On low index nickel surfaces, repulsive interactions between atomic ox
ygen and CO drive the phase separation of these species into oxygen-ri
ch and GO-rich islands. Because these adsorbates interact differently
with crystallographic steps, the size and the structure of these islan
ds are modified on stepped surfaces. We have monitored coadsorption-in
duced changes in the distribution of CO with IRRAS, observing six diff
erent CO stretching bands which are assigned to distinct local chemiso
rption environments. When oxygen fully saturates sites along the step
edge, the steps are completely blocked from CO adsorption and virtuall
y all the CO population on the terraces shifts from atop to bridge sit
es. This terrace site shift is similarly accomplished by atomic oxygen
chemisorbed at terrace sites. From these coadsorption-induced changes
in CO site distributions, constrained by the 10 Angstrom terrace widt
h, we conclude the through-metal O-CO interaction responsible for this
CO site shift must be operative over a range of 5 Angstrom. At theta(
0) = 0.18 ML, when oxygen occupies, but does not fully saturate the st
ep edge, a new CO adsorption site is created, with a characteristic fr
equency of 1750 cm(-1). This new site is assigned to CO bonded to kink
s along the step edge based upon its low intensity (similar to geometr
ic kink density), enhanced binding strength and sensitivity to oxygen
coverage. At higher oxygen coverages, compression of the CO adlayer is
observed, with CO shifting to asymmetric bridge sites. As saturation
coverage is approached, CO occupies weakly bound sites in close proxim
ity (similar to 3 Angstrom) to O adatoms, with high characteristic fre
quencies of 2100 cm(-1). (C) 1997 Elsevier Science B.V.