The coadsorption system Ag(110)-O/H2O is known to give rise to well de
fined OH layers in a thermally activated process between 190 and 220 K
. In a high resolution EELS study we have found that the (1 x n), n =
3,2 ordered layers produced from the (n x ii, n = 6,4 reconstructed Ag
(110)-O surface are characterized by very sharp loss peaks at 277 cm(-
1) (v(M-OH)) and 3390 cm(-1) (v(O-H)). The dominant M-OH loss exhibits
essentially the same halfwidth as the specular peak, whereas the OH b
ending mode at 675 cm(-1) is significantly broadened and shows a shoul
der at 755 cm(-1). The (1 x 1)-OH phase formed from the (2 x 1)-O reco
nstructed phase is less stable than the lower coverage OH layers. Such
studies may play an important role in understanding the mechanism of
this almost unique stoichiometric reaction.