尖晶石
煅烧
化学计量学
氧化钴
氧化物
材料科学
钴
无机化学
无定形固体
分解
相(物质)
固溶体
催化作用
化学工程
化学
物理化学
结晶学
冶金
有机化学
工程类
生物化学
作者
Bolatbek Khussain,A.S. Sass,Alexandr Brodskiy,Kenzhegul Rakhmetova,Ivan Torlopov,Magira Zhylkybek,Т.С. Байжуманова,С.А. Тунгатарова,Atabek Khussain,M. Zh. Zhurinov,Abzal Kenessary,Ranida Tyulebayeva,Alexandr Logvinenko,Yernar Narimanov
出处
期刊:Catalysts
[Multidisciplinary Digital Publishing Institute]
日期:2024-07-03
卷期号:14 (7): 425-425
标识
DOI:10.3390/catal14070425
摘要
In order to establish the formation patterns of the Co–Mg oxide system, samples with different Co:Mg ratios and heat treatment temperatures were synthesized and studied. A study of the samples confirmed the phase transition of MgxCo2–xO4 spinels into the corresponding solid solutions at 800–900 °C. The similarity of the formation patterns for different compositions is shown. The rocksalt oxide in low-temperature samples is an anion-modified paracrystalline phase that forms a “true” solid solution only upon spinel decomposition. The TPR profiles of the decomposed Co3O4 spinel show surface Co3O4 peaks and a wide peak corresponding to the well-crystallized CoO, while partial Co3O4 TPR up to 380 °C results in dispersed and amorphous CoO. The high-temperature non-stoichiometric samples are poorly reduced, indicating their low oxygen reactivity. Spinel reoxidation after heat treatment to 1100 °C by calcination at 750 °C showed complete regeneration for MgCo2O4–Co3O4 samples and its absence in case of an excess of MgO relative to stoichiometry.
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