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Co-adsorption of fluoride and hydroxide ions on Ag(111) in alkaline electrolytes: Electrochemical and SHG studies

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Danckwerts,  Matthias
Physical Chemistry, Fritz Haber Institute, Max Planck Society;

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Savinova,  Elena R.
Physical Chemistry, Fritz Haber Institute, Max Planck Society;

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Horswell,  Sarah L.
Physical Chemistry, Fritz Haber Institute, Max Planck Society;

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Pettinger,  Bruno
Physical Chemistry, Fritz Haber Institute, Max Planck Society;

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Doblhofer,  Karl
Physical Chemistry, Fritz Haber Institute, Max Planck Society;

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10.1524_zpch.217.5.557.20458.pdf
(Publisher version), 165KB

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Citation

Danckwerts, M., Savinova, E. R., Horswell, S. L., Pettinger, B., & Doblhofer, K. (2003). Co-adsorption of fluoride and hydroxide ions on Ag(111) in alkaline electrolytes: Electrochemical and SHG studies. Zeitschrift für Physikalische Chemie, 217(5), 557-572. doi:10.1524/zpch.217.5.557.20458.


Cite as: https://hdl.handle.net/11858/00-001M-0000-0011-120F-9
Abstract
Hydroxide (OH–) adsorption at Ag(111)/alkaline electrolyte interfaces is the initial step leading to the formation of surface oxide. We investigate how OH– anion adsorption is influenced by co-adsorption of supporting electrolyte anions (F–). Pure NaF and NaOH as well as mixed electrolytes ranging from pH=5.8 to 14 are investigated. The rotational anisotropy of the second harmonic generation (SHG) signal is measured to distinguish adsorptive processes from structural changes on the Ag surface. Our results clearly show a crossover from F–-dominated to OH–-dominated adsorption, while both species remain charged upon adsorption. At more positive potentials, but below the reversible potential of bulk oxide growth, OH is discharged leading to sub-monolayer oxide build-up, whereas in acidic electrolyte, Ag is dissolved. At intermediate pH, the formation of a structured OH–/F– co-adsorbed layer is proposed.