test catalytic activity. Benzyl chloride is a superior benzylating agent compared to benzyl alcohol in activity and selectivity. Cent percent selectivity towards monobenzylated product is obtained in all the cases. Fe pillared systems exhibit maximum activity. The catalytic activities of the systems can be correlated with the amount of strong add sites. The effects of various reaction variables on the reaction have been studied. Presence of moisture has a diminishing effect on the reaction rate.
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The 15Kh2MFA steel is a kind of Cr-Mo-V family steels and can be used in turbines for energy generation, pressure vessels, nuclear reactors or applications where the range of temperature that the material works is between 250 to 450°C. To improve the properties of these steels increasing the service temperature and the thermal stability is add a second particle phase. These particles can be oxides, carbides, nitrites or even solid solution of some chemical elements. On this way, this work aim to study the effect of addition of 3wt% of niobium carbide in the metallic matrix of 15Kh2MFA steel. Powder metallurgy was the route employed to produce this metallic matrix composite. Two different milling conditions were performed. Condition 1: milling of pure 15Kh2MFA steel and condition 2: milling of 15Kh2MFA steel with addition of niobium carbide. A high energy milling was carried out during 5 hours. Then, these two powders were sintered in a vacuum furnace (10-4torr) at 1150 and 1250°C during 60 minutes. After sintering the samples were normalized at 950°C per 3 minutes followed by air cooling to obtain a desired microstructure. Results show that the addition of niobium carbide helps to mill faster the particles during the milling when compared with that steel without carbide. At the sintering, the niobium carbide helps to sinter increasing the density of the samples reaching a maximum density of 7.86g/cm³, better than the melted steel as received that was 7,81g/cm³. In spite this good densification, after normalizing, the niobium carbide don t contributed to increase the microhardness. The best microhardness obtained to the steel with niobium carbide was 156HV and to pure 15Kh2MFA steel was 212HV. It happened due when the niobium carbide is added to the steel a pearlitic structure was formed, and the steel without niobium carbide submitted to the same conditions reached a bainitic structure
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Conselho Nacional de Desenvolvimento Científico e Tecnológico