We have studied the structure of the clean and Cs covered Ag(001) surf
ace, using surface X-ray diffraction. For the clean unreconstructed Ag
(001) surface the analysis of the integer-order crystal truncation rod
s gives evidence for a compression of the first interlayer spacing rel
ative to the bulk by Delta d(12)/d(bulk) = -0.8(8)%, whereas for the s
econd interlayer spacing we obtain an expansion of Delta d(23)/d(bulk)
= 1.0(8)%. For the first two Ag layers we observe enhanced thermal di
sorder as expressed by the isotropic mean-squared displacement amplitu
de, U = 0.011(1) Angstrom(2) at 340 K relative to the bulk value of 0.
009 Angstrom 2 at this temperature. Our X-ray results for Ag(001) are
in good agreement with previous experimental and theoretical results.
The adsorption of 0.25ML (1 ML = 1.25 x 10(15) adatoms/cm(2)) Cs on th
e Ag(001) surface at 170K leads to the formation of a c(2 x 4) superst
ructure. The Cs atoms are found to occupy fourfold hollow sites at dc(
s) = 2.49(20) Angstrom above the Ag(001) surface thereby shifting the
underlying Ag atoms laterally by 0.029(5) Angstrom from their bulk pos
itions. From the adsorption height we derive an effective Cs radius of
1.78(16) Angstrom. Large anisotropic disorder is observed for the Cs
adatoms. Within the harmonic approximation we derive mean-squared disp
lacement amplitudes of U-11 = 0.08(1) Angstrom(2), U-22 = 0.10(1) Angs
trom(2) and U-33 = 0.27(3) Angstrom(2). An alternative model, suggeste
d by the very large value of U-33, was also tried, in which there are
15% of Ag vacancies in the top layer and a lower Cs site. This 'unusua
l' model is discussed in the context of current theories of alkali met
al induced reconstructions.