FTIR and Raman spectroscopy characterization of functional groups in various rank coals

被引:594
作者
He Xueqiu [1 ,2 ,3 ]
Liu Xianfeng [2 ,3 ]
Nie Baisheng [2 ,3 ]
Song Dazhao [1 ]
机构
[1] Univ Sci & Technol Beijing, Sch Civil & Resource Engn, Beijing 10083, Peoples R China
[2] China Univ Min & Technol Beijing, State Key Lab Coal Resources & Safe Min, Beijing 10083, Peoples R China
[3] China Univ Min & Technol Beijing, Sch Resources & Safety Engn, Beijing 10083, Peoples R China
基金
中国国家自然科学基金;
关键词
FTIR; Raman spectroscopy; Functional groups; Coal; Evolutionary trend; X-RAY-DIFFRACTION; STATE C-13 NMR; LATE PERMIAN COALS; STRUCTURAL FEATURES; ELECTRON-MICROSCOPY; AUSTRALIAN COALS; CARBONACEOUS MATERIALS; MACERAL COMPOSITION; METHANE ADSORPTION; SPECTRAL-ANALYSIS;
D O I
10.1016/j.fuel.2017.05.101
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
080707 [能源环境工程]; 082001 [油气井工程];
摘要
Coals varying in rank from lignite to anthracite were comprehensively characterized with regard to chemical structure using FTIR and Raman spectroscopy. Structural parameters were determined from spectrum deconvolution, and correlations were established for these parameters. The evolution of coal structure is complex with three stage characteristics at R-o = 0.4-1.3%, 1.3-2.0% and 2.0-4.0%, respectively. At R-o = 0.4-1.3%, the rapid decline in oxygen-containing functional groups accompanied with the enrichment of aliphatic compounds is the main characteristic. When R-o = 1.3-2.0%, the sharp changes of the band position difference (G-D-1), A(D1)/A(G) and apparent aromaticity (fa) are caused by the strongest aromatization at this period. The aromatic rings and degree of graphitization are significantly enhanced, with the length of aliphatic chains (A(CH2)/A(CH3)) decreasing to the lowest level. When R-o = 2.0-4.0%, the slow variation of parameters (fa, 'C', G-D-1 and A(D1)/A(G)) confirms that most of heterocycle compounds and amorphous carbon structures have been lost. The size of aromatic clusters and graphite crystallite continuously increase, and the microcrystalline structure in coal is gradually perfected, closer to graphite structure. These findings can provide a comprehensive understanding of chemical and physical properties of coals. (C) 2017 Elsevier Ltd. All rights reserved.
引用
收藏
页码:555 / 563
页数:9
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