4.7 Article

Characterization of coalification jumps during high rank coal chemical structure evolution

Journal

FUEL
Volume 185, Issue -, Pages 298-304

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.fuel.2016.07.121

Keywords

Coal; Coalification jumps; Chemical structure; Structural parameters; Fourier Transform Infrared

Funding

  1. National Natural Science Foundation of China [41472135, 41072117, 41430317]
  2. Natural Science Foundation of Jiangsu Province, China [BK20160243]
  3. China Postdoctoral Science Foundation [2015M581878]

Ask authors/readers for more resources

The functional groups and coalification jumps were studied by the Fourier Transform Infrared spectroscopy (FTIR), characterized along with the increasing temperature. The raw coal sample with high coal rank (R-o,(max) = 1.82%) was used to further form some high rank samples using improved microscale sealed vessel (MSSV) pyrolysis method for the FTIR analyses. The MSSV pyrolysis simulates coalification process under different temperatures by heating the raw coal from 350 degrees C to 550 degrees C at a heating rate of 10 degrees C/h, producing the high rank coal samples that can be used for characterization of the functional groups and coalification jumps. Combined with proximate and ultimate analyses, FTIR provides new insight to the chemical structure of the coal samples. The results show that the typical vibration of function groups includes C-H aromatic out-of-plane deformation at 877 cm(-1), 812 cm(-1) and 784 cm(-1); carbonyl/carboxyl C=O stretching at 1712 cm(-1); -OH stretching at 3422 cm(-1) and aromatic C-H stretching at 3040 cm(-1). The structural parameters, such as degree of condensation 1 and 2 (DOC1, DOC2), aromaticity 1 and 2 (AR1, AR2), A-factor, C-factor, and CH2/CH3 were calculated by peaks area of the FTIR spectrum. The calculation provides fundamental information to correlate the intensity of functional groups factors such as temperature and vitrinite reflectance etc. It was found that AR2 values for semi-anthracites and anthracites showed relatively large variation, likely because of the decreasing intensities of Char peaks via de-functionalization during coalification. Besides, AR1 and AR2 behave quite similarly as their FTIR spectrum peaks show the same range from 450 degrees C to 500 degrees C. The values of both DOC1 and DOC2 generally increased in the range of temperature from 350 degrees C to 370 degrees C and reached the peak at 370 degrees C followed by a sharp decline. The phenomenon was likely due to the large loss of hydrogen in corresponding temperature range, which limited intensities of the aromatic CHx stretching band at 3000-3100 cm(-1). The A-factor and C-factor gradually decreased as temperature increased. In addition, the jumps were presented in terms of the structural parameters and methane yield lines. A new jump was identified at R-o,R-max = 3.22-3.03% after 470 degrees C. Furthermore the methane yield data comparatively show consistent with the functional group of vitrinite molecule in different rank. (C) 2016 Elsevier Ltd. All rights reserved.

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