西山矿区煤层煤结构的 FTIR 特征研究

    FTIR characteristics of coal seam structure in Xishan Mining Area

    • 摘要: 为了研究西山矿区的煤结构特征,借助傅里叶红外光谱技术(FTIR)对屯兰矿7个不同煤层的原煤样品的化学结构进行了分析表征。光谱特征曲线结果表明:各煤层样品在 3 600 cm−1以下的宽阔频带的出现是由OH伸缩振动引起的,样品的最大吸收位于3 430~3 400 cm−1附近;02#、2#、7#、8#、9#煤样品在 800~1 800 cm−1频带上振动较强,该范围内多为含氧官能团,主要包括羟基(醇羟基和酚羟基)、羧基、羰基等,这些基团本身具有很强的亲水性,增加了煤内部结构的含水率,导致自身的能量密度降低,不利于煤的深加工和利用。通过对FTIR吸收峰归属研究、图谱分析与拟合,获得与煤成熟度相关的基于FTIR技术的芳碳率(fa-FTIR)值;通过建立试验研究获得的fa-FTIR值与理论芳碳率(fa-T)值之间的回归模型,得出两者之间的正相关系数R2=0.804,表明采用FTIR技术计算出的芳碳率是可靠的;通过研究煤变质程度(最大反射率Rmax)与红外结构参数的相关性,发现随着Rmax增大,芳碳率fa-FTIR增大,生烃潜力‘A’降低,此阶段煤化会使煤中芳香烃类物质增多。

       

      Abstract: In order to study the characteristics of coal structure in Xishan Mining area, the chemical structure of raw coal samples from 7 different coal seams in Tunlan Mine in Xishan Mining area was analyzed and characterized by Fourier infrared spectroscopy (FTIR). The results of spectral characteristic curves show that: the wide frequency band below 3 600 cm−1 of each coal seam sample is caused by OH stretching vibration; the maximum absorption of the sample is in the vicinity of 3 430-3 400 cm−1; coal samples 02#, 2#, 7#, 8#, and 9# vibrate strongly in the 800-1 800 cm−1 frequency band, in which there are mostly oxygen-containing functional groups, mainly including hydroxyl group (alcohol hydroxyl group and phenolic hydroxyl group), carboxyl group, carbonyl group, etc. These groups themselves have strong hydrophilicity, increasing the water content of coal internal structure, resulting in a decrease in their own energy density. It is not conducive to the deep processing and utilization of coal. Through the study of FTIR absorption peak attribution, spectrum analysis and fitting, the aryl carbon ratio (fa-FTIR) value based on FTIR technology related to coal maturity was obtained; the regression model between the experimental value of fa-FTIR and the theoretical arylene carbon rate (fa-T) is established, and the positive correlation coefficient R2=0.804 is obtained, indicating that the arylene carbon rate calculated by FTIR is reliable. By studying the correlation between the metamorphic degree of coal (the maximum reflectance Rmax) and infrared structural parameters, it is found that with the increase of Rmax, the aryl carbon rate fa-FTIR increases, and the hydrocarbon generation potential ‘A’ decreases. At this stage, coalification will increase the aromatic hydrocarbons in coal.

       

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