SURFACE CHARACTERIZATION STUDY OF THE THERMAL-DECOMPOSITION OF AGO

Citation
Jf. Weaver et Gb. Hoflund, SURFACE CHARACTERIZATION STUDY OF THE THERMAL-DECOMPOSITION OF AGO, Journal of physical chemistry, 98(34), 1994, pp. 8519-8524
Citations number
52
Categorie Soggetti
Chemistry Physical
ISSN journal
00223654
Volume
98
Issue
34
Year of publication
1994
Pages
8519 - 8524
Database
ISI
SICI code
0022-3654(1994)98:34<8519:SCSOTT>2.0.ZU;2-8
Abstract
In this study the thermal decomposition of AgO was examined by collect ing XPS data from a pressed powder AgO sample before and after anneali ng at 100, 200, 300, and 400 degrees C. Comparative data were also col lected from a polycrystalline Ag foil that had been extensively cleane d by annealing at 500 degrees C and sputtering with 2 keV Ar+. However , a mixture of dissolved atomic oxygen and hydroxyl groups characteriz ed by a broad peak in the O 1s spectrum and centered at a binding ener gy (BE) of 531.0 eV remain on the foil after cleaning. The composition al and chemical-state changes that occur on the AgO surface during an anneal are characterized according to the peak intensity and shape cha nges and BE shifts in the XPS spectra. The results show that the BE sh ifts of the Ag 3d peaks from AgO and Ag2O are -0.7 and -0.3 eV relativ e to the metallic state. The predominant form of contamination on the AgO sample is a carbonate or bicarbonate species. The removal of more than 50% of the carbonate contamination during the 100 degrees C annea l results in a fwhm decrease of 0.15 eV in the Ag 3d peaks and narrowi ng of the Ag MNN and valence-band peaks. These peak shapes and BEs are believed to be characteristic of AgO features. Annealing at 200 degre es C results in decomposition of the AgO to Ag2O and complete decompos ition of the carbonate species. Incomplete dissociation of Ag2O at 300 degrees C produces a mixture of Ag2O and Ag metal on the surface whic h yields XPS features characteristic of a combination of both Ag state s. The Ag 3d(5/2) peak is centered at a BE of 367.7 eV, as reported fo r Ag2O, but is broadened (fwhm = 2.1 eV) compared to either the Ag2O o r Ag metal feature. Peak broadening also occurs in both the Ag MNN and valence-band spectra, and the splitting in the Ag MNN peaks decreases relative to the spectra obtained from Ag2O. Annealing at 400 degrees C for 30 min results in nearly complete decomposition of the remaining silver oxide. The XPS spectra closely resemble those obtained from th e Ag foil. Some oxygen remains in the near-surface region as dissolved O or OH, Ag2O, and atomically adsorbed O.