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.
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.
Liu Jinzhong. CHARACTERISTICS OF FTIR,ESR,XRD OF THE COAL METAMORPHIZED BY SUB-VOCANICS[J]. COAL GEOLOGY & EXPLORATION, 1993, 21(5): 16-20.
Citation: Liu Jinzhong. CHARACTERISTICS OF FTIR,ESR,XRD OF THE COAL METAMORPHIZED BY SUB-VOCANICS[J]. COAL GEOLOGY & EXPLORATION, 1993, 21(5): 16-20.

次火山热变质煤的物理测试特征

CHARACTERISTICS OF FTIR,ESR,XRD OF THE COAL METAMORPHIZED BY SUB-VOCANICS

  • 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。

     

    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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