陈高健, 曹代勇, 王安民, 等. 添加二氧化硅的煤石墨化高温高压模拟实验[J]. 矿业科学学报, 2024, 9(2): 144-155. DOI: 10.19606/j.cnki.jmst.2024.02.002
引用本文: 陈高健, 曹代勇, 王安民, 等. 添加二氧化硅的煤石墨化高温高压模拟实验[J]. 矿业科学学报, 2024, 9(2): 144-155. DOI: 10.19606/j.cnki.jmst.2024.02.002
CHEN Gaojian, CAO Daiyong, WANG Anmin, et al. High-temperature and high-pressure simulation of coal graphitization with SiO2 additive[J]. Journal of Mining Science and Technology, 2024, 9(2): 144-155. DOI: 10.19606/j.cnki.jmst.2024.02.002
Citation: CHEN Gaojian, CAO Daiyong, WANG Anmin, et al. High-temperature and high-pressure simulation of coal graphitization with SiO2 additive[J]. Journal of Mining Science and Technology, 2024, 9(2): 144-155. DOI: 10.19606/j.cnki.jmst.2024.02.002

添加二氧化硅的煤石墨化高温高压模拟实验

High-temperature and high-pressure simulation of coal graphitization with SiO2 additive

  • 摘要: 为研究自然条件下二氧化硅矿物对煤石墨化作用的影响,将二氧化硅添加剂与分选后的煤中镜质组(来自中国西南部贵州省格目底矿区)充分混合后,开展实验条件为600~1 200 ℃、1.5~2.0 GPa的高温高压模拟实验,对煤系石墨形成环境进行反演。通过X射线衍射、拉曼光谱和高分辨率透射电镜对石墨化产物进行分析,研究二氧化硅对煤的石墨化过程的影响。研究发现,二氧化硅在高温高压环境下存在阻碍石墨化作用的效果,抑制煤石墨化程度的增长。这一结果可为自然条件下构造强烈地区煤石墨化程度较低的现象提供一种解释。

     

    Abstract: This study investigates the effect of SiO2 minerals on coal graphitization under natural conditions through high-temperature and high-pressure simulation experiment to invert the coal-based graphite formation environment.We thoroughly mixed the SiO2 additive with the sorted vitrinite in coal (from the Gemudi mining area in Guizhou provinceSW China) and then carried out high-temperature and high-pressure simulation experiment with ranging from 600 ℃ to 1 200 ℃, 1.5 GPa to 2.0 GPa.The graphitization products of the samples were analyzed by X-ray diffraction, Raman spectroscopy, and high-resolution transmission electron microscopy (HRTEM) to investigate the influence of the SiO2 additive on the process of coal graphitization.Results show that in contrast to the graphitization-promoting ability exhibited in high-temperature environments, SiO2 demonstrates a hindering effect on graphitization in high-temperature and high-pressure environments, inhibiting the growth of coal graphitization.This finding provides an hypothesis for the lower graphitization of coal in areas with strong tectonics under natural conditions.

     

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