In situ scanning tunneling microscopy (STM) has been applied to study adsorption and oxide formation on Cu(111) in weakly alkaline, neutral, and acidic sulfate-containing solutions. In 5 × 10 − 4 M NaOH + 5 × 10 − 3 M Na 2 SO 4 ( pH ∼ 10.5 ) , a hexagonally structured OH layer is formed at potentials well below oxide formation despite the tenfold larger sulfate concentration showing a stronger interaction of OH − with the Cu surface than SO 4 2 − . In 5 × 10 − 3 M Na 2 SO 4 ( pH ∼ 7 ) , a partially structured and highly mobile adlayer is formed at potentials quite near the onset of oxide formation with coexisting ( 3 × 3 ) -ordered domains and nonordered domains. This is assigned to the competitive adsorption of water molecules with sulfate anions. In contrast, a highly ordered and stable ( 3 × 7 ) adsorbed layer is formed in 5 × 10 − 3 M H 2 SO 4 . It is assigned to the coadsorption of sulfate anions and cations ( H 3 O + or H + ) , the latter compensating the repulsive forces between sulfate anions and thus stabilizing the adlayer. The anodic Cu(I) oxide is (111)-oriented and has a faceted surface in solutions of alkaline, weakly alkaline, and neutral pH.
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Maurice et al. (2003) studied this question.
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