J. Michael Gottfried, K. Christmann / Surface Science 566–568 (2004) 1112–1117
1113
requires thorough quantitative kinetic measure-
ments [2]. While these are rare, there is also a lack
of UHV reference studies on gold single-crystal
surfaces. In one of the few previous investigations,
Outka and Madix [7] oxidized CO on an oxygen-
precovered Au(1 1 0) surface and evaluated an
apparent activation energy of (8 ± 4) kJ/mol for the
overall reaction. A true activation energy of the
surface reaction could not be determined because
the CO desorption energy remained unknown.
In one of our recent reports on oxygen
adsorption on Au(1 1 0)-(1 · 2) [8] we performed
reactive thermal desorption measurements of the
CO oxidation reaction and found a rate maximum
at 175 K. Above this temperature the rate has a
negative temperature coefficient. This result sug-
gests a negative apparent activation energy and is
thus at variance with the positive value reported by
Outka and Madix. To clarify this point we now
performed detailed kinetic measurements. The
data obtained in this and our recent publications
enable us to present a complete energy diagram of
the CO oxidation over Au(1 1 0).
Fig. 1. CO oxidation over O/Au(1 1 0)-(l · 2). CO
2
desorption
rate as a function of time for temperatures between 60 and 400
þ
K. Detected mass: m=z ¼ 44 (CO ). Inset: semi-logarithmic
2
plot.
2
. Experimental
all experiments the sample was heated to 450 K.
Thereafter, the sample temperature was set to a
constant value and the CO pressure was (almost)
A detailed description of our sample and its
ꢀ
6
preparation was given in Ref. [9], whereas the
experimental details of the kinetic measurements
can be found in Ref. [8].
instantaneously increased to 1 · 10 mbar. The
2
resulting CO desorption flux, which was mea-
sured with
a
mass spectrometer, decreases
The error of the pressure measurement amounts
to 20%. The different gauge sensitivities for the
particular gases were compensated by dividing the
approximately exponentially with time (Fig. 1).
First, we qualitatively consider the initial rates
(t ¼ 0): in the low-temperature range between 60
and 160 K, the initial rate increases with tempera-
ture due to the usual rise of the reaction rate con-
meter reading by the following factors: CO 1.1, O
0.8 (values recommended by the manufacturer of
the gauge).
2
stant k . Above 180 K, however, the rate decreases,
r
indicating a negative apparent activation energy.
The most likely reason is a decrease of the CO
equilibrium coverage with increasing temperature,
which is not compensated by the increase of kr.
Assuming a Langmuir–Hinshelwood mecha-
nism, which is strongly suggested by the behaviour
in the high-temperature range, we can derive a
mechanism that allows a quantitative analysis and
the determination of the true activation energy of
the surface reaction. The following mechanism is
proposed:
3
. Results and discussion
Fig. 1 displays the CO
2
desorption rate, RCO2 , as
a function of time for various fixed temperatures
between 60 and 400 K. In all measurements, the
following procedure was applied: chemisorbed
atomic oxygen (0.45 ML) was prepared by electron
bombardment of physisorbed O as described in
2
Refs. [9,10]. To ensure a uniform oxygen phase in