Journal of Thermal Analysis and Calorimetry

, Volume 117, Issue 1, pp 489–497 | Cite as

Thermogravimetric analysis of peat decomposition under different oxygen concentrations

  • Weitao Zhao
  • Haixiang Chen
  • Naian Liu
  • Jianjun Zhou
Article

Abstract

Smoldering combustion of peat is of global concern as a natural hazard to consume sequestered carbon and form wide-area haze. It is affected by thermal decomposition kinetics of peat and the diffusion and availability of oxygen. In this work, thermal decomposition behavior of peat was investigated using thermogravimetric analysis under the atmosphere with different oxygen concentrations. The results showed that thermal decomposition process of peat could be divided into three stages: dehydration, oxidative pyrolysis of organic matters into volatiles and char, and oxidation of the generated char. The apparent activation energies of peat decomposition under different oxygen concentrations were calculated by model-free methods of Kissinger, FWO, Starink, Gyulai, and Friedman. A two-step reaction model was proposed to describe thermal decomposition kinetics of peat (excluding dehydration stage) and the effect of oxygen concentration on the kinetic parameters was discussed. These results provide basic data for smoldering modeling of peat.

Keywords

Peat Thermal decomposition Thermogravimetric analysis Smoldering 

Notation

TG

Thermogravimetry

DTG

Derivative thermogravimetry (K−1)

E, E1, E2

Apparent activation energy (kJ mol−1)

R

Ideal gas constant, 8.314 J K−1 mol−1)

A, A1, A2

Arrhenius frequency factor

T

Absolute temperature (K)

β

Heating rate of decomposition (K min−1)

k1, k2

Reaction rate coefficients

P

The initial mass of the peat removed moisture and mineral content

D, V1, V2

Product of reaction

V1, V2

The mass loss (gas mass) of two-step reaction, respectively

m0, m

The mass of beginning and end of peat decomposition (g)

r1, r2

Dimensionless parameter defined by Eq. (5)

n1, n2

Reaction order

OF

Objective function

RSQ

R-Squared

Notes

Acknowledgements

This work was sponsored by the National Natural Science Foundation of China (51176179 and 51120165001) and the National Basic Research Program of China (973 Program, No. 2012CB719702). Chen was supported by Fundamental Research Funds for the Central University (WK2320000020).

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Copyright information

© Akadémiai Kiadó, Budapest, Hungary 2014

Authors and Affiliations

  • Weitao Zhao
    • 1
  • Haixiang Chen
    • 1
  • Naian Liu
    • 1
  • Jianjun Zhou
    • 1
  1. 1.State Key Laboratory of Fire ScienceUniversity of Science and Technology of ChinaHefeiChina

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