硫砷铜矿化学浸出动力学研究
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:Kinetics of Enargite Chemical Leaching
  • 作者:伍赠玲 ; 吴智 ; 朱永官
  • 英文作者:Wu Zengling;Wu Zhi;Zhu Yongguan;Key Laboratory of Urban Environment and Health,Institute of Urban Environment,Chinese Academy of Sciences;State Key Laboratory of Comprehensive Utilization of Low-Grade Refractory Gold Ores,Zijin Mining Group Co. Ltd.;
  • 关键词:硫砷铜矿 ; 浸出动力学 ; 活化能 ; 温度 ; 氧化还原电位
  • 英文关键词:enargite;;leaching kinetics;;activation energy;;temperature;;redox potential
  • 中文刊名:ZXJS
  • 英文刊名:Chinese Journal of Rare Metals
  • 机构:中国科学院城市环境研究所城市环境与健康重点实验室;紫金矿业集团股份有限公司低品位难处理黄金资源综合利用国家重点实验室;
  • 出版日期:2015-04-07 09:27
  • 出版单位:稀有金属
  • 年:2015
  • 期:v.39;No.233
  • 基金:国家自然科学基金项目(51474075);; 福建省科技厅区域重大项目(2013H4020)资助
  • 语种:中文;
  • 页:ZXJS201508010
  • 页数:6
  • CN:08
  • ISSN:11-2111/TF
  • 分类号:69-74
摘要
模拟生物堆浸工艺条件,在硫酸铁酸性介质体系下,进行硫砷铜矿化学浸出动力学实验研究。硫砷铜矿化学性质稳定,在初始Fe3+浓度31 g·L-1,Fe2+浓度0.02 g·L-1,初始p H=1.00±0.05,氧化还原电位恒定在(900±5)m V,30℃条件下浸出96 h,硫砷铜矿的浸出率仅有2.49%。不同电位对硫砷铜矿浸出的影响结果表明,硫砷铜矿的浸出率与电位呈弱正相关,30,45,60,75℃时硫砷铜矿的浸出率与电位的关联指数分别为0.0037,0.0053,0.0062,0.0120。低温下电位对溶解速率影响很小,高温下较显著。研究了温度对硫砷铜矿浸出的影响,氧化还原电位在800 m V时,温度在30~75℃范围,硫砷铜矿硫酸铁酸性化学浸出的表观活化能Ea=57.87 k J·mol-1。实验结果表明,硫酸铁酸性浸出硫砷铜矿符合典型的缩核模型,速率受表面化学反应控制,而非扩散。结合低品位次生硫化铜矿生物堆浸生产实际,为生产实践提出了工艺优化措施。
        Simulating the bio-heap leaching,enargite leaching kinetics tests were carried out under the condition of ferric sulfate acid medium. The chemical property of enargite was found to be stable. About 2. 49% of enargite was dissolved after leaching at 30 ℃ for96 h in a solution containing 31 g·L- 1Fe3 +and 0. 02 g·L- 1Fe2 +with p H of 1. 00 ± 0. 05,under the redox potential of( 900 ± 5)m V. The dissolution rate of enargite was weakly dependent on redox potential,with the reaction orders of 0. 0037,0. 0053,0. 0062,0. 0120 respectively at 30,45,60 and 75 ℃. Potential had few effects on the dissolution rate at lower temperature but a significant effect at higher temperature. The effect of temperature was investigated. An apparent activation energy of 57. 87 k J·mol- 1was obtained with Ehof 800 m V in the temperature range of 30 ~ 75 ℃. It indicated that the kinetics of arsenic dissolution were well represented by a shrinking core model for spherical particles,the kinetics of which were controlled by surface reaction,not by diffusion. Based on the bio-heap leaching practice of low-grade secondary copper sulfide,some suggestions were proposed to optimize the process.
引文
[1]Filippou D,St-Germain P,Grammatikopoulos T.Recovery of metal values from copper-arsenic minerals and other related resources[J].Mineral Processing and Extractive Metallurgy Review,2007,28(4):247.
    [2]Da Pelo S,Musu E,Atzei D,Elsener B,Fantauzzi M,Rossi M.Enargite oxidation:a review[J].Earth Science Reviews,2008,86(1-4):62.
    [3]Sasaki K,Takatasugi K,Ishikura K,Hirajima T.Spectroscopic study on oxidative dissolution of chalcopyritie,enargite and tennantite at differnt p H values[J].Hydrometallurgy,2010,100(3-4):144.
