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关于铁/氮/碳氧还原催化剂在热解条件下合成过程中如何演变的原位研究。

An in situ exploration of how Fe/N/C oxygen reduction catalysts evolve during synthesis under pyrolytic conditions.

作者信息

Yin Shuhu, Yi Hongyuan, Liu Mengli, Yang Jian, Yang Shuangli, Zhang Bin-Wei, Chen Long, Cheng Xiaoyang, Huang Huan, Huang Rui, Jiang Yanxia, Liao Honggang, Sun Shigang

机构信息

State Key Laboratory of Physical Chemistry of Solid Surfaces, Engineering Research Center of Electrochemical Technologies of Ministry of Education, College of Chemistry and Chemical Engineering, and Discipline of Intelligent Instrument and Equipment, Xiamen University, Xiamen, 361005, P. R. China.

Center of Advanced Electrochemical Energy, Institute of Advanced Interdisciplinary Studies, School of Chemistry and Chemical Engineering, Chongqing University, Chongqing, 400044, PR China.

出版信息

Nat Commun. 2024 Jul 24;15(1):6229. doi: 10.1038/s41467-024-50629-x.

Abstract

In pursuing cheap and effective oxygen reduction catalysts, the Fe/N/C system emerges as a promising candidate. Nevertheless, the structural transformations of starting materials into Fe- and N-doped carbon catalysts remains poorly characterized under pyrolytic conditions. Here, we explore the evolution of Fe species and track the formation of Fe-N site development by employing diverse in-situ diagnostic techniques. In-situ heating microscopy reveals the initial formation of FeO nanoparticles and subsequent internal migration within the carbon matrix, which stops once FeO is fully reduced. The migration and decomposition of nanoparticles then leads to carbon layer reconstruction. Experimental and theoretical analysis reveals size-dependent behavior of FeO where nanoparticles below 7 nm readily release Fe atoms to form Fe-N while nanoparticles with sizes >10 nm tend to coalesce and impede Fe-N site formation. The work visualizes the pyrolysis process of Fe/N/C materials, providing theoretical guidance for the rational design of catalysts.

摘要

在寻求廉价且高效的氧还原催化剂时,铁/氮/碳体系成为了一个有前景的候选者。然而,在热解条件下,起始材料向铁和氮掺杂的碳催化剂的结构转变仍未得到充分表征。在此,我们通过采用多种原位诊断技术来探索铁物种的演变,并追踪铁氮位点的形成过程。原位加热显微镜揭示了FeO纳米颗粒的初始形成以及随后在碳基质中的内部迁移,一旦FeO完全还原,迁移就会停止。纳米颗粒的迁移和分解随后导致碳层重构。实验和理论分析揭示了FeO的尺寸依赖性行为,其中尺寸小于7纳米的纳米颗粒容易释放铁原子以形成Fe-N,而尺寸大于10纳米的纳米颗粒倾向于聚结并阻碍Fe-N位点的形成。这项工作可视化了铁/氮/碳材料的热解过程,为催化剂的合理设计提供了理论指导。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cb80/11266712/55cf8f2a5384/41467_2024_50629_Fig1_HTML.jpg

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