“…O  is identified by an O 1s binding energy between 530.0 and 531.0 eV [12,26,29,30,40,48], a Ag-O stretching frequency of 640 cm −1 when incorporated between the top two layers of a reconstructed Ag(1 1 1) surface [12,23,26,27,31], and gives a broad O 2 desorption signal between 680 and 800 K [13,16,17,28,31]. Grain boundaries or related dislocations in the silver structure facilitate the formation of the O  [10,11,15,16,23,24,31,45]. At temperatures above 773 K, O  formation is accompanied by bulk restructuring into facets of (1 1 1) texture [12,[14][15][16][17]19,[26][27][28][29][30][31][46][47][48].…”