    [4]Elsener B,Atzei D,Fantauzzi M,Rossi A.Electrochemical and XPS surface analytical studies on the reactivity of enargite[J].E.Schweizerbart'sche Verlagsbuchhandlung,2007,19(3):353.
    [5]Fantauzzi M,Elsener B,Atzei D,Lattanzi P,Rossi A.The surface of enargite after exposure to acidic ferric solutions:an XPS/XAES study[J].Surface and Interface Analysis,2007,39(12-13):908.
    [6]Watling H R.The bioleaching of sulphide minerals with emphasis on copper sulphides—a review[J].Hydrometallurgy,2006,84:81.
    [7]Kong W Z,Wu Z L,Liu J Y.Technical progress of enargite leaching technology[J].Nonferrous Metals(Extractive Metallurgy),2014,8:14.(孔维长,伍赠玲,刘金艳.硫砷铜矿浸出技术进展[J].有色金属(冶炼部分),2014,8:14.)
    [8]Sullivan J D.Chemical and physical features of copper leaching[J].Trans.Am.Inst.Min.Metall.,1933,106:514.
    [9]Brown D W,Sullivan J D.Dissolution of various copper minerals[R].U.S.Bureau of Mines Report of Investigation,1934.3228.
    [10]Koch S,Grasselly G.Data on the oxidation of sulphide ore deposites[J].Acta Univ.Szeged,Sect.Sci.Nat.,1952,6:23.
    [11]Ehrlich H L.Bacterial oxidation of arsenopyrite and enargite[J].Economic Geology,1964,59(7):1306.
    [12]Dutrizac J E,Mac Donald J R C.The kinetics of dissolution of enargite in acidified ferric sulphate solutions[J].Canadian Metallurgical Quarterly,1972,11(3):469.
    [13]Dutrizac J E,Mac Donald J R C.Ferric iron as a leaching medium[J].Mineral Science Engineer,1974,6(2):59.
    [14]Da Pelo S.Mineralogical and Geochemical Environment of Active and Abandoned Mining Area[D].Italy:University of Cagliari,1998.152.
    [15]Filipek L H,Plumlee G S.The Environmental Geochemistry of Mineral Deposits,Part B:Society of Economic Geologists[M].Colorado:Littleton,Co.,1999.373.
    [16]Fantauzzi M,Atzei D,Elsener B,Lattanzi P,Rossi A.XPS and XAES analysis of the chemical state of copper,arsenic and sulphur in natural and synthetic enargite[J].Surface and Interface Analysis,2006,38(5):922.
    [17]Herreros O,Quiroz R,Hernandez M C,Vinals J.Dissolution kinetics of enargite in dilute Cl2/Cl-media[J].Hydrometallurgy,2002,64:153.
    [18]Padilla R,Giron D,Ruiz M C.Leaching of enargite in H2SO4-Na Cl-O2media[J].Hydrometallurgy,2005,80:272.
    [19]Gupta M Z.An Investigation into the Leaching of Enargite under Atmospheric Conditions[D].Kingston:Queen's University,2010.85.
    [20]Csicsovszki G,Gupta M,Peacey J.An investigation into the leaching of enargite under atmospheric conditions[A].Hydro Copper 2011[C].Chile:6th International Seminar on Copper Hydrometallurgy,2011.2.
    [21]Li H G.Metallurgical Principle[M].Beijing:Science Press,2005.308.(李洪桂.冶金原理[M].北京:科学出版社,2005.308.)
    [22]Zhong S P,Wu Z,Huang Z S,Ruan R M.Oxidation kinetics reaction of gold-bearing pyrite in sulphuric acid[J].Chinese Journal of Rare Metals,2013,37(2):295.(衷水平,吴智,黄中省,阮仁满.硫酸介质中载金黄铁矿的氧化动力学[J].稀有金属,2013,37(2):295.)
    [23]Ruan R M,Zou G,Zhong S P,Wu Z L,Chan Brenda,Wang D Z.Why Zijinshan copper bioheapleaching plant works efficiently at low microbial activity-study on leaching kinetics of copper sulfides and its implications[J].Minerals Engineering,2013,48(4):36.
    [24]Rivera-Vasquez B F.Electrochemical and Leaching Studies of Enargite and Chalcopyrite[D].Columbia:University of British,2011.65.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700