In-situ FTIR study of reaction mechanism and chemical kinetics of a Xundian lignite during non-isothermal low temperature pyrolysis

Niu Z., Liu G., Yin H., Zhou C., Wu D., Yousaf B., ...More

ENERGY CONVERSION AND MANAGEMENT, vol.124, pp.180-188, 2016 (SCI-Expanded) identifier identifier

  • Publication Type: Article / Article
  • Volume: 124
  • Publication Date: 2016
  • Doi Number: 10.1016/j.enconman.2016.07.019
  • Journal Name: ENERGY CONVERSION AND MANAGEMENT
  • Journal Indexes: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Page Numbers: pp.180-188
  • Keywords: Lignite, Coal pyrolysis, Functional groups, In-situ FTIR, Kinetics of pyrolysis, LOW-RANK COAL, THERMAL-DECOMPOSITION, AUSTRALIAN COALS, ACIDIC GROUPS, BROWN COALS, IR, BONDS
  • Middle East Technical University Affiliated: No

Abstract

Investigating the real time changes of functional groups during lignite pyrolysis can deepen understanding of reaction mechanism of lignite under oxygen-free condition, and help upgrading its quality and enhancing the conversion efficiency. In this study, non-isothermal low temperature pyrolysis of lignite using in-situ Fourier Transform Infrared Spectroscopy (FTIR) was carried out to investigate the evolution of six most abundant functional groups in lignite. The evolution of these functional groups was divided into several stages with different mechanisms and kinetic characteristics. The decomposition of C-O associated with hydroxyls by hydrogen bonds (HBs) played an important role in the pyrolysis process below 400 degrees C. The activation energies for the pyrolysis of lignite at various stages were mostly lower than 70 kJ/mol, and demonstrated the important role of HBs in the low temperature pyrolysis. Additionally, the HBs were mainly related to the aromatic phenol, aromatic ether and phenoxy for C-O, and quinone and carboxyl for C=O. At higher temperature stage (above 300 degrees C), the oxygen contained functional groups, including carboxyl, carbonyl and especially ether, began to decompose, resulting in greater loss of coal materials. At the temperature up to 400 degrees C, the C-C bonds began to break apart, which caused the primary decomposition of aliphatic groups and the increasing intensity of aromatic C-H. (C) 2016 Elsevier Ltd. All rights reserved.