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A method for controlling alkali-metal oxide activities in one-atmosphere experiments and its application to measuring the relative activity coefficients of NaO0.5 in silicate melts

机译:一种控制大气中碱金属氧化物活性的方法及其在测量硅酸盐熔体中NaO0.5相对活性系数中的应用

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摘要

The activity of alkali metal oxides can be controlled in one-atmosphere wire-loop experiments at high temperature by suspending a crucible containing alkali silicate melt beneath the samples. The method has been applied to measuring the activity coefficient of NaO0.5 in a series of CMAS-NaO0.5 melts relative to that in the anorthite-diopside eutectic composition at 1400 °C, using a reservoir of NaO0.5-SiO2 melt. The results show that this relative activity coefficient decreases strongly with SiO2, increases with CaO and MgO, but is insensitive to AlO0.5. This latter behavior is inconsistent with "quasi-crystalline" models of melt thermodynamics that hypothesize Na-Al species.
机译:可以通过在样品的下面悬浮含坩埚的碱金属硅酸盐熔体,在高温的一个大气压线环实验中控制碱金属氧化物的活性。 方法已用于测量一系列CMAS-NaO 0.5 熔体中NaO 0.5 的活度系数使用NaO 0.5 -SiO 2 储层相对于钙长石-透辉石 共晶成分的相对含量sup>融化。结果表明,相对活性系数 随SiO 2 强烈下降,随CaO和MgO增大,但 对AlO <0.5>不敏感。后一种行为与 假设Na-Al物种的熔融热力学的“准晶体”模型不一致。

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  • 来源
    《American Mineralogist》 |2005年第3期|00000497-00000501|共5页
  • 作者

    Hugh St. C. O’Neill;

  • 作者单位

    Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia;

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  • 正文语种 eng
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