氧气
氧气储存
钴
分压
氧化物
大气温度范围
氧化钴
化学
可控气氛
极限氧浓度
大气(单位)
固体氧
材料科学
化学工程
无机化学
冶金
有机化学
热力学
工程类
物理
作者
Teruki Motohashi,S. Kadota,H. Fjellvåg,Maarit Karppinen,H. Yamauchi
标识
DOI:10.1016/j.mseb.2007.09.052
摘要
An uncommon oxygen intake/release phenomenon was discovered for the layered cobalt oxide system, REBaCo4O7+δ (RE = Dy, Y, Yb, and Lu). Compounds, REBaCo4O7+δ, can intake oxygen up to δ ≈ 1.3 and release it in atmospheric O2 as temperature increases in a narrow range below 400 °C. The oxygen intake/release processes are highly reversible, being controlled by both temperature and/or oxygen partial pressure. The oxygen-rich phase (with δ = 1.0–1.3) releases upon heating all excess oxygen atoms in a single-step process about 400 °C, whereas oxygen intake occurs in the temperature range of 200–350 °C when slowly cooled in an O2-containing atmosphere. The oxygen intake/release characteristics are also strongly dependent on the choice of RE. This suggests that the crystal structure of the compounds is the key for this uncommon phenomenon. Obviously these compounds are promising candidates for oxygen-storage applications.
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