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An investigation on the thermodynamics and kinetics of magnesium hydride decomposition based on isotope effects

机译:基于同位素效应的氢化镁分解热力学和动力学研究

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摘要

This work investigates the thermodynamics and kinetics of magnesium hydride decomposition by analyzing isotope effects in hydride and deuteride samples. Complete pressure composition desorption isotherm measurements of MgD_2 are reported for the first time. Deuterium desorption enthalpy and entropy obtained from the van't Hoff plot of the middle plateau fugacities are 73.8 ± 0.4 kJ/mol and 135.5 ± 0.6 J/mol K, respectively, which are in good accordance with the values obtained more than fifty years ago from plateau pressure measurements. This result reveals that the enthalpy of desorption of MgD_2 is slightly lower than that of MgH_2, whereas the entropy change is higher for the deuteride than for the hydride. Although the differences in the enthalpy and entropy of both isotopes are weak, the synergy of both effects is capable of explaining the higher equilibrium pressures for the deuteride than for the hydride. On the other hand, kinetics of magnesium hydride decomposition has been investigated by simultaneous H and D desorption experiments from mixed hydride-deuteride samples. The obtained results reveal that that decomposition is controlled by the nucle-ation and growth of the Mg phase. Because this reaction step is not affected by the isotopic replacement of H for D no isotope effect is observed in the kinetics of magnesium hydride decomposition. On the contrary, a marked isotope effect is observed in the kinetics of H_2(D2) absorption by magnesium. In this case, the lighter isotope shows faster kinetics than the heavier one, what has been related to the fact that absorption is rate limited by H(D) diffusion through the hydride(deuteride) phase.
机译:这项工作通过分析氢化物和氘代样品中的同位素效应来研究氢化镁分解的热力学和动力学。首次报道了MgD_2的完全压力成分解吸等温线测量。从中部高原松散度的Van't Hoff图获得的氘解吸焓和熵分别为73.8±0.4 kJ / mol和135.5±0.6 J / mol K,与五十多年前获得的值相符从高原压力测量该结果表明,MgD_2的解吸焓略低于MgH_2,而氘代的熵变高于氢化物。尽管两种同位素在焓和熵上的差异均较弱,但两种作用的协同作用能够解释氘化氢的平衡压力高于氢化物的平衡压力。另一方面,已经通过同时进行的氢化物和氘化氢样品的H和D解吸实验研究了氢化镁的分解动力学。所得结果表明,分解受Mg相的成核和生长控制。由于该反应步骤不受D的H同位素取代的影响,因此在氢化镁分解动力学中未观察到同位素效应。相反,在镁吸收H_2(D2)的动力学中观察到了明显的同位素效应。在这种情况下,较轻的同位素显示出比较重的同位素更快的动力学,这与以下事实有关:吸收受H(D)通过氢化物(氘代)相扩散的速率限制。

著录项

  • 来源
    《International journal of hydrogen energy》 |2011年第14期|p.8351-8357|共7页
  • 作者单位

    Departamento Fisica de Materiales, Universidad Autonoma de Madrid, Cantoblanco, 28049 Madrid, Spain;

    Departamento Fisica de Materiales, Universidad Autonoma de Madrid, Cantoblanco, 28049 Madrid, Spain;

    Departamento Fisica de Materiales, Universidad Autonoma de Madrid, Cantoblanco, 28049 Madrid, Spain;

    Departamento Fisica de Materiales, Universidad Autonoma de Madrid, Cantoblanco, 28049 Madrid, Spain;

    Departamento Fisica de Materiales, Universidad Autonoma de Madrid, Cantoblanco, 28049 Madrid, Spain;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    hydrogen absorbing materials; metal hydrides; gas-solid reactions; thermodynamic properties; kinetics;

    机译:吸氢材料金属氢化物;气固反应热力学性质;动力学;
  • 入库时间 2022-08-18 00:28:54

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