Hengyi He , Baisheng Nie , Peng Liu , Jijiang Huang , Hao Zhang , Yanan Hou , Kaidan Bai
{"title":"煤地下燃烧-气体动力学的官能团驱动调控","authors":"Hengyi He , Baisheng Nie , Peng Liu , Jijiang Huang , Hao Zhang , Yanan Hou , Kaidan Bai","doi":"10.1016/j.psep.2025.107359","DOIUrl":null,"url":null,"abstract":"<div><div>Enhanced combustion coupled with in-situ thermal energy extraction in underground coal seams represents a novel paradigm-shifting strategy for coal resource extraction through in-situ chemical fluidized mining. Systematic investigation into the combustion dynamics and reactive gas evolution under injection-enhanced conditions provides validation for optimizing this in-situ thermo-chemical conversion process. This study elucidates the metamorphic dependence of coal combustion through combined FTIR and TG-FTIR analyses, delineating functional group evolution and gaseous emission dynamics across coals of different metamorphic grades. The results indicate that the intensification of the coal metamorphism, characterized by increased multi-substituted aromatic groups (2 adjacent H deformation) and stable OH-π structures, alongside reduced active oxygen-containing groups (conjugated C<img>O and -COOH) and asymmetric aliphatic chains, collectively diminishes the coal ignitability. Combustion performance indices reveal that low-metamorphic-degree coal exhibits enhanced ignition and combustion efficiency at lower temperatures, whereas high-metamorphic-degree coals demonstrate inferior ignitability but achieve higher combustion rates. Highly metamorphosed coal typically exhibits lower CO<sub>2</sub> emission intensity and higher CO emission intensity due to incomplete oxidation. This divergence in combustion products directly correlates with enhanced oxygen demand requirements for complete oxidation at higher metamorphic stages. CH<sub>4</sub> emission predominantly occurs within the 200–700℃ thermal regime, with 400°C serving as a critical thermal demarcation point for the peak CH<sub>4</sub> release intensity from coals of varying metamorphic degrees. NO is the main component of the harmful gas NO<sub>x</sub>, and highly metamorphosed coal releases less NO. Ignition propensity demonstrates linear dependence with -COOH, and the burnout efficiency exhibits proportional enhancement of the 3 adjacent H deformation. OH-OH, asym. R₂CH₂, and asym. RCH₃ collectively control the volumetric release of gaseous species during coal combustion. These findings offer a scientific basis for optimizing underground coal combustion systems by strategically utilizing natural variations in coal maturity.</div></div>","PeriodicalId":20743,"journal":{"name":"Process Safety and Environmental Protection","volume":"200 ","pages":"Article 107359"},"PeriodicalIF":6.9000,"publicationDate":"2025-05-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Functional group-driven modulation of combustion-gas kinetics in underground coal enhanced combustion\",\"authors\":\"Hengyi He , Baisheng Nie , Peng Liu , Jijiang Huang , Hao Zhang , Yanan Hou , Kaidan Bai\",\"doi\":\"10.1016/j.psep.2025.107359\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Enhanced combustion coupled with in-situ thermal energy extraction in underground coal seams represents a novel paradigm-shifting strategy for coal resource extraction through in-situ chemical fluidized mining. Systematic investigation into the combustion dynamics and reactive gas evolution under injection-enhanced conditions provides validation for optimizing this in-situ thermo-chemical conversion process. This study elucidates the metamorphic dependence of coal combustion through combined FTIR and TG-FTIR analyses, delineating functional group evolution and gaseous emission dynamics across coals of different metamorphic grades. The results indicate that the intensification of the coal metamorphism, characterized by increased multi-substituted aromatic groups (2 adjacent H deformation) and stable OH-π structures, alongside reduced active oxygen-containing groups (conjugated C<img>O and -COOH) and asymmetric aliphatic chains, collectively diminishes the coal ignitability. Combustion performance indices reveal that low-metamorphic-degree coal exhibits enhanced ignition and combustion efficiency at lower temperatures, whereas high-metamorphic-degree coals demonstrate inferior ignitability but achieve higher combustion rates. Highly metamorphosed coal typically exhibits lower CO<sub>2</sub> emission intensity and higher CO emission intensity due to incomplete oxidation. This divergence in combustion products directly correlates with enhanced oxygen demand requirements for complete oxidation at higher metamorphic stages. CH<sub>4</sub> emission predominantly occurs within the 200–700℃ thermal regime, with 400°C serving as a critical thermal demarcation point for the peak CH<sub>4</sub> release intensity from coals of varying metamorphic degrees. NO is the main component of the harmful gas NO<sub>x</sub>, and highly metamorphosed coal releases less NO. Ignition propensity demonstrates linear dependence with -COOH, and the burnout efficiency exhibits proportional enhancement of the 3 adjacent H deformation. OH-OH, asym. R₂CH₂, and asym. RCH₃ collectively control the volumetric release of gaseous species during coal combustion. These findings offer a scientific basis for optimizing underground coal combustion systems by strategically utilizing natural variations in coal maturity.</div></div>\",\"PeriodicalId\":20743,\"journal\":{\"name\":\"Process Safety and Environmental Protection\",\"volume\":\"200 \",\"pages\":\"Article 107359\"},\"PeriodicalIF\":6.9000,\"publicationDate\":\"2025-05-22\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Process Safety and Environmental Protection\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0957582025006263\",\"RegionNum\":2,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"ENGINEERING, CHEMICAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Process Safety and Environmental Protection","FirstCategoryId":"93","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0957582025006263","RegionNum":2,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ENGINEERING, CHEMICAL","Score":null,"Total":0}
Functional group-driven modulation of combustion-gas kinetics in underground coal enhanced combustion
Enhanced combustion coupled with in-situ thermal energy extraction in underground coal seams represents a novel paradigm-shifting strategy for coal resource extraction through in-situ chemical fluidized mining. Systematic investigation into the combustion dynamics and reactive gas evolution under injection-enhanced conditions provides validation for optimizing this in-situ thermo-chemical conversion process. This study elucidates the metamorphic dependence of coal combustion through combined FTIR and TG-FTIR analyses, delineating functional group evolution and gaseous emission dynamics across coals of different metamorphic grades. The results indicate that the intensification of the coal metamorphism, characterized by increased multi-substituted aromatic groups (2 adjacent H deformation) and stable OH-π structures, alongside reduced active oxygen-containing groups (conjugated CO and -COOH) and asymmetric aliphatic chains, collectively diminishes the coal ignitability. Combustion performance indices reveal that low-metamorphic-degree coal exhibits enhanced ignition and combustion efficiency at lower temperatures, whereas high-metamorphic-degree coals demonstrate inferior ignitability but achieve higher combustion rates. Highly metamorphosed coal typically exhibits lower CO2 emission intensity and higher CO emission intensity due to incomplete oxidation. This divergence in combustion products directly correlates with enhanced oxygen demand requirements for complete oxidation at higher metamorphic stages. CH4 emission predominantly occurs within the 200–700℃ thermal regime, with 400°C serving as a critical thermal demarcation point for the peak CH4 release intensity from coals of varying metamorphic degrees. NO is the main component of the harmful gas NOx, and highly metamorphosed coal releases less NO. Ignition propensity demonstrates linear dependence with -COOH, and the burnout efficiency exhibits proportional enhancement of the 3 adjacent H deformation. OH-OH, asym. R₂CH₂, and asym. RCH₃ collectively control the volumetric release of gaseous species during coal combustion. These findings offer a scientific basis for optimizing underground coal combustion systems by strategically utilizing natural variations in coal maturity.
期刊介绍:
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