We report measurements of the kinetics of scanned probe oxidation under con
ditions of high humidity and pulsed bias. For a hydrophobic Si surface the
oxidation rate for short pulse times (similar to 10 ms) is controlled by th
e density of H2O molecules in the ambient humidity surrounding the tip-samp
le interface. At longer pulse times (similar to 0.1 s) liquid H2O bridges t
his interface and the maximum oxidation rate increases by a factor of simil
ar to 10(4) because of the increased density of H2O molecules. We propose t
hat the rate-limiting step of the oxidation process is the production of O
anions from the ambient humidity. (C) 2000 American Institute of Physics. [
S0003-6951(00)04013-4].