Abstract

In order to reveal the distribution characteristics of functional groups and the difference of microcrystalline structure parameters between outburst coal and primary coal, the coal samples inside and outside the outburst holes of the Sanjia coal mine were examined. The functional groups and microcrystalline structure parameters of outburst coal and primary coal in the Sanjia coal mine were studied by infrared spectroscopy, X-ray diffraction (XRD) experiment and peak-splitting fitting method. The results showed that the substitution mode of the benzene ring in an aromatic structure was mainly benzene ring tri-substituted, with primary coal of 32.71% and outburst coal of 31.6%. The primary coal contained more functional groups, from which hydrogen bonds can easily be formed, meaning that gas is not easily adsorbed by coal. The aromatic hydrogen rate (fHa) of the outburst coal was 0.271, the aromatic carbon rate (ƒC) was 0.986, the aromaticity I1 was 0.477, I2 was 0.373 and the length of the aliphatic branched chain (ACH2/ACH3) was 0.850. Compared with the primary coal, the aromatic hydrogen rate, aromatic carbon rate and the aromaticity of the outburst coal were higher, indicating that the hydrogen and carbon elements in the aromatic functional groups of outburst coal were higher and that the aliphatic functional group was higher than the aromatic structural functional group. ACH2/ACH3 and maturity (Csd) were slightly lower than those of primary coal, indicating that the coal has more straight chains than side chains, while aliphatic hydrocarbons are mostly short chains and have high branched degree. There were obvious 002 and 100 peaks in the XRD pattern. The d002 and d100 of outburst coal were 3.570 and 2.114, respectively, while the number of effective stacking aromatics was 3.089, which was lower than that of primary coal, indicating that the structure of the dense ring in the coal saw certain changes.

Highlights

  • IntroductionGuizhou Province in south China has abundant coal resources, wide distribution and complete coal types; the natural occurrence conditions of coal seams in Guizhou are poor, the occurrence of gas is complex and its control is difficult at underground mines [1–3]

  • The analysis shows that the aromatic hydrogen rate and aromatic carbon rate of outburst coal are higher than those of primary coal, indicating that the hydrogen and carbon elements in aromatic functional groups are higher

  • The proximate analysis results show that the volatile matter and moisture content of outburst coal are higher than those of primary coal, but that the ash content is lower than that of primary coal

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Summary

Introduction

Guizhou Province in south China has abundant coal resources, wide distribution and complete coal types; the natural occurrence conditions of coal seams in Guizhou are poor, the occurrence of gas is complex and its control is difficult at underground mines [1–3]. Gas exists in coal or surrounding rock in a free state and suction state [4–8]. The functional group of coal determines the chemical adsorption characteristics of coal, which is mainly controlled by the maceral and mineralogical compositions of coal seams and could indirectly affect the adsorption state of gas by coal seams [9–18]. It is of great significance to study the functional group distribution and microcrystalline structure parameters of coal in order to understand gas occurrence and predict gas disasters

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