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Biodesulfurization of high sulfur fat coal with indigenous and exotic microorganisms

机译:高硫脂肪煤与本地和外来微生物的生物脱硫

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摘要

Coal is the most abundant fossil fuel in the world and its combustion accompanies with the emission of SOX, which is responsible for serious environmental problems. To reduce the emission of SOX is essential for clean fuel. In the present study, indigenous microorganisms acclimatized from fat coal itself and exotic microorganisms from sewage sludge were used for coal biodesulfurization. X-ray diffraction (XRD), Fourier transform infrared spectroscopy (FT-IR), and Raman spectral analysis were used to investigate the structural change of fat coal during the bioleaching. Results showed that kaolinite and quartz were the main minerals, and pyrite was the main inorganic sulfide in fat coal. After 36-day biodesulfurization, the total sulfur in fat coal decreased from 5.07% to 2.77% and 2.75%, and the pyritic removal was 77.68% and 87.88% with indigenous and exotic microorganisms, respectively. The exotic microorganisms were more effective to oxidize the pyrite than the indigenous microorganisms. But both microorganisms did not interact with the organic sulfur, which existed as C-S bond in fat coal. FT-IR analyses showed the damage of kaolinite structure, indicating potential microbial effect on kaolinite, which has not been reported before. Raman spectral analysis was for the first time used to investigate the changes of coal macromolecular structure during the bioleaching. FT-IR and Raman spectra confirmed the changes of aromatic C-H, O-H bonds, which led to the increase of carbon crystallinity index. (C) 2018 Elsevier Ltd. All rights reserved.
机译:煤炭是世界上最丰富的化石燃料,其燃烧伴随着SOX的排放,导致严重的环境问题。减少SOX的排放对于清洁燃料至关重要。在本研究中,从脂肪煤本身中驯化的本地微生物和污水污泥中的外来微生物用于煤炭生物脱硫。利用X射线衍射(XRD),傅里叶变换红外光谱(FT-IR)和拉曼光谱分析技术研究了生物浸出过程中脂肪煤的结构变化。结果表明,肥煤中高岭石和石英是主要矿物,黄铁矿是主要的无机硫化物。经过36天的生物脱硫后,肥煤中的总硫从5.07%下降到2.77%和2.75%,原生和外来微生物的硫铁矿去除分别为77.68%和87.88%。外来微生物比本地微生物更有效地氧化黄铁矿。但是两种微生物都没有与有机硫相互作用,而有机硫以脂肪煤中的C-S键存在。 FT-IR分析表明高岭石结构受到破坏,表明对高岭石具有潜在的微生物作用,这以前没有报道。拉曼光谱分析首次用于研究生物浸出过程中煤大分子结构的变化。 FT-IR和拉曼光谱证实了芳族C-H,O-H键的变化,从而导致碳结晶度指数的增加。 (C)2018 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Journal of Cleaner Production》 |2018年第1期|562-570|共9页
  • 作者单位

    Beijing Forestry Univ, Coll Environm Sci & Engn, Qinghua East Rd 35, Beijing 100083, Peoples R China;

    Beijing Forestry Univ, Coll Environm Sci & Engn, Qinghua East Rd 35, Beijing 100083, Peoples R China;

    Renmin Univ China, Sch Environm & Resource, Zhongguancun St 59, Beijing 100872, Peoples R China;

    Beijing Forestry Univ, Coll Environm Sci & Engn, Qinghua East Rd 35, Beijing 100083, Peoples R China;

    Beijing Forestry Univ, Coll Environm Sci & Engn, Qinghua East Rd 35, Beijing 100083, Peoples R China;

    Beijing Forestry Univ, Coll Environm Sci & Engn, Qinghua East Rd 35, Beijing 100083, Peoples R China;

    Shanxi Agr Univ, Coll Urban & Rural Construct, Taigu 030801, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Biodesulfurization; Coal; Pyrite; Kaolinite; Microorganisms;

    机译:生物脱硫煤炭黄铁矿高岭石微生物;

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