The adsorption of oxygen on two different stepped Ru(001) surfaces (n(
001) x 1(010) with n = 13 or 39) was investigated by LEED. For the hig
h (low) step density surface, saturation with oxygen leads to a (2 x 2
) LEED pattern with broadened spots of sixfold symmetry at normal inci
dence in the temperature regime between 300 and 500 (750) K. This is d
ue to the incoherent superposition of diffraction from the two nonequi
valent terrace types separated by monoatomic steps. After annealing to
temperatures between 500 (750) K and 1200 K or adsorption at these te
mperatures, however, the patterns become threefold symmetric correspon
ding to the threefold symmetry of one terrace. Using spot profile anal
ysis and the comparison of experimental LEED-IV curves as analytical t
ools, we conclude that only one type of terrace, separated by double s
teps, is present after annealing, and that the local geometry within t
he terraces is the same as on the nominally flat surface in both tempe
rature regimes. The predominant terrace type for higher adsorption tem
peratures can be identified by comparison of the experimental IV curve
s with calculated curves. In doing so, we find that the step face cont
ains a fourfold hollow site whose occupation by oxygen is proposed to
be the driving force for this surface reconstruction with considerable
material transport.