Abstract
A composition- and temperature-dependent mobility database of all ionic species in the LaCoO3-δ
phase was developed and combined with a La-Co-O thermodynamic database
to simulate kinetic demixing and partial decomposition in LaCoO3-δ oxygen membranes operated under a 0.0001/0.21 bar oxygen partial pressure difference at 1073 K for 1 year. Formation of La2O3, Co3O4
and CoO phases across the membrane is predicted. The kinetic demixing
process can be divided into two stages, namely, establishment of the
oxygen potential gradient (fast) and demixing of the cations (slow); the
former is controlled by the mobility of oxygen ions, and the latter is
determined by the higher mobility of Co ions as compared to the La ion
in the ABO3-type perovskite. A drift motion of both oxide surfaces towards the high PO2 side occurs with the movement of cations.
| Original language | English |
|---|---|
| Journal | Journal of Membrane Science |
| Volume | 548 |
| Pages (from-to) | 526-539 |
| ISSN | 0376-7388 |
| DOIs | |
| Publication status | Published - 2018 |
Keywords
- LaCoO3-δ
- Kinetic demixing/decomposition
- Oxygen potential gradient
- Oxygen membrane
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