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黃鐵礦燒渣微生物脫硫

Bio-desulphurization from Pyrite Slag with Thiobacillus Ferrooxidans

  • 摘要: 在燒渣生物脫硫的試驗.論研究了礦漿濃度、Fe3+濃度及pH值對游離T.f菌濃度和脫硫率的影響.證明燒渣脫硫是T.f.菌直接浸出作用和由細菌而產生的Fe3+間接浸出作用的聯合;脫硫速率和菌種氧化活性受到吸附在固相上和液相中細菌生長情況、礦漿濃度、pH值和Fe3+的影響;三價鐵離子的添加可影響菌種活性,抑制浸出的進行,且易在礦物表面產生沉淀,降低氧化率.燒渣生物脫硫后,可達到鐵精礦標準.

     

    Abstract: The bio-desulphurization experiments on slag were carried out. The results show that pulp density, Fe3+ concentration and pH are effect on Thiobacillus ferrooxidans(T.f.) consistency free in the solution and desulphurization rate. The bio-desulphurization from slag is due to the combination of the direct bacterial action on the mineral surface with the indirect leaching by the ferric ion produced by the bacteria into the solution. Desulphurization rate and oxidative activity of the T.f. are influenced by the growth of T.f adhered to the mineral, mineral density, Fe3+ concentration and pH consistency. The addition of ferric ion can interfere in the bacteria oxidative activity and result in inhibiting effect on the desulphurization, some sediment on the surface of the mineral are formed to reduce desulphurization rate.

     

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