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纳米金的迁移富集与黄铁矿富金关系

TRANSPORT AND ENRICHMENT OF NANOMETER SIZED GOLD IN RELATION TO GOLD RICH PYRITE

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【作者】 姜泽春章振根莫德明陈大梅

【Author】 Jiang Zechun Zhnag Zhengen Mo Deming Chen Damei (Institute of Geochemistry,Chinese Academy of Sciences,Guiyang,550002)

【机构】 中国科学院贵阳地球化学研究所

【摘要】 黄铁矿是金矿床中常见的矿物,也是重要的载金矿物之一,有的黄铁矿富金,有的黄铁矿不含金或含微量金。为什么黄铁矿对纳米金的吸附作用强?讨论了纳米微粒金与黄铁矿的关系后指出,半导体型黄铁矿有N型和P型两种。前者具负热电动势、带负电;后者具正电位带正电荷。当其与SiO2水溶液迁移时,若与带正电荷的P型黄铁矿相遇,即被P型黄铁矿吸附沉淀成矿。带负电荷的黄铁矿不能吸附带负电荷的纳米金,因而不能成矿。

【Abstract】 Pyrite is a common mineral in gold ore deposits and one of the important gold rich minerals.Some pyrites are rich in gold and other contain no or a trace amount of gold.Why does pyrite have such a strong capacity of adsorbing nanometer sized gold? The paper discusses the relation between nanometer sized gold and pyrite,it points out that there are two types of semiconductive pyrite:N pyrite and P pyrite.The former with negative charge is possessed of negative thermoelectromotive force;the latter with positive charge is possessed of the positive thermoelectromotive force.When nanometer sized gold is transported with aqueous solution of silicondioxide and encountered with P pyrite,it will be adsorbed on pyrite,followed by ore deposition.N pyrite with negative charge can not adsorbnanometer sized gold with negative charge,and therefore no gold deposition would occur.

【基金】 自然科学基金
  • 【文献出处】 矿产与地质 ,MINERAL RESOURCES AND GEOLOGY , 编辑部邮箱 ,1998年06期
  • 【分类号】P618.510.1
  • 【被引频次】8
  • 【下载频次】211
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