LIU Qian, ZHONG Wenqi, SU Wei, et al. Oxy-coal combustion kinetics and formation characteristics of pollutants based on TG-MS analysis[J]. CIESC Journal, 2018, (1): 523-530.
DOI:
LIU Qian, ZHONG Wenqi, SU Wei, et al. Oxy-coal combustion kinetics and formation characteristics of pollutants based on TG-MS analysis[J]. CIESC Journal, 2018, (1): 523-530.DOI: 10.11949/j.issn.0438-1157.20171038.
Oxy-coal combustion kinetics and formation characteristics of pollutants based on TG-MS analysis
Oxy-fuel combustion is one of the most promising CO2 capture technologies. The oxygen-enriched combustion of pulverized coal was simulated in a thermogravimetric analyzer coupled with a mass spectrometry (TG-MS) in order to understand the ignition model and the generation characteristics of pollutants during combustion. Bituminous and anthracite standard coals were selected as the samples. The tests were done with oxygen volume fractions of 21%
30% and 50% with two kinds of atmospheres (O2/Ar and O2/CO2). In the O2/CO2 atmosphere
both of the ignition temperature and burnout temperature were lower
the combustion rate was improved
the combustion time was shortened
and the combustion performance was much better. Based on the TG/DTG curves
the ignition models of pulverized coal were judged. It was showed that the heterogeneous ignition of pulverized coal happened in O2/Ar atmosphere
while the homogeneous ignition occurred in O2/CO2 atmosphere. Also
the activation energy and pre-exponential factor of coal combustion were calculated by Coats-Redfern method. When the oxygen volume fraction was above 30%
the apparent activation energy of the anthracite coal combustion in O2/CO2 atmosphere was significantly lower than that in O2/Ar atmosphere
indicating an obvious improvement in reactivity. In the same reaction conditions
the activation energy of bituminous coal was lower than that of anthracite coal
and the former was more prone to ignition and combustion
showing better combustion performance. In the atmosphere of O2/CO2
the generation of CO and volatile-NO was promoted
and the formation temperature was lower than in O2/Ar atmosphere. Meanwhile
the abundant CO would lead to NO reduction reaction.
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