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赞比亚某铜矿石工艺矿物学研究
引用本文:孔令采,李正要.赞比亚某铜矿石工艺矿物学研究[J].金属矿山,2015,44(1):72-76.
作者姓名:孔令采  李正要
作者单位:1.新兴发展集团有限公司,北京 100020; 2.北京科技大学土木与环境工程学院,北京 100083
摘    要:赞比亚某铜矿石属结合相占比较高的氧化矿石,铜品位为2.10%,伴生有价元素铁、金、银、钴品位分别为24.20%、0.20 g/t、7.60 g/t、0.05%。为确定该矿石的合理选矿工艺流程,对矿石进行了工艺矿物学研究。结果表明:①该矿石的矿物组成较复杂,主要有用矿物有赤褐铁矿、磁铁矿、磷铜铁矿、绿磷铁铜矿、假孔雀石等。②矿石的构造主要有多孔状、团块状、浸染团粒状、条纹条带状、圈层状、变胶状、晶洞状、细脉状构造;矿石的结构主要有他形粒状结构,隐晶质结构,束状、梳状、柱状结构,交代结构。③磷铜铁矿、绿磷铁铜矿、假孔雀石中的铜分别占总铜的41.03%、40.27%、15.35%,磷铜铁矿、绿磷铁铜矿均为隐晶质集合体,粒度较细,集合体粒度一般均为0.01~0.5 mm,假孔雀石粒度一般为0.01~0.4 mm,少量可达0.8 mm;赤褐铁矿粒度一般为0.01~0.5 mm,少量达4 mm;磁铁矿粒度较大,一般为0.1~0.2 mm。因此,该铜矿石属难选多金属氧化矿石。

关 键 词:铜矿石  磷铜铁矿  绿磷铁铜矿  假孔雀石  赤褐铁矿  磁铁矿  工艺矿物学  

Study on Process Mineralogy for a Copper Ore in Zambia
Kong Lingcai,Li Zhengyao.Study on Process Mineralogy for a Copper Ore in Zambia[J].Metal Mine,2015,44(1):72-76.
Authors:Kong Lingcai  Li Zhengyao
Affiliation:1.Xinxing Development Group Co.,Ltd.,Beijing 100020,China;2.School of Civil and Environment Engineering,University of Science and Technology Beijing,Beijing 100083,China
Abstract:A certain copper ore in Zambia is a kind of oxidized ore with high proportion of combined phases,in which the grade of copper is 2.10%,and grade of other associated valuable elements such as Fe,Au,Ag,and Co are 24.20%,0.20 g/t,7.60 g/t,and 0.05% respectively.In order to determine the proper beneficiation process,study on process mineralogy of this copper ore was made.The results show that ①the mineral composition is complex and the main useful minerals include hematite-limonite,magnetite,chalcosiderite,green chalcosiderite,pseudo-malachite and so on.②the mineral structures mainly include vesicular,crumby,disseminated granular,riband-striped,circle-like,metacolloform,miarolitic,and veinlet structures,the mineral textures mainly include xenomorphic granular,cryptocrystalline,sarciniform,pectination,columnar and metasomatic.③copper in chalcosiderite,green chalcosiderite and pseudo-malachite account for 41.03%,40.27%,and 15.35% of the total copper respectively.Chalcosiderite and green chalcosiderite are all cryptocrystalline aggregation with particle size of 0.01~0.5 mm.The particle size of pseudo-malachite is generally within the range from 0.01 to 0.4 mm,and few reach up to 0.8 mm.The particle size of hematite-limonite is generally within the range from 0.01 to 0.5 mm,and few reach up to 4 mm.The particle size of magnetite is larger,which is generally within the range from 0.1 to 0.2 mm.Therefore,this kind of copper ore belongs to refractory multi-metal oxidized ore.
Keywords:Copper ore  Chalcosiderite  Green chalcosiderite  Pseudo-malachite  Hematite-limonite  Magnetite  Process mineralogy
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