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Short communications Analytic calculation of cation distribution equilibria in the cubic phase of jacobsite-hausmannite system

机译:短通信雅克贝斯-菱锰矿体系立方相中阳离子分布平衡的解析计算

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摘要

Cation and cation vacancy distribution equilibria in the cubic phase of jacobsite-hausmannite solid solution system have been calculated by a defect-chemical approach as a function of some equilibrium constants, partial pressure of oxygen Po_2 and compositional ratio x in Mn_xFe_(3-x)O_4 (x = 1 to 3). The concentration of metal vacancy was zero and a considerable amount of Fe~(2+) in the octahedral site, which was equal to Fe~(3+) in the tetrahedral site, appeared in case of appropriate values of equilibrium constants and small values of Po_2. The distribution results in a fairly good agreement with the reported Moessbauer spectroscopic data. In spite of constant metal ratio, the concentraion of Fe~(2+) is lessened with increasing Po_2 and metal vacancy in the tetrahedral site appeared considerably. These results suggest that the estimation of temperature and Po_2 for formation of natural specimen is possible from the observed values of cation distribution, if some thermodynamic values are known.
机译:通过缺陷化学方法,根据某些平衡常数,氧Po_2的分压和Mn_xFe_(3-x)中的组成比x,通过缺陷化学方法计算了雅克贝-钙锰矿固溶体系统立方相中的阳离子和阳离子空位分布平衡O_4(x = 1至3)。金属空位的浓度为零,八面体部位的Fe〜(2+)的数量与四面体部位的Fe〜(3+)相当,如果平衡常数的取值适当而取小,则出现的Po_2。分布结果与报告的Moessbauer光谱数据相当吻合。尽管金属比例恒定,但随着Po_2的增加,Fe〜(2+)的浓度降低,并且四面体位点中的金属空位明显增加。这些结果表明,如果已知一些热力学值,则可以根据观察到的阳离子分布值来估算用于形成天然样品的温度和Po_2。

著录项

  • 来源
    《Mineralogical Journal》 |1995年第8期|p.372-377|共6页
  • 作者单位

    Department of Earth and Planetary Sciences, Graduate School of Science, Hokkaido University, Sapporo 060, Japan;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 矿物学;
  • 关键词

  • 入库时间 2022-08-18 00:24:26

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