Patterns of Formation of Binary Cobalt–Magnesium Oxide Combustion Catalysts of Various Composition

Catalysts Pub Date : 2024-07-03 DOI:10.3390/catal14070425
B. Khussain, Alexandr Sass, Alexandr Brodskiy, Kenzhegul Rakhmetova, Ivan Torlopov, Magira Zhylkybek, T. Baizhumanova, S. Tungatarova, A. Khussain, Murat Zhurinov, A.ZH. Kenessary, Ranida Tyulebayeva, Alexandr Logvinenko, Yernar Narimanov
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Abstract

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.
不同成分的二元钴-氧化镁燃烧催化剂的形成模式
为了确定 Co-Mg 氧化物体系的形成模式,合成并研究了不同 Co:Mg 比例和热处理温度的样品。对样品的研究证实,在 800-900 °C 时,MgxCo2-xO4 尖晶石相变为相应的固溶体。不同成分的形成模式具有相似性。低温样品中的氧化岩盐是一种阴离子修饰的准晶相,只有在尖晶石分解后才会形成 "真正的 "固溶体。分解后的 Co3O4 尖晶石的 TPR 曲线显示出表面 Co3O4 峰和一个与良好结晶的 CoO 相对应的宽峰,而高达 380 °C 的部分 Co3O4 TPR 曲线则显示出分散和无定形的 CoO。高温非均相样品的还原性很差,这表明它们的氧反应活性很低。通过 750 ℃ 煅烧热处理至 1100 ℃ 后的尖晶石再氧化表明,MgCo2O4-Co3O4 样品可完全再生,而相对于化学计量而言过量的氧化镁则不会再生。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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