ABSTRACT This paper establishes correlations between various pyrolysis products collected from the vicinity of the fire zone and the prevailing temperature using substance identification via GC-MS analysis. Further experimental comparisons among multiple substances reveal a strong correlation between phenols and temperature. This leads to the identification of temperature-specific products primarily composed of phenols, ultimately enhancing the accuracy of fire area temperature recognition. This experiment utilized a self-built fixed bed and GC-MS technology to qualitatively and quantitatively study the release characteristics of gaseous tars from lignite, long-flame coal, and gas coal at different temperatures (300°C, 350°C, 400°C, 450°C, 500°C) under pyrolysis conditions. The experimental results showed that there are significant differences in the tar components produced during pyrolysis among coals with different degrees of metamorphism. The composition ratios are all in the order of oxygen-containing organic compounds > aromatic hydrocarbons > aliphatic hydrocarbons, and the three most abundant organic compounds are phenol, o-cresol, and p-cresol. The types and quantities of organic compounds in coal pyrolysis tars are positively correlated with reaction temperature. Based on a third-order polynomial fitting of the total amount of compounds in pyrolysis tars and the corresponding temperature under pyrolysis conditions, the representative subclasses of each type of substance were further fitted. The results of the temperature correlation show that the fitting trend of phenols with temperature is similar to the overall trend and far superior to naphthalene organics and saturated alkanes. In the vertical comparison of phenolic content at different temperatures, common identifiable substances such as C8H10O and C23H32O2 are selected, and specific substance identification was provided for coal samples of different ranks of coal metamorphism. This ultimately provides a new approach for establishing a method to identify the combustion state of coal fires at 300–500°C.
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