Zhang Xiao, Tang Jupeng
School of Civil Engineering, Liaoning Technical University, Fuxin, Liaoning 123000, P R China.
College of Environment, Shenyang University, Shenyang, Liaoning 110044, P R China.
ACS Omega. 2025 Feb 20;10(8):7937-7948. doi: 10.1021/acsomega.4c08809. eCollection 2025 Mar 4.
Massive quantities of NH generated after blasting in underground coal mines are believed to enhance the adsorption of O by coal and accelerate the rate of coal's spontaneous combustion oxidation. The adsorption behavior of coal for NH and O after blasting in underground coal mines provides critical insights into the mechanisms of coal's spontaneous combustion. This research was conducted on Xiaolongtan lignite, examining the adsorption characteristic of NH/O binary gas mixtures and single-component NH and O on lignite at 278.15-323.15 K and 0-500 kPa using Grand Canonical Monte Carlo simulations. Additionally, the kinetic properties of the lignite/NH and lignite/O systems were analyzed at 278.15-323.15 K using molecular dynamics simulations. The results revealed that the adsorption isotherms conformed well to the Langmuir equation. Under the specified conditions, the adsorption amount of lignite decreased with increasing temperature, and the gas adsorption amount followed the order: NH > O. The adsorption selectivity coefficient of NH and O was largely unaffected by the molar ratio but decreased as the temperature increased. The integral area of the relative concentration curve confirmed that the adsorption of NH and O onto lignite decreased with increasing temperature, maintaining the order NH > O. Under identical temporal conditions, the mean square displacement and diffusion coefficients of the gases increased with temperature, with O exhibiting a higher diffusion coefficient than NH. Furthermore, the interaction energy of the lignite/NH and lignite/O systems decreased as the temperature increased, with NH exhibiting the strongest interactions with lignite at the same temperature.
地下煤矿爆破后产生的大量氨气被认为会增强煤对氧气的吸附作用,并加速煤自燃氧化的速率。地下煤矿爆破后煤对氨气和氧气的吸附行为为煤自燃的机理提供了关键见解。本研究以小龙潭褐煤为对象,采用巨正则蒙特卡罗模拟方法,研究了在278.15 - 323.15 K和0 - 500 kPa条件下褐煤对氨/氧二元混合气体以及单一组分氨气和氧气的吸附特性。此外,利用分子动力学模拟分析了在278.15 - 323.15 K条件下褐煤/氨气和褐煤/氧气体系的动力学性质。结果表明,吸附等温线与朗缪尔方程拟合良好。在规定条件下,褐煤的吸附量随温度升高而降低,气体吸附量顺序为:氨气>氧气。氨气和氧气的吸附选择性系数在很大程度上不受摩尔比影响,但随温度升高而降低。相对浓度曲线的积分面积证实,褐煤对氨气和氧气的吸附量随温度升高而降低,且保持氨气>氧气的顺序。在相同时间条件下,气体的均方位移和扩散系数随温度升高而增大,氧气的扩散系数高于氨气。此外,褐煤/氨气和褐煤/氧气体系的相互作用能随温度升高而降低,在相同温度下,氨气与褐煤的相互作用最强。