Determination of proton- and oxide ion tracer diffusion in lanthanum tungstate (La/W=5.6) by means of ToF-SIMS

被引:19
作者
Hancke, Ragnhild [1 ]
Fearn, Sarah [2 ]
Kilner, John A. [2 ]
Haugsrud, Reidar [1 ]
机构
[1] Univ Oslo, Dept Chem, FERMiO, NO-0349 Oslo, Norway
[2] Univ London Imperial Coll Sci Technol & Med, Dept Mat, London SW7 2BP, England
基金
英国工程与自然科学研究理事会;
关键词
SURFACE EXCHANGE; OXYGEN DIFFUSION; CONDUCTOR; WATER; SOLUBILITY; DEUTERIUM; HYDROGEN;
D O I
10.1039/c2cp42278f
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
Tracer diffusion of protons and oxide ions, as well as chemical diffusion of water, have been determined for the high temperature proton conductor lanthanum tungstate by means of time-of-flight secondary ion mass spectrometry (ToF-SIMS). The oxygen tracer diffusion and surface exchange coefficients, D*(O) and k*(O), were measured after exchange anneals in water vapor enriched in (H2O)-O-18 between 350 and 620 degrees C, and the apparent activation energies were 176 and 82 kJ mol(-1), respectively. The hydrogen tracer diffusion coefficient (D*(H)) was measured between 220 and 320 degrees C after exchange anneals in D2O-containing atmospheres, and the apparent activation energy was 63 kJ mol(-1). The extracted D*(H) agrees with the results of transient conductivity-and TG-measurements. Chemical diffusion and surface exchange coefficients, D-H(delta) and k(H)(delta), were measured at 250 and 400 degrees C, and the result confirms that the material is hydrated by ambipolar sluggish transport of protons and oxide ions. The surface exchange coefficients were compared to the result of TG relaxation, suggesting that access to oxygen vacancies limits the overall surface exchange reaction under incorporation of water and oxygen.
引用
收藏
页码:13971 / 13978
页数:8
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