The formation of chemisorbed O phases on Ru(0001) by exposure to O-2 a
t low pressures is apparently limited to coverages Theta less than or
equal to 0.5. Using low-energy electron diffraction and density-functi
onal theory we show that this restriction is caused by kinetic hinderi
ng and that a dense O overlayer (Theta = 1) can be formed with a (1 x
1) periodicity. The structural and energetic properties. of this new a
dsorbate phase are analyzed and discussed in view of attempts to bridg
e the so-called ''pressure gap'' in heterogeneous catalysis. It is arg
ued that the identified system actuates the unusually high rate of oxi
dizing reactions at Ru surfaces under high oxygen pressure conditions.