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矿石之微生物脱磷机理的初步研究

郑少奎1, 杨敏1, 关晓辉2, 魏德洲3, 张维庆3   

  1. 1. 中国科学院 生态环境研究中心,北京 100085;2. 东北电力学院应用化学系,吉林 吉林市 132012;3. 东北大学 土木工程学院,辽宁 沈阳 110006
  • 收稿日期:2000-06-20 修回日期:2000-06-20 出版日期:2000-06-20 发布日期:2000-06-20

The Studies on Dephosphorization of Phosphorus-Rich Rhodochrosite by Microorganisms

ZHENG Shao-kui1, YANG Min1, GUAN Xiao-hui2, WEI De-zhou3, ZHANG Wei-qing3   

  1. 1. The Research Center for Eco-environment Science, Academy of China, Beijing 100085; 2. The Department of Applied Chemistry, Northeast Electricity College, Jilin 132012; 3. The College of Resource and Civil Engineering, Northeast University, Shenyang 100085
  • Received:2000-06-20 Revised:2000-06-20 Online:2000-06-20 Published:2000-06-20

摘要: 以生尘芽孢杆菌进行了微生物脱磷机理与应用的探索性研究。试验结果表明:生尘芽孢杆菌脱磷必须经过两个步骤:(1)通过产生有机酸降低溶液pH值使磷矿石中的磷溶出;(2)当溶液中的磷达到一定浓度后微生物形成胞内聚磷酸盐。

Abstract: Manganese ore in China is rich in phosphorus which is often required to be removed in iron and steel industry. Biological dephosphorization was teste d in this study. Bacillus pulvifaciens and a kind of fungi were comp ared in te rms of organic acid production, and the former was found to be more effective fo r organic acid production and was used in the experiments. The dephosphoriza tion tests on an apatite ore were done in two steps: (1)Phosphate dissolution by lowering pH to 3 via organic acid formation; (2) Phosphate is uptaken by bacteria. The first step could be replaced by adding inorganic acid to adjusting pH.