Structures and contributions of active substances in the latent oxidation of coal based on the oxygen isotope tracer method

The oxygen isotope tracer method was used to determine the structures and contributions of the active substances that trigger coal spontaneous combustion (CSC). After artificially changing the oxygen isotope ratio, the coal samples were subjected to isothermal oxidation under different conditions (d...

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Published inEnergy (Oxford) Vol. 291; p. 130405
Main Authors Zhao, Xingguo, Dai, Guanglong, Qin, Ruxiang, Zhou, Liang, Li, Jinhu, Li, Jinliang, He, Yinnan
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 15.03.2024
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ISSN0360-5442
DOI10.1016/j.energy.2024.130405

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Abstract The oxygen isotope tracer method was used to determine the structures and contributions of the active substances that trigger coal spontaneous combustion (CSC). After artificially changing the oxygen isotope ratio, the coal samples were subjected to isothermal oxidation under different conditions (different temperatures, different oxidation times and different coal types) in an 18O2 atmosphere. First, the oxidation gases were obtained with cyclic oxidation experiments. The basic parameters were provided for tests of the gas isotopes. The oxidation products labeled with 18O were then analyzed with an isotope ratio mass spectrometer. The original active substances in the coal were determined. Evolution of the functional groups in the coal was determined by XPS. The transformation paths of the active substance were analyzed. The results showed that during the oxidation process, more than 70 % of the CO was generated from the original hydroxyl and aldehyde groups in the coal, and more than 99 % of the CO2 was generated from the original carboxyl groups in the coal. Inhibition of oxidative decomposition of hydroxyl, aldehyde and carboxyl groups can effectively control CSC and solve the problem of CO overflow caused by low-rank coal oxidation. •Oxygen isotope tracer method applied to coal combustion.•70 % of the CO was generated from the original hydroxyl and aldehyde groups.•99 % of the CO2 was generated from the original carboxyl groups in the coal.•Critical temperature for alkyl structures to CO was between 60 °C and 70 °C.
AbstractList The oxygen isotope tracer method was used to determine the structures and contributions of the active substances that trigger coal spontaneous combustion (CSC). After artificially changing the oxygen isotope ratio, the coal samples were subjected to isothermal oxidation under different conditions (different temperatures, different oxidation times and different coal types) in an 18O2 atmosphere. First, the oxidation gases were obtained with cyclic oxidation experiments. The basic parameters were provided for tests of the gas isotopes. The oxidation products labeled with 18O were then analyzed with an isotope ratio mass spectrometer. The original active substances in the coal were determined. Evolution of the functional groups in the coal was determined by XPS. The transformation paths of the active substance were analyzed. The results showed that during the oxidation process, more than 70 % of the CO was generated from the original hydroxyl and aldehyde groups in the coal, and more than 99 % of the CO2 was generated from the original carboxyl groups in the coal. Inhibition of oxidative decomposition of hydroxyl, aldehyde and carboxyl groups can effectively control CSC and solve the problem of CO overflow caused by low-rank coal oxidation. •Oxygen isotope tracer method applied to coal combustion.•70 % of the CO was generated from the original hydroxyl and aldehyde groups.•99 % of the CO2 was generated from the original carboxyl groups in the coal.•Critical temperature for alkyl structures to CO was between 60 °C and 70 °C.
The oxygen isotope tracer method was used to determine the structures and contributions of the active substances that trigger coal spontaneous combustion (CSC). After artificially changing the oxygen isotope ratio, the coal samples were subjected to isothermal oxidation under different conditions (different temperatures, different oxidation times and different coal types) in an ¹⁸O₂ atmosphere. First, the oxidation gases were obtained with cyclic oxidation experiments. The basic parameters were provided for tests of the gas isotopes. The oxidation products labeled with ¹⁸O were then analyzed with an isotope ratio mass spectrometer. The original active substances in the coal were determined. Evolution of the functional groups in the coal was determined by XPS. The transformation paths of the active substance were analyzed. The results showed that during the oxidation process, more than 70 % of the CO was generated from the original hydroxyl and aldehyde groups in the coal, and more than 99 % of the CO₂ was generated from the original carboxyl groups in the coal. Inhibition of oxidative decomposition of hydroxyl, aldehyde and carboxyl groups can effectively control CSC and solve the problem of CO overflow caused by low-rank coal oxidation.
ArticleNumber 130405
Author Qin, Ruxiang
He, Yinnan
Zhao, Xingguo
Dai, Guanglong
Li, Jinhu
Zhou, Liang
Li, Jinliang
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Keywords Oxygen isotope tracer
Active substance
Latent period
Coal spontaneous combustion
CO and CO2
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SubjectTerms active ingredients
Active substance
aldehydes
carbon dioxide
CO and CO2
coal
Coal spontaneous combustion
combustion
energy
evolution
Latent period
Oxygen isotope tracer
oxygen isotopes
spectrometers
tracer techniques
Title Structures and contributions of active substances in the latent oxidation of coal based on the oxygen isotope tracer method
URI https://dx.doi.org/10.1016/j.energy.2024.130405
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Volume 291
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