首页> 外文会议>International Biohydrometallurgy Symposium, IBS-2001 Sep 16-19, 2001, Ouro Preto, Minas Gerais, Brazil >Bioleaching of a Mixed Copper Sulfide Ore Containing Enargite and Luzonite
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Bioleaching of a Mixed Copper Sulfide Ore Containing Enargite and Luzonite

机译:含堇青石和绿宝石的混合硫化铜矿的生物浸出

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The Nena deposit of the currently undeveloped Frieda River copper project in Papua New Guinea contains the copper minerals chalcocite (Cu_2S), covellite (CuS), enargite (Cu_3AsS_4), and luzonite (a dimorph of enargite), along with significant amounts of pyrite (FeS_2). This study was done to determine if the ore and a flotation concentrate could be bioleached and if copper was extracted selectively from certain of the minerals. Shake flask tests were done at 25℃ with Acidithiobacillus-Leptospirillum-type bacteria and at 50℃ with mixed, moderately thermophilic sulfide-oxidizing bacteria. Copper extraction by Acidithiobacillus-Leptospirillum bacteria was 56% from the ore (particle size minus 10 mesh) and 47% from the concentrate (P_(80) 20um). Thermophilic bacteria extracted somewhat more copper, amounting to 65% from the ore and 62% from the concentrate. About 20% to 25% of the arsenic in the ore and in the concentrate was extracted when pyrite was oxidized at high solution redox potential. However, it does not appear that arsenic was released from the enargite/luzonite, based on microscopy of polished sections and because arsenic was extracted into solution in the absence of copper extraction. Bioleaching of Frieda River ore and concentrate, especially with thermophilic bacteria, extracted most of the chalcocite and covellite but extracted little of the enargite/luzonite. The source of the extracted arsenic remains uncertain and requires further investigation. Some deposits of enargite may be refractory to bioleaching.
机译:巴布亚新几内亚目前未开发的弗里达河铜项目的尼娜矿床包含铜矿物辉铜矿(Cu_2S),铜锌矿(CuS),顽辉石(Cu_3AsS_4)和绿宝石岩(顽辉石的二形体),以及大量的黄铁矿( FeS_2)。进行这项研究是为了确定矿石和浮选精矿是否可以进行生物浸出,以及是否从某些矿物中选择性提取了铜。摇瓶试验是在25℃下对嗜酸硫杆菌属-细螺旋体型细菌进行的,而在50℃对混合的中等嗜热的硫化物氧化菌进行的。酸性硫杆菌-细螺旋体细菌的铜提取量为矿石的56%(粒径减去10目),精矿中的铜含量为47%(P_(80)20um)。嗜热细菌从铜矿中提取了更多的铜,分别占矿石的65%和精矿的62%。当黄铁矿在高溶液氧化还原电势下被氧化时,矿石和精矿中约20%至25%的砷被提取。然而,基于抛光切片的显微镜,并且由于砷在没有铜萃取的情况下被萃取到溶液中,因此似乎没有从辉石/绿宝石释放出砷。弗里达河矿石和精矿的生物浸出,尤其是嗜热细菌的浸出,提取了大部分的辉绿岩和陨石,但几乎没有提取到浮辉岩/绿宝石。提取的砷的来源仍然不确定,需要进一步调查。镁矿的某些沉积物可能难以生物浸出。

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