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添加二氧化硅的煤石墨化高温高压模拟实验OA北大核心CSTPCD

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

中文摘要英文摘要

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.

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 Ge-mudi mining area in Guizhou province[SW China])and then carried out high-temperature and high-pressure simulation experiment with ranging from 600℃to 1200℃,1.5 GPa to 2.0 GPa.The graphitization products of the samples were analyzed by X-ray diffraction,Raman spectroscopy,and high-resolution trans-mission 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.

陈高健;曹代勇;王安民;魏迎春;刘志飞;赵萌

中国矿业大学(北京) 地球科学与测绘工程学院,北京 100083||地球化学过程与资源环境效应湖南省重点实验室,湖南长沙 410116中国矿业大学(北京) 地球科学与测绘工程学院,北京 100083

地质学

煤系石墨高温高压二氧化硅添加剂石墨化

coal-based graphitehigh temperature and high pressureSiO2 additivegraphitization

《矿业科学学报》 2024 (002)

惰质组与镜质组大分子结构演化差异性及其动力学机制

144-155 / 12

国家自然科学基金(42072197,41902170,41772156)

10.19606/j.cnki.jmst.2024.02.002

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