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Redox Equilibria of Transition Metals in Silicate Melts

机译:硅酸盐熔体中过渡金属的氧化还原平衡

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An investigation is carried out at present by ourselves to determine the redox equilibria of titanium, niobium and chromium in calcium-silicate melts at low contents of the transition metals. The results have been discussed in this lecture together with data on vanadium which have been published previously by one of the authors and together with literature data on iron. The slags were equilibrated with gases of controlled oxygen pressure at 1600 鳦, and wet chemical analysis was used, after quenching, to determine the different metal ions. The project is not finished yet and some of the obtained data have to be checked. Nevertheless, it can already be demonstrated that the ratios of the two differently charged species depend on oxygen pressure, within their scatter, with the power required by the oxidation reaction. Increasing CaO/SiO_2 ratio stabilizes the higher valent metalion. The redox equilibria for chromium and vanadium are particularly interesting because ions with three oxidation states (Cr~(2+), Cr~(3+) and Cr~(6+), or V~(3+), V~(4+) and V~(5+)) can coexist in intermediate ranges of oxygen pressure which is very much in contrast to the behavior of these metals in aqueous solutions.
机译:目前我们自己进行研究以确定过渡金属含量低时硅酸钙熔体中钛,铌和铬的氧化还原平衡。该结果已与本报告中的一位作者先前发表的钒数据以及有关铁的文献数据一起讨论过。炉渣在1600鳦下用控制氧气压力的气体平衡,淬火后使用湿化学分析法测定不同的金属离子。该项目尚未完成,必须检查一些获得的数据。然而,已经证明两种带不同电荷的物质的比例取决于其分散内的氧气压力以及氧化反应所需的功率。 CaO / SiO_2比值的增加可稳定较高价的金属离子。铬和钒的氧化还原平衡特别有趣,因为具有三种氧化态(Cr〜(2 +),Cr〜(3+)和Cr〜(6+)或V〜(3 +),V〜(4)的离子+)和V〜(5+))可以共存于氧气压力的中间范围内,这与这些金属在水溶液中的行为形成鲜明对比。

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