氧气
透氧性
钙钛矿(结构)
材料科学
磁导率
碳酸盐
氧气输送
化学
化学工程
膜
无机化学
结晶学
冶金
生物化学
工程类
有机化学
作者
Jianfang Zhou,Xia Tang,Chengzhang Wu,He Wang,Kun Zhang,Weizhong Ding,Yonggang Jin,Chenghua Sun
标识
DOI:10.1021/acs.jpcc.5b05920
摘要
In this study, the degradation and recovery mechanisms of perovskite Ba1.0Co0.7Fe0.2Nb0.1O3−δ (BCFN) membrane under a CO2-containing atmosphere were investigated. The oxygen permeability of the BCFN membrane is degraded quickly with pure CO2 gas in the sweep side and then would be partially recovered if the sweep gas changes to 5% CO2. It is found that the existence of oxygen can stabilize the cubic perovskite structure of BCFN. Isotopic exchange test confirms the fast exchange of oxygen between the lattice oxygen of BCFN bulk and the oxygen in the formed carbonate. Pores or cracks are generated during the dynamical exchange of oxygen and serve as the permeable channels of oxygen, resulting in the partial recovery of oxygen permeability under 5% CO2 concentration.
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