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PREPARATION AND PROPERTIES OF PALLADIUM AND PLATINUM SUPPORTED ON LAYER SILICATE MINERALS

机译:层状硅酸盐矿物上钯和铂的制备及其性能

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摘要

The addition of molecular hydrogen at 140(DEGREES)C to Pd(NH(,3))(,4)('2+) and Pt(NH(,3))(,4)('2+) complexes exchanged on Wyoming montmorillonites, at various metal weight to support weight ratios, results in metal reduction according to the mechanism M(NH(,3))(,4)('2+) + H(,2) (--->) M(DEGREES) + 2NH(,4)('+) + 2NH(,3). In a parallel reaction, the concurrent reduction of structural iron (III) occurs, producing an increase in the layer charge of the mineral. Charge balance is maintained by the additional formation of ammonium cations by ammine protonation.;Metal reduction is accompanied by the collective migration of atoms and/or crystallites from the internal surface of the mineral to sites, on the external surface and edges, of low negative charge. At high metal concentrations, large clusters of > 100(ANGSTROM) are easily visible by transmission electron microscopy. Also apparent is a high proportion of the metal crystallites formed in diameters of 50(ANGSTROM) or less. As the metal concentration decreases, mean metal diameters decrease and the particle size distributions become narrower.;Attempts to measure metal dispersions (number of surface metal atoms/total number of metal atoms) by the hydrogen titration of oxygenated surface metal atoms result in a drastic overestimation of this value. The primary cause appears to be related to the spillover of atomic hydrogen from the metal to the support phase. Infrared evidence exists which implicates the role of structural iron, present in the montmorillonite support, as hydrogen atom acceptor sites. Molecular water, formed during the titration reaction, also appears to be involved in the process, acting as a carrier for hydrogen atoms between the metal surface and the acceptor sites.;Values, more indicative of the actual metal dispersion, are obtainable by measuring the gravimetric loss of water after the initial hydrogen titration. This technique offers a simple and convenient method for determining metal dispersion independent of hydrogen spillover.;Finally, the catalytic activity of palladium loaded montmorillonites is demonstrated for the hydrogenation of 1-hexene. The higher specific activity of these catalysts compared to a 5.0% Pd(.)Al(,2)O(,3) would indicate the manifestation of hydrogen spillover once again.
机译:在140(DEGREES)C上将分子氢加到交换上的Pd(NH(,3))(,4)('2+)和Pt(NH(,3))(,4)('2+)络合物上怀俄明州蒙脱土在各种金属重量与支撑重量比下,根据机理M(NH(,3))(,4)('2+)+ H(,2)(-)M导致金属还原(度数)+ 2NH(,4)('+)+ 2NH(,3)。在平行反应中,同时发生结构铁(III)的还原,从而增加了矿物的层电荷。通过胺的质子化作用额外形成铵阳离子,从而保持电荷平衡。金属还原伴随着原子和/或微晶从矿物内表面向低负离子外表面和边缘位置的集体迁移。收费。在高金属浓度下,透射电子显微镜很容易看到大于100(ANGSTROM)的大簇。同样明显的是形成直径为50(或更小的金属微晶。随着金属浓度的降低,平均金属直径减小并且粒度分布变窄。;尝试通过氧化表面金属原子的氢滴定法测量金属分散度(表面金属原子数/金属原子总数)会导致剧烈的高估了这个值。主要原因可能与氢原子从金属到载体相的溢出有关。存在红外证据暗示存在于蒙脱石载体中的结构铁作为氢原子受体位点的作用。滴定反应过程中形成的分子水似乎也参与了该过程,充当了金属表面和受体位点之间氢原子的载体。初始氢滴定后重量失水。该技术提供了一种简便而又便捷的测定金属分散度的方法,而与氢的溢出无关。最后,证明了负载钯的蒙脱石对1-己烯加氢的催化活性。与5.0%Pd(。)Al(,2)O(,3)相比,这些催化剂具有更高的比活度,这表明氢再次溢出。

著录项

  • 作者

    HARRISON, JEFFREY BAKER.;

  • 作者单位

    University of Florida.;

  • 授予单位 University of Florida.;
  • 学科 Inorganic chemistry.
  • 学位 Ph.D.
  • 年度 1982
  • 页码 89 p.
  • 总页数 89
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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