I. Rze ꢀz nicka, T. Matsushima / Chemical Physics Letters 377 (2003) 279–285
285
desorption components,a fast one and a slow one.
The former showed high translational energy and
was suppressed above the KT. This component
for her 2000–2004 scholarship. This work was
supported in part by Grant-in-Aid No. 13640493
for General Scientific Research from the Japan
Society for the Promotion of Science.
10
2
showed a cos h form. CO desorption collimated
sharply along the surface normal,similarly to that
in Ôactive AÕ on Rh(1 1 0). No Ôactive BÕ was ob-
served in the steady-state conditions on Pd(1 1 0).
LEED observations were consistent with the
absence of bi-directional desorption. We monitored
the LEED intensity on Pd(1 1 0) around the KT,as
shown in Fig. 5. The LEED pattern changed from
c(2 ꢁ 4)-O [12] into the (1 ꢁ 1) without passing the
meta-stable (1 ꢁ 2) below the KT and showed the
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(
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5
hancement of the meta-stable (1 ꢁ 2) was found
below the KT. Similar changes were observed in the
temperature range of 360–460 K. This is consistent
with the meta-stable (1 ꢁ 2),which can be prepared
by oxygen removal with hydrogen and is converted
into the (1 ꢁ 1) above 355 K [13].
[
[
(
[
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3
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On Rh(1 1 0),declining facets with a (1 1 1)
structure on reconstructed (1 ꢁ 2) were confirmed
[
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to be active for a CO formation process by means
2
[
[
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[
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Rosei,Surf. Sci. 260 (1992) L24.
state CO oxidation. CO desorption is split into bi-
2
directional lobes collimated at ꢀ24° off normal and
the meta-stable (1 ꢁ 2) structure stabilized by oxy-
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2
gen provides declining CO formation sites. On the
[
other hand,on Pd(1 1 0),no meta-stable (1 ꢁ 2)
structure is observed below the kinetic transition
and the reconstructed (1 ꢁ 2) stabilized by oxygen is
converted directly into the (1 ꢁ 1) form.
1
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(1977) 89.
[
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(
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Acknowledgements
[
Rze ꢀz nicka Izabela is indebted to the Ministry of
Education,Science,Sports and Culture of Japan