Reaction Mechanism of Catalytic Gasification by Calcium-Based Catalysts and Oxidized Coal Residues in Coalfield Fire Zones

IF 1.1 4区 化学 Q3 CHEMISTRY, MULTIDISCIPLINARY Canadian Journal of Chemistry Pub Date : 2024-07-12 DOI:10.1139/cjc-2024-0087
Liangzhou Chen, Wei Lu, Xuyao Qi
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Abstract

Fires originating from coal spontaneous combustion within coalfields result not only in substantial coal resource depletion but also producing residual low-activity pyrolysis coal chars exhibiting varying degrees of oxidation. These chars develop progressively through successive heat penetration at the fire front and post-fire extinguishment phases. This paper focuses on the alkaline earth metal-activated catalytic gasification of residual oxidized coal in fire zones, constructs a carbon-based model of oxidized coal in fire zones. The results show that the reaction active sites of the oxidized coal carbon matrix model are mainly concentrated on the carbon atoms at the end of the aromatic ring. During catalytic gasification, the calcium-based catalyst engages with these active sites, forming a preliminary catalyst. The transformation of oxidized coal into CO primarily occurs through two distinct routes. Calcium attaches to the surface of the oxidized coal's carbon-based structure, establishing active sites. Acting as a facilitator, it aids the movement of CO2 to the carbon-based surface, leading to its further breakdown into CO. The catalytic species containing calcium persistently amalgamates with active sites on coal coke surface, fostering the release of additional CO. Moreover, these catalytic species with calcium also bind CO2 and unite with active coal coke sites, generating carbon-oxygen complexes on the surface. These complexes are thermally unstable and decompose, yielding CO and initiating the formation of fresh active sites on the coal coke surface. Consequently, they interact further with calcium-based catalytic species, culminating in the creation of catalyst precursors, which drive a recurrent catalytic reaction process.
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煤田火区钙基催化剂与氧化煤残渣催化气化的反应机理
煤田内煤炭自燃引起的火灾不仅导致大量煤炭资源枯竭,还会产生残留的低活性热解煤炭,并呈现出不同程度的氧化。这些煤炭是通过火前和火后熄灭阶段的连续热渗透逐步形成的。本文以碱土金属激活催化气化火区残余氧化煤为研究对象,构建了火区氧化煤的碳基模型。结果表明,氧化煤碳基模型的反应活性位点主要集中在芳香环末端的碳原子上。在催化气化过程中,钙基催化剂与这些活性位点接触,形成初步催化剂。氧化煤转化为一氧化碳主要有两种不同的途径。钙附着在氧化煤的碳基结构表面,形成活性位点。作为一种促进剂,它帮助二氧化碳移动到碳基表面,从而进一步分解成二氧化碳。含钙的催化物质会持续与煤焦表面的活性位点结合,促进释放更多的二氧化碳。此外,这些含钙催化剂还能与二氧化碳结合,并与煤焦表面的活性位点结合,在表面生成碳-氧复合物。这些复合物热不稳定,会分解产生二氧化碳,并在煤焦表面形成新的活性位点。因此,它们与钙基催化剂进一步相互作用,最终生成催化剂前体,推动催化反应过程的反复进行。
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来源期刊
Canadian Journal of Chemistry
Canadian Journal of Chemistry 化学-化学综合
CiteScore
1.90
自引率
9.10%
发文量
99
审稿时长
1 months
期刊介绍: Published since 1929, the Canadian Journal of Chemistry reports current research findings in all branches of chemistry. It includes the traditional areas of analytical, inorganic, organic, and physical-theoretical chemistry and newer interdisciplinary areas such as materials science, spectroscopy, chemical physics, and biological, medicinal and environmental chemistry. Articles describing original research are welcomed.
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