Kinetic Energy Effects on the Oxidation of Ni(111)
Using Molecular Oxygen Beams
ABSTRACT -
The oxidation kinetics of the Ni(111) surface have been quantitatively examined utilizing kinetic
energy selected supersonic beams of molecular oxygen. Using in
situ high-resolution
electron-energy-loss spectroscopy, we have observed notable differences in the oxidation mechanism for
this interface as a function of incident beam energy. Exposure of a 300 K surface to a
relatively low energy 60 meV O2 beam leads to
oxidation kinetics which follow an island growth
model, qualitatively similar to what is seen with simple ambient gas dosing. In contrast to this,
exposure to a relatively high energy 600 meV O2
beam yields fundamentally different oxidation
behavior: the kinetics of oxidation no longer follow an island growth
model but rather behave with
a Langmuir-like sticking model, implying key differences in the nucleation stage for interface
oxidation. Cryogenically cooled Ni(111) could not be oxidized using either of these incident beam
conditions, indicating that the energetic constraints needed to move from oxygen chemisorption
to actual metallic oxidation cannot be simply overcome using incident O2
kinetic energy.
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The kinetic energy dependent oxidation data were obtained by
alternately dosing the
crystal with a supersonic beam and monitoring the dipole-allowed oxygen vibrations (~65 meV
energy loss) in situ with HREELS. Because the spectra were
acquired with a low electron beam
energy of 3.5 eV at a small current density of 2 nA/cm2, the probe electrons did not cause any
extraneous effects on the oxidation kinetics.
Two different beams were used to oxidize the
crystal: one beam, neat O2 expanded from a room
temperature nozzle, had a mean kinetic energy
of 60 meV; the other beam, a 5% mixture of O2
seeded in He, had a mean kinetic energy of 600
meV. Curve fits to time-of-flight data taken with the QMA are shown in
figure 1. The beam
flux for each condition was determined from time-of-flight data and from the pressure rise in the
third differential region of the beamline. Fluxes for the low and high energy
beams were adjusted to be equal simplifying
analysis of the comparative kinetics. Each beam was used to dose the nickel surface at two
different substrate temperatures, 300 K and 120 K.
Figure 2(a) shows typical HREEL spectra during dosing. The
growth of the Ni-O
stretch
signal at ~65 meV due to increased oxygen adsorption can be clearly seen. The inset in this figure
shows the shifts in the Ni-O peak position as a function of exposure. There shifts are indicative
of the different stages of oxygen overlayer formation. Figure 2(b)
was constructed by plotting
the ratio of the integrated intensity of the Ni-O peak to the integrated
specular peak,
versus oxygen exposure in units of Langmuirs (1 L = 10-6 torr sec).
The HREELS intensity ratio
is calibrated to monolayers of NiO using the known saturation limit of 3
ML at
room temperature. This calibration gives comparable results to the frequently used Auger
method of determining concentrations of surface oxygen. Different phases
of oxygen uptake are indicated in figure 2(b).
Figure 3 shows the oxygen uptake on Ni(111) versus exposure
to
both low and high
kinetic energy beams with the substrate at either 120 K or 300 K. For all four of these dosing
conditions, oxygen uptake has the same behavior below 25 L exposure: rapid chemisorption to
ca. 0.25 ML. Beyond 25 L, the behavior of the room and low temperature surfaces deviates
significantly. The low temperature substrate saturates at the chemisorption limit for both beam
conditions, a behavior seen previously under exposure to O2
from background dosing.
In contrast, the oxygen uptake on the room temperature surfaces continues beyond the
chemisorption limit for both beam energies. For both beam conditions, oxidation begins quickly
and then slows near the saturation limit of oxygen uptake. The shapes of the oxygen uptake
curves differ significantly for each dosing energy.
We first attempted to fit the oxidation data of figure 3 for
both
the high and low energy beams with the island growth model [P.H. Holloway and J.B.
Hudson, Surf. Sci. 43 (1974) 123 and 141], a model originally
developed to explain oxidation in the thermal regime using ambient gases. While the low energy beam data is
well reproduced by this model, it provides a poor description of the high energy beam data. The
inability to fit both data sets with the same kinetic model suggests that qualitatively different
mechanisms of oxide growth occur when using low and high energy incident fluxes of O
2. This has led us to develop a new model based on Langmuir kinetics.
For a detailed description of the island growth and Langmuir models please refer to
"Kinetic Energy Effects on the Oxidation of Ni(111) Using O2
Molecular Beams" B.D. Zion, A.T. Hanbicki and S.J. Sibener, Surface
Science Letters 417 L1154-L1159 (1998).
The functional difference for the rate of oxygen uptake between these two models
is that the island growth model is second order with respect to exposure whereas the Langmuir model is
first order. The simplicity in the difference between models belies the fundamental difference in their
derivations. Each model has been used to fit the 60 and 600 meV beam data
as shown in figure 4.
From a least squares analysis, and indeed as is evident upon inspection, it is determined that the
island growth model provides a clear fit to the data obtained with the lower energy beam. To
describe the high energy beam data it is necessary to invoke the Langmuir growth model which
more accurately follows the rapid rise at oxide onset and subsequent tail off in slope near 3 ML coverage.
One conclusion of this work in the comparison of the low energy beam
data and
previous work done with simple background dosing of the sample. The data for oxygen uptake
on the room temperature substrate under exposure to the low energy beam is best fit with the
same model originally derived to fit the background dosing data, implying no qualitative changes
in the kinetics of nickel oxidation. However, a significant difference in the value of the rate
constants for background and beam dosing suggests a quantitative difference in oxide
growth under beam exposure. A likely explanation for this difference is that the collimated beam
limits the angle of incidence whereas background dosing exposes the surface to molecules
from all possible angles, with commensurate differences in sticking.
The primary finding from this study is that the kinetics of oxidation actually change
functional form under exposure to high kinetic energy molecular beams. For low energy dosing,
oxidation is well described by the island growth model; however, the high kinetic energy data
cannot be fit with this model. In this regime the oxidation mechanism follows a kinetic scheme
better described by the proposed Langmuir model. In this picture, oxidation may occur
anywhere on the exposed surface, not just at island perimeters. This model may also be thought
of as oxide nucleation site formation occurring anywhere on the surface. For this model to be
true, we require that the rate at which oxygen is incorporated into the new nucleation sites be
much faster than the rate at which oxygen is incorporated into oxide islands. This interpretation
implies that there is an energy barrier to oxide nucleation that is overcome by the use of the high
energy incident molecules.
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