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次火山热变质煤的物理测试特征
引用本文:刘金钟.次火山热变质煤的物理测试特征[J].煤田地质与勘探,1993,21(5):16-20.
作者姓名:刘金钟
作者单位:中国科学院地球化学研究所广州分部 510640
摘    要:样品采自伊敏褐煤盆地中一个因次火山活动形成的烟煤区,包含了从褐煤到瘦煤的变质系列。红外光谱分析表明,煤的含氧基团在褐煤阶段已开始消失,烷基和芳环同步增加,在R°=1.10%时达最大值。顺磁共振自由基浓度和X-衍射参数La/Lc介于区域变质煤和岩浆接触热变质煤之间,芳核外官能团的热演化超前于芳核骨架及R°的演化。 

关 键 词:煤变质作用    红外光谱    电子顺磁共振    X—射线衍射分析
收稿时间:1992-08-01

CHARACTERISTICS OF FTIR,ESR,XRD OF THE COAL METAMORPHIZED BY SUB-VOCANICS
Liu Jinzhong.CHARACTERISTICS OF FTIR,ESR,XRD OF THE COAL METAMORPHIZED BY SUB-VOCANICS[J].Coal Geology & Exploration,1993,21(5):16-20.
Authors:Liu Jinzhong
Institution:National Organic Geochemistry Laboratory, Guangzhou Branch, Institute of Geochemistry, Chinese Academy of Science
Abstract:The samples collected from a bituminous coal area formed by subvocanics in Yimin Brown Coal Field compose a series from brown coal to lean coal.Analysis of FTIR shows that oxygen-bearing functional group began to disapear in brown coal,alkyl and aromatic rings increase synchronously with increase of R°,reaching maxmium when R° is 1.10.Analysis of ESR and XRD shows that concentration of free radical and the ratio La/Lc of aromatic skeleton of the coal are between those of area-metamorphized coal and vocanics-contact metamorphized coal.Evolution of functional group is prior than that of aromatic skeleton and R°。 
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