中国有色金属学报(英文版)
中國有色金屬學報(英文版)
중국유색금속학보(영문판)
TRANSACTIONS OF NONFERROUS METALS SOCIETY OF CHINA
2015年
1期
303-313
,共11页
赵红波%胡明皓%李旖旎%朱珊%覃文庆%邱冠周%王军
趙紅波%鬍明皓%李旖旎%硃珊%覃文慶%邱冠週%王軍
조홍파%호명호%리의니%주산%담문경%구관주%왕군
黄铜矿%斑铜矿%电化学溶解%酸性培养基%细菌浸出
黃銅礦%斑銅礦%電化學溶解%痠性培養基%細菌浸齣
황동광%반동광%전화학용해%산성배양기%세균침출
chalcopyrite%bornite%electrochemical dissolution%acid culture medium%bioleaching
采用电化学测试和X射线光电子能谱(XPS)测试分析黄铜矿与斑铜矿在酸性细菌培养基中的电化学溶解过程。斑铜矿直接氧化反应比还原反应更容易发生,但黄铜矿既难被氧化,又难被还原。斑铜矿具有更高的氧化速率,从而比黄铜矿更容易被溶解。铜蓝(CuS)是黄铜矿与斑铜矿溶解过程的中间产物。因此,斑铜矿的溶解途径主要为直接氧化过程,中间产物铜蓝(CuS)可能限制其进一步溶解。黄铜矿的溶解途径包含了还原?氧化过程,其中,黄铜矿首先被还原为与斑铜矿类似的中间产物,再进一步被氧化,并产生铜蓝(CuS),而黄铜矿的最初还原过程是其溶解过程的主要限制步骤。
採用電化學測試和X射線光電子能譜(XPS)測試分析黃銅礦與斑銅礦在痠性細菌培養基中的電化學溶解過程。斑銅礦直接氧化反應比還原反應更容易髮生,但黃銅礦既難被氧化,又難被還原。斑銅礦具有更高的氧化速率,從而比黃銅礦更容易被溶解。銅藍(CuS)是黃銅礦與斑銅礦溶解過程的中間產物。因此,斑銅礦的溶解途徑主要為直接氧化過程,中間產物銅藍(CuS)可能限製其進一步溶解。黃銅礦的溶解途徑包含瞭還原?氧化過程,其中,黃銅礦首先被還原為與斑銅礦類似的中間產物,再進一步被氧化,併產生銅藍(CuS),而黃銅礦的最初還原過程是其溶解過程的主要限製步驟。
채용전화학측시화X사선광전자능보(XPS)측시분석황동광여반동광재산성세균배양기중적전화학용해과정。반동광직접양화반응비환원반응경용역발생,단황동광기난피양화,우난피환원。반동광구유경고적양화속솔,종이비황동광경용역피용해。동람(CuS)시황동광여반동광용해과정적중간산물。인차,반동광적용해도경주요위직접양화과정,중간산물동람(CuS)가능한제기진일보용해。황동광적용해도경포함료환원?양화과정,기중,황동광수선피환원위여반동광유사적중간산물,재진일보피양화,병산생동람(CuS),이황동광적최초환원과정시기용해과정적주요한제보취。
The electrochemical dissolution process of chalcopyrite and bornite in acid bacteria culture medium was investigated by electrochemical measurements and X-ray photoelectron spectroscopy (XPS) analysis. Bornite was much easier to be oxidized rather than to be reduced, and chalcopyrite was difficult to be both oxidized and reduced. The relatively higher copper extraction of bornite dissolution can be attributed to its higher oxidation rate. Covellite (CuS) was detected as the intermediate species during the dissolution processes of both bornite and chalcopyrite. Bornite dissolution was preferred to be a direct oxidation pathway, in which bornite was directly oxidized to covellite (CuS) and cupric ions, and the formed covellite (CuS) may inhibit the further dissolution. Chalcopyrite dissolution was preferred to be a continuous reduction?oxidation pathway, in which chalcopyrite was initially reduced to bornite, then oxidized to covellite (CuS), and the initial reduction reaction was the rate-limiting step.