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西秦岭铀矿床含矿热液物理化学条件改变对铀沉淀影响
引用本文:何明友.西秦岭铀矿床含矿热液物理化学条件改变对铀沉淀影响[J].矿物岩石,1996,16(2):90-95.
作者姓名:何明友
作者单位:中国科学院地球化学研究所
摘    要:本文研究了西秦岭铀矿床含矿热液物理化学条件的改变对铀沉淀富集的影响。研究表明,铀在相对还原条件下迁移,而在相对氧化条件下沉淀富集。铀的沉淀富集主要发生在含矿热液的温度、压力和氧逸度大幅度降低,酸性增强及氧化-还原电位增高的物理化学条件下。

关 键 词:铀矿床  含铀热液  物理化学条件    沉淀

THE INFLUENCE ON PRECIPITATION OF URANIUM BY THE CHANGES OF PHYSICO-CHEMICAL CONDITIONS OF U-BEARING HYDROTHERMAL SOLUTION IN THE WEST QINLING URANIUM DEPOSITS
He Mingyou.THE INFLUENCE ON PRECIPITATION OF URANIUM BY THE CHANGES OF PHYSICO-CHEMICAL CONDITIONS OF U-BEARING HYDROTHERMAL SOLUTION IN THE WEST QINLING URANIUM DEPOSITS[J].Journal of Mineralogy and Petrology,1996,16(2):90-95.
Authors:He Mingyou
Abstract:The reduction and enrichment of uranium effected by the changes of physico-chemical conditions of U-bearing hydrothermal solution in the west Qinling uranium deposits was studied by. It is indicated that uranium was moved out in the relative reducing condition and enriched precipitation in the relative oxidizing condition. Uranium mineralizing process occurred in the stage of that high temperature and pressure, high fo2 and pH, and low Eh was changed into low temperature and pressure, low fo2 and pH, and high Eh.
Keywords:uranium deposit  U-bearing hydrothermal solution  moving forms of uranium  enrich ment of uranium  physical-chemical conditions  
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