Effect of A and B-site cations on surface exchange coefficient for ABO3 perovskite materials

被引:84
作者
Armstrong, Eric N. [1 ]
Duncan, Keith L. [1 ]
Wachsman, Eric D. [2 ]
机构
[1] Univ Florida, Florida Inst Sustainable Energy, Gainesville, FL 32611 USA
[2] Univ Maryland, Energy Res Ctr, College Pk, MD 20742 USA
关键词
OXYGEN SELF-DIFFUSION; ELECTRICAL-CONDUCTIVITY; TRACER DIFFUSION; ION-TRANSPORT; OXIDE IONS; PART I; KINETICS; LAFEO3; NONSTOICHIOMETRY; RELAXATION;
D O I
10.1039/c2cp42919e
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
A novel approach, called isothermal isotope exchange (IIE), was applied to varying A- and B-site lanthanum manganites, ferrites, and cobaltites in the perovskite crystal structure in order to extract accurate surface exchange coefficients (k*). Pure electronic conductors revealed temperature dependent isotope exchange, while for mixed ionic and electronic conductors (MIEC) the extent of exchange was independent of temperature. MIEC materials have higher k* values than pure electronic conductors in the temperature range from 500-850 degrees C, demonstrating the importance of both electronic species and oxygen vacancies being present for surface exchange. Strontium doped perovskites exhibited opposite temperature dependencies to parent materials. Some perovskites exhibited an apparent negative activation energy for k*, the behavior of which is explained by a precursor-mediated mechanism for dissociative adsorption. The results have significant implications for the improvement of the oxygen reduction reaction for fuel cells, metal-air batteries, and numerous other energy technologies.
引用
收藏
页码:2298 / 2308
页数:11
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