Surface-oxide growth at platinum electrodes in aqueous H2SO4 Reexamination of its mechanism through combined cyclic-voltammetry, electrochemical quartz-crystal nanobalance, and Auger electron spectroscopy measurements

被引:396
作者
Jerkiewicz, G
Vatankhah, G
Lessard, J
Soriaga, MP
Park, YS
机构
[1] Queens Univ, Dept Chem, Kingston, ON K7L 3N6, Canada
[2] Univ Kashan, Nano SciTech Ctr, Kashan 87314, Iran
[3] Univ Sherbrooke, Dept Chim, Sherbrooke, PQ J1K 2R1, Canada
[4] Texas A&M Univ, Dept Chem, College Stn, TX 77843 USA
基金
加拿大自然科学与工程研究理事会; 美国国家科学基金会;
关键词
platinum oxide growth; electrochemical quartz-crystal nanobalance; Auger electron spectroscopy; oxide growth mechanism;
D O I
10.1016/j.electacta.2003.11.008
中图分类号
O646 [电化学、电解、磁化学];
学科分类号
081704 ;
摘要
The mechanism of platinum surface electro-oxidation is examined by combined cyclic-voltammetry (CV), in situ electrochemical quartz-crystal nanobalance (EQCN) and ex situ Auger electron spectroscopy (AES) measurements. The CV, EQCN and AES data show that the charge density, interfacial mass variation and intensity of the O-to-Pt AES signal ratio increase in a continuous, almost linear manner as the potential is raised from 0.85 to 1.40 V. In addition, the charge density, mass variation and O-to-Pt signal ratio profiles, follow each other, thus indicating that the surface oxidation proceeds by a progressive coordination of O-containing species to the Pt substrate. The coupled CV and EQCN measurements lead to in situ determination of the molecular weight of the interfacial species; these were identified as chemisorbed O (O-chem) at 0.85 less than or equal to E less than or equal to 1.10 V and as O2- in the form of a surface PtO at 1.20 less than or equal to E less than or equal to 1.40 V. The AES results reveal that the first half-monolayer of O-chem is formed through discharge of H2O molecules and such formed O-chem resides on the Pt surface. Subsequent discharge of H2O molecules leads to formation of the second half-monolayer of O,h,m that is accompanied by the interfacial place exchange Of O,h,,,, and surface Pt atoms; this process results in the development of a quasi-3D surface PtO lattice comprising Pt2+ and O2-. AES data demonstrate that the place-exchange process occurs in the 1.10 - 1.20 V potential range. The experimentally determined molecular weight of the species added to the surface is 15.8 g mol(-1), which points to O and to anhydrous PtO as the surface oxide formed. (C) 2003 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1451 / 1459
页数:9
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