CAJ | 학술논문

针对某低品位硫化铜矿进行工艺矿物学研究，结果表明，该铜矿石矿物成分复杂，主要原生硫化铜矿物为黄铜矿，次生硫化铜矿物为铜蓝和少量辉铜矿、砷黝铜矿，氧化铜矿物为黑铜矿；脉石矿物以石英、绿帘石、石榴石、透辉石、透闪石、绿泥石、绢云母、长石为主。原矿含铜0．55％，铜在原生硫化铜和次生硫化铜矿物中的分布率分别为42．18％和36．36％。黄铜矿为细～微细粒不均匀嵌布，粒度集中在0．01～0．16 mm；铜蓝嵌布粒度则集中在0．02～0．16 mm。由于部分硫化铜矿物常和石英、磁黄铁矿共生，选择合理的磨矿细度，使细粒嵌布的铜矿物充分单体解离是本矿石获得较好选矿指标的关键。
침대모저품위류화동광진행공예광물학연구，결과표명，해동광석광물성분복잡，주요원생류화동광물위황동광，차생류화동광물위동람화소량휘동광、신유동광，양화동광물위흑동광；맥석광물이석영、록렴석、석류석、투휘석、투섬석、록니석、견운모、장석위주。원광함동0．55％，동재원생류화동화차생류화동광물중적분포솔분별위42．18％화36．36％。황동광위세～미세립불균균감포，립도집중재0．01～0．16 mm；동람감포립도칙집중재0．02～0．16 mm。유우부분류화동광물상화석영、자황철광공생，선택합리적마광세도，사세립감포적동광물충분단체해리시본광석획득교호선광지표적관건。
The process mineralogy of a low grade sulfide copper ore was researched in this paper. The results show that mineral compositions of the copper ore are complex and chalcopyrite is primary sulfide copper mineral, while the secondary sulfide copper minerals are covellite and a spot of chalco-cite and tennantite,and tenorite is the main oxidized copper mineral .The main gangue minerals are quartz, epidote, garnet, diopside, tremolite, chlorite, sericite and feldspar.The grade of copper in raw ore is 0.55%and the distributions of Cu in primary and secondary sulfide copper are 42.18%and 36.36%respectively.Chalcopyrite is finely-microfinely uneven disseminated between 0.01 mm and 0 .16 mm, while chalcocite is between 0.02 mm and 0.16 mm.As the copper minerals partly in-tergrow with quartz and pyrrhotine, choosing a reasonable grinding fineness to ensure full liberation of the fine-disseminated copper minerals is the key to obtain a good beneficiation indexes.