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新疆准噶尔煤田南部大黄山矿区主煤层自燃动力学研究

Investigation of the kinetics of spontaneous combustion of the major coal seam in Dahuangshan mining area of the Southern Junggar coalfield, Xinjiang, China.

作者信息

Shen Li, Zeng Qiang

机构信息

School of Resource and Environment Sciences, Xinjiang University, Urumqi, 830046, China.

Institute for Arid Ecology and Environment, Xinjiang University, Urumqi, 830046, China.

出版信息

Sci Rep. 2021 Jan 13;11(1):876. doi: 10.1038/s41598-020-79223-z.

Abstract

In the present paper, with using diverse methods (including the SEM, the XRD, the TPO, the FTIR, and the TGA) , the authors analysed samples of the major coal seam in Dahuangshan Mining area with different particle sizes and with different heated temperatures (from 50 to 800 °C at regular intervals of 50 °C). The results from SEM and XRD showed that high temperature and high number of pores, fissures, and hierarchical structures in the coal samples could facilitate oxidation reactions and spontaneous combustion. A higher degree of graphitization and much greater number of aromatic microcrystalline structures facilitated spontaneous combustion. The results from TPO showed that the oxygen consumption rate of the coal samples increased exponentially with increasing temperature. The generation rates of different gases indicated that temperatures of 90 °C or 130 °C could accelerate coal oxidation. With increasing temperature, the coal oxidation rate increased, and the release of gaseous products was accelerated. The FTIR results showed that the amount of hydroxide radicals and oxygen-containing functional groups increased with the decline in particle size, indicating that a smaller particle size may facilitate the oxidation reaction and spontaneous combustion of coal. The absorbance and the functional group areas at different particle sizes were consistent with those of the heated coal samples, which decreased as the temperature rose. The results from TGA showed that the characteristic temperature T declined with decreasing particle size. After the sample with 0.15-0.18 mm particle size was heated, its carbon content decreased, and its mineral content increased, inhibiting coal oxidation. This result also shows that the activation energy of the heated samples tended to increase at the stage of high-temperature combustion with increasing heating temperature.

摘要

在本文中,作者使用多种方法(包括扫描电子显微镜(SEM)、X射线衍射仪(XRD)、程序升温氧化(TPO)、傅里叶变换红外光谱仪(FTIR)和热重分析仪(TGA)),对大黄山矿区主要煤层不同粒径和不同加热温度(从50℃到800℃,每隔50℃)的样品进行了分析。扫描电子显微镜和X射线衍射仪的结果表明,煤样中的高温以及大量的孔隙、裂隙和分级结构会促进氧化反应和自燃。较高的石墨化程度和大量的芳香微晶结构会促进自燃。程序升温氧化的结果表明,煤样的耗氧率随温度升高呈指数增加。不同气体的生成速率表明,90℃或130℃的温度会加速煤的氧化。随着温度升高,煤的氧化速率增加,气态产物的释放加速。傅里叶变换红外光谱仪的结果表明,羟基和含氧官能团的数量随粒径减小而增加,这表明较小的粒径可能会促进煤的氧化反应和自燃。不同粒径下的吸光度和官能团面积与加热后的煤样一致,且随着温度升高而降低。热重分析仪的结果表明,特征温度T随粒径减小而降低。粒径为0.15 - 0.18mm的样品加热后,其碳含量降低,矿物含量增加,抑制了煤的氧化。该结果还表明,加热样品的活化能在高温燃烧阶段会随着加热温度的升高而趋于增加。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c42d/7806908/10e752aa7e62/41598_2020_79223_Fig1_HTML.jpg

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