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含气煤水润湿过程中的气体驱替特征及微观影响机制

Gas displacement characteristics during the water wetting process of gas-bearing coal and microscopic influence mechanism.

作者信息

Yue Jiwei, Xu Jinlin, Zhang Jianguo, Shi Biming, Zhang Mingyue, Li Yang, Wang Chen

机构信息

School of Safety Science and Engineering, Anhui University of Science and Technology, Huainan 232001, China; Pingdingshan Tian'an Coal Industry Co., Ltd., Pingdingshan 467036, China; State Key Laboratory of Coking Coal Exploitation and Comprehensive Utilization, Pingdingshan 467000, China.

School of Safety Science and Engineering, Anhui University of Science and Technology, Huainan 232001, China.

出版信息

Sci Total Environ. 2024 Nov 1;949:175034. doi: 10.1016/j.scitotenv.2024.175034. Epub 2024 Jul 25.

Abstract

Gas and dust posed a threat to the safe working environment of miners. The key to the effectiveness of coal seam water injection in controlling gas and dust was the wetting of the coal body by water. The gas displacement characteristics were crucial for evaluating the wetting effect of coal. To investigate gas displacement characteristics during the water wetting process of gas-bearing coal, this study employed an experimental equipment of water wetting gas-bearing coal to test the gas displacement quantity under varying gas pressure conditions, and the microscopic influence mechanism was revealed. During the water wetting gas-bearing coal, there was an increase in the accumulated displacement gas quantity corresponding to rising adsorption equilibrium pressures, whereas the accumulated displacement gas rate decreased. Water wetting progressively reduced the system's Helmholtz free energy, reaching a minimum at equilibrium, indicative of a balanced wetting state. The displacement gas quantity curve initially rose linearly, reflecting rapid infiltration, then curved upwards more gradually as gravity and viscosity slowed the process, until reaching a relatively stable state. The curve mirrored the coal's saturation progression. The molecular formula of anthracite was CHNO. Elemental compositions of carbon, hydrogen, oxygen, and nitrogen matched elemental analysis results. The bridge carbon ratio of this molecular model was aligning with the bridge carbon ratio ascertained from the C NMR spectrum analysis. Above the coal-water interface, the relative concentration of water molecules increased with the increase of gas pressure. However, below the coal and water interface, the relative concentration of water molecules increased with the decrease of gas pressures. As the gas pressure increased, the adsorption degree of water molecules weakened, the degree of gas displacement in coal decreased, the diffusion coefficient of methane molecules decreased, the dispersion degree of water molecules increased, the aggregation degree weakened, and the diffusion coefficient of water molecules increased. The study results laid a theoretical foundation for revealing the mechanism of coal seam water injection wetting gas-bearing coal, achieving collaborative gas disaster prevention and pre-wetting dust reduction.

摘要

瓦斯和粉尘对矿工的安全工作环境构成威胁。煤层注水控制瓦斯和粉尘效果的关键在于水对煤体的湿润作用。瓦斯置换特性对于评估煤的湿润效果至关重要。为了研究含瓦斯煤水湿润过程中的瓦斯置换特性,本研究采用含瓦斯煤水湿润实验装置,测试了不同瓦斯压力条件下的瓦斯置换量,并揭示了微观影响机制。在含瓦斯煤水湿润过程中,随着吸附平衡压力升高,累计置换瓦斯量增加,而累计置换瓦斯速率降低。水湿润使系统的亥姆霍兹自由能逐渐降低,在平衡时达到最小值,表明处于平衡湿润状态。置换瓦斯量曲线最初呈线性上升,反映快速渗透,随后随着重力和粘度使过程减缓,曲线上升逐渐变缓,直至达到相对稳定状态。该曲线反映了煤的饱和度变化过程。无烟煤的分子式为CHNO。碳、氢、氧、氮的元素组成与元素分析结果相符。该分子模型的桥碳比与通过碳核磁共振谱分析确定的桥碳比一致。在煤 - 水界面上方,水分子的相对浓度随瓦斯压力升高而增加。然而,在煤与水界面下方,水分子的相对浓度随瓦斯压力降低而增加。随着瓦斯压力升高,水分子的吸附程度减弱,煤中瓦斯置换程度降低,甲烷分子扩散系数减小,水分子分散程度增加,聚集程度减弱,水分子扩散系数增大。研究结果为揭示煤层注水湿润含瓦斯煤的机理、实现协同瓦斯灾害防治和预湿降尘奠定了理论基础。

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