文献类型：期刊文献

英文题名：Structure characteristics and gasification activity of residual carbon from entrained-flow coal gasification slag

作者：Wu, Shiyong[1,2];Huang, Sheng[1,2];Ji, Liyuan[1];Wu, Youqing[1,2];Gao, Jinsheng[1,2]

机构：[1]E China Univ Sci & Technol, Dept Chem Engn Energy Resources, Shanghai 200237, Peoples R China;[2]E China Univ Sci & Technol, Minist Educ, Key Lab Coal Gasificat & Energy Chem Engn, Shanghai 200237, Peoples R China

年份：2014

卷号：122

起止页码：67

外文期刊名：FUEL

收录：;EI(收录号：20140717304928);WOS:【SCI-EXPANDED(收录号:WOS:000331544100009)】；

基金：This work was supported by the National Basic Research Program of China (No. 2010CB227003), the National High Technology Research and Development Program of China (No. 2012AA101810), the State Natural Science Foundation of China (No. 20876050) and the Opening Fund of State Key Laboratory of Coal Combustion in China (No. fsklcc0911).

语种：英文

外文关键词：Entrained-flow coal gasification; Gasification slag; Residual carbon; Structure characteristics; Gasification activity

摘要：The structure characteristics and gasification activity of residual carbon from entrained-flow coal gasification slag were mainly investigated using a pore structure analyzer, a scanning electron microscopy, a Raman spectroscopy and a thermo-gravimetric analyzer. Simultaneously, a kind of residual carbon from coal chars was used for a reference. Results showed that the residual carbon which was usually considered as "the unburnt carbon" in gasification slags, was potentially originated from volatile matters (especially those with macromolecular structures) of the original coal pyrolysis, partly-gasified carbons and/or unreacted pyrolytic carbons. Compared to the residual carbon in coal chars, that in gasification slags had a higher pore surface area, a larger average pore size, a more ordered carbon crystalline structure and less total active sites, whereas that in both coarse and fine slags presented a distinctly higher gasification activity, mainly ascribed to its quite more abundant porosity. Compared to the residual carbon in the fine slag, that in the coarse slag had a lower pore surface area, a slightly more disordered carbon crystalline structure and more total active sites, but that in the coarse slag presented a higher gasification activity, especially after the carbon conversion of around 0.5. This was probably due to more total active sites in the residual carbon of the coarse slag, especially its more active sites with mixed sp(2)-sp(3) bond form. Besides, it also could be inferred that the activity of active sites with sp(2) bond form was superior to that with mixed sp(2)-sp(3) bond form. (C) 2014 Elsevier Ltd. All rights reserved.