We have obtained the first far infrared measurement of an atomic adsor
bate-substrate stretch on a single crystal surface. The infrared refle
ction-absorption technique is employed on O/Ag(110), with an apparatus
consisting of a laboratory source of infrared radiation, an evacuated
FTIR, and a He-cooled bolometer detector. Complementary STM measureme
nts, performed in situ, allowed rigorous characterization of surface s
tructure. At room temperature and the lowest detectable coverage (0.14
ML), the frequency of the O-Ag symmetric stretch is (v) over tilde(ss
) = 319 +/- 1 cm(-1). This band shifts continuously upwards to 335 +/-
1 cm(-1) as coverage is increased to 0.5 ML, where the (2 x 1)-0 phas
e is fully developed. The intensity of this dipole transition is analy
zed with a standard Lorentz oscillator model. The effective charge tra
nsfer for the oscillating dipolar complex is evaluated at just 0.036 /- 0.005e(-), indicating that the O/Ag(110) bond is polar covalent in
character. Since the observed frequency shift cannot result from simpl
e dipole-dipole interactions alone, other physical origins are discuss
ed.