<th id="5nh9l"></th><strike id="5nh9l"></strike><th id="5nh9l"><noframes id="5nh9l"><th id="5nh9l"></th><strike id="5nh9l"></strike>
<progress id="5nh9l"><noframes id="5nh9l"><th id="5nh9l"><noframes id="5nh9l">
<th id="5nh9l"></th> <strike id="5nh9l"><noframes id="5nh9l"><span id="5nh9l"></span>
<progress id="5nh9l"><noframes id="5nh9l"><span id="5nh9l"><noframes id="5nh9l"><span id="5nh9l"></span><strike id="5nh9l"><noframes id="5nh9l"><strike id="5nh9l"></strike>
<span id="5nh9l"><noframes id="5nh9l">
<span id="5nh9l"><noframes id="5nh9l">
<span id="5nh9l"></span><span id="5nh9l"><video id="5nh9l"></video></span>
<th id="5nh9l"><noframes id="5nh9l"><th id="5nh9l"></th>
<progress id="5nh9l"><noframes id="5nh9l">

不同類型黃銅礦的生物浸出研究

Study on bioleaching of different types of chalcopyrite

  • 摘要: 研究了兩種不同類型(黃鐵礦型,斑巖型)黃銅礦生物浸出的差異.實驗結果表明:兩類黃銅礦生物浸出差別很大,48 d后黃鐵礦型黃銅礦浸出率為46.96%,斑巖型黃銅礦浸出率為14.5%.對Fe2+、礦物表面Cu2p譜圖和礦床特征的分析發現:適量的Fe2+能促進黃銅礦的浸出,但最佳用量不一樣;浸渣表面產物不同,斑巖型黃銅礦表面出現富銅層,阻礙了浸出繼續進行;與原礦相比,銅結合能都降低,符合Hiroyoshi等提出黃銅礦浸出的兩步溶解模型;兩類黃銅礦生物浸出的差異是由成礦巖體、圍巖、伴生礦物和元素、成礦溫度和壓力等因素綜合決定的.

     

    Abstract: Bioleaching of chalcopyrite with two different types,pyrite type and porphyry type,was compared.It is shown that there is a great difference in leaching efficiency.After 48d,the copper leaching rate reaches 46.96% for the pyritic chalcopyrite,while it is 14.5% for the porphyry chalcopyrite.Based on the analysis of Fe2+,Cu 2p spectra on the chalcopyrite surface and deposit characteristics,a moderate amount of Fe2+ can promote bioleaching of the two kinds of chalcopyrite,but their optimal dosages are distinct.Different products appear on the surfaces of leached residues,and there is a copper-rich layer on the porphyry chalcopyrite,which hinders a greater copper extraction.Compared with the crude ore,Cu peak shift to lower binding energies was observed,following the leaching mechanism suggested by Hiroyoshi et al.the difference in bio-leaching between them is dependent on the integration of many factors such as metallogenic rock,wall rock,associated minerals and elements,metallogenic temperature and pressure.

     

/

返回文章
返回
<th id="5nh9l"></th><strike id="5nh9l"></strike><th id="5nh9l"><noframes id="5nh9l"><th id="5nh9l"></th><strike id="5nh9l"></strike>
<progress id="5nh9l"><noframes id="5nh9l"><th id="5nh9l"><noframes id="5nh9l">
<th id="5nh9l"></th> <strike id="5nh9l"><noframes id="5nh9l"><span id="5nh9l"></span>
<progress id="5nh9l"><noframes id="5nh9l"><span id="5nh9l"><noframes id="5nh9l"><span id="5nh9l"></span><strike id="5nh9l"><noframes id="5nh9l"><strike id="5nh9l"></strike>
<span id="5nh9l"><noframes id="5nh9l">
<span id="5nh9l"><noframes id="5nh9l">
<span id="5nh9l"></span><span id="5nh9l"><video id="5nh9l"></video></span>
<th id="5nh9l"><noframes id="5nh9l"><th id="5nh9l"></th>
<progress id="5nh9l"><noframes id="5nh9l">
259luxu-164