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煤-高岭石复合煤矸石狭缝模型中CO生成与吸附的分子模拟

Molecular simulation of CO production and adsorption in a coal-kaolinite composite gangue slit model.

作者信息

Zhang Jing, Li Zhi, Li Xuping, Ren Xiaopeng, Zhou Chenhong, Li Tianyu

机构信息

School of Mining and Coal, Inner Mongolia University of Science and Technology China

Inner Mongolia Key Laboratory of Mining Engineering China.

出版信息

RSC Adv. 2024 Jun 17;14(27):19301-19311. doi: 10.1039/d4ra03151b. eCollection 2024 Jun 12.

Abstract

To reveal the mechanism of CO gas generation and adsorption in coal gangue slits at the microscopic level, a new composite kaolinite-coal-kaolinite (KCK) slit model was constructed by combining the Hongqingliang (HQL) coal molecular model and the Bish kaolinite model to characterize the crack structure of the gangue. It is compared with the kaolinite model (TriK) commonly used in gangue research. Molecular dynamics was used to study the production of CO in different oxygen environments and variation in the adsorption amount, adsorption sites and diffusion coefficient in the temperature range from 293.15 K to 333.15 K. The results indicate that CO mainly comes from the decomposition of ether and phenol in organic structures, and the lower the oxygen concentration, the lesser the CO production time. The KCK model has a higher average adsorption capacity and weaker diffusion capacity mainly due to the additional adsorption sites provided by the carbon-containing structural layer, and CO is mainly adsorbed near the oxygen-containing functional groups. Although kaolinite exhibits bonding adsorption on the Al-O plane, its adsorption site is limited to the surface. The slit model with the carbon structure can better reflect the complex conditions of gas motion in the gangue, thus providing a reference to determine the spontaneous combustion conditions of the gangue hill the index gas.

摘要

为了在微观层面揭示煤矸石孔隙中CO气体产生与吸附的机制,通过结合红庆梁(HQL)煤分子模型和比什高岭石模型构建了一种新的复合高岭石-煤-高岭石(KCK)孔隙模型,以表征煤矸石的裂隙结构。将其与煤矸石研究中常用的高岭石模型(TriK)进行比较。利用分子动力学研究了不同氧环境下CO的产生以及在293.15 K至333.15 K温度范围内吸附量、吸附位点和扩散系数的变化。结果表明,CO主要来自有机结构中醚和酚的分解,氧浓度越低,CO产生时间越短。KCK模型具有较高的平均吸附容量和较弱的扩散能力,主要是由于含碳结构层提供了额外的吸附位点,且CO主要吸附在含氧官能团附近。虽然高岭石在Al-O平面上表现出键合吸附,但其吸附位点仅限于表面。具有碳结构的孔隙模型能够更好地反映煤矸石中气体运移的复杂情况,从而为确定煤矸石山自燃条件的指标气体提供参考。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/86b4/11181295/eb3c10500710/d4ra03151b-f1.jpg

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