2019
DOI: 10.1016/j.fuel.2018.11.060
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Low-temperature oxidation of free radicals and functional groups in coal during the extraction of coalbed methane

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Cited by 52 publications
(18 citation statements)
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“…During this process, the old free radical is constantly annihilated, and new free radical are generated. When the free radical continues to accumulate to initiate a chain reaction, the free radical concentration soars, and the reaction with oxygen continues to accelerate to produce a large amount of heat, eventually leading to coal spontaneous combustion 21,22 . According to the experiment, the ESR spectra of coal gangue during heating and oxidation under oxygen concentrations of 0%, 5%, 10%, 15%, and 21% are as shown in Figure 2.…”
Section: Results and Analysismentioning
confidence: 98%
“…During this process, the old free radical is constantly annihilated, and new free radical are generated. When the free radical continues to accumulate to initiate a chain reaction, the free radical concentration soars, and the reaction with oxygen continues to accelerate to produce a large amount of heat, eventually leading to coal spontaneous combustion 21,22 . According to the experiment, the ESR spectra of coal gangue during heating and oxidation under oxygen concentrations of 0%, 5%, 10%, 15%, and 21% are as shown in Figure 2.…”
Section: Results and Analysismentioning
confidence: 98%
“…Natural desorption of gases from bituminous coal results in methane release to the atmosphere with smaller amounts of ethane, propane and carbon dioxide 35 37 . Extensive studies in this field were performed by Xu et al 38 , 39 and Chen et al 40 . Exposing of coal to air results in parallel processes of coal oxidation and desorption of carbon monoxide and dioxide 41 .…”
Section: Resultsmentioning
confidence: 99%
“…This implied that -COOH had a high reaction activity and was the main reaction group during the low temperature oxidation process. 23 When the temperature was below 200°C, the carboxyl group's change range in the air atmosphere was similar to its change range in the argon atmosphere. This means then, that it could be inferred that oxygen was not directly involved in the change of the -COOH content at this stage.…”
Section: The Change In -Coohmentioning
confidence: 93%
“…However, under air atmosphere, the amount of C-O-C at 500°C was 3.6 times more than that at 30°C. This demonstrated that C-O-C was a stable structure, and that the participation of oxygen hindered the formation of C-O-C. 23 It was therefore difficult for C-O-C to participate in the coal oxidation reaction, but it could stably exist at a high temperature.…”
Section: The Change In C-o-cmentioning
confidence: 99%
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