碳钠钙铀矿的成矿实验研究
DOI:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:


Experimental Researches on the Formation of Andersonite
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    本文介绍了碳钠钙铀矿的合成原理,并介绍了在18℃、37℃、60℃、80℃、92℃下的合成实验过程。然后,对合成的碳钠钙铀矿进行了X射线粉晶衍射分析、化学分析、差热分析、热失重分析、光性鉴定及红外光谱分析。此外,对合成碳钠钙铀矿还进行了荧光光谱研究及碳钠钙铀矿成矿母液pH值范围及成矿过程中pH值变化实验。该实验表明:母液稳定pH值范围为7.22—9.30,能形成碳钠钙铀矿的母液值范围为8.00—9.30,结晶形成过程中,母液pH值向一个很窄的pH值范围靠拢,即pH为8.00—8.25。

    Abstract:

    According to the crystal-chemical formula of andersonite, i. e., Na2Ca[UO2 (C03)3]6H20, the synthesis of andersonite was completed under the condition of oom temperature and one atmosphere by using uranyl nitrate, anhydrous sodi- um carbonate and calcium nitrate. Later, the same mineral was also synthesi- zed at 37℃,60℃, 80℃ and 92℃ . Besides, experiments on pH stable range for the formation of andersonite at room temperature and under one atmosphere were performed. It has been observed that the pH values for the stableness of the parent solutions range from 7.22 to 9.30, and the pH values for the for- mation of andersonite range from 8.00 to 9.30. During crystallization the pH values of original solutions vary within a narrow range(8.00-8.25) .Such pheno- mena of andersonite as their fluorescence spectra and variation in fluorescence intensity were studied at room and lower temperatures.

    参考文献
    相似文献
    引证文献
引用本文

沈才卿,1988,碳钠钙铀矿的成矿实验研究[J].岩石矿物学杂志,7(1):79~88. Shen Caiqing,1988,Experimental Researches on the Formation of Andersonite[J]. Acta Petrologica et Mineralogica,7(1):79~88.

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:
  • 最后修改日期:
  • 录用日期:
  • 在线发布日期:
  • 出版日期: