1993
DOI: 10.1007/bf00331749
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The formation of subsurface oxygen on Pt(100)

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Cited by 91 publications
(44 citation statements)
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“…We note that Rotermund et al [45] already suggested thermodynamically stable subsurface oxygen to explain a change in work function for Pt(100) when the oxygen-covered surface was heated from 360 to 600 K. Furthermore, they observed desorption of the subsurface oxygen at 760 K, which is lower but comparable to what we observe for Pt(111), and the reactivity of subsurface O towards CO oxidation similar to ours [46].…”
Section: Resultssupporting
confidence: 89%
“…We note that Rotermund et al [45] already suggested thermodynamically stable subsurface oxygen to explain a change in work function for Pt(100) when the oxygen-covered surface was heated from 360 to 600 K. Furthermore, they observed desorption of the subsurface oxygen at 760 K, which is lower but comparable to what we observe for Pt(111), and the reactivity of subsurface O towards CO oxidation similar to ours [46].…”
Section: Resultssupporting
confidence: 89%
“…Here y 1 is the critical concentration of CO at which an SRS starts, while y 2 is the critical concentration of CO where an SRS stops. Experiments show that the production of CO 2 starts as soon as y CO departs from zero [9][10][11]. Inspired by the work of Ziff et al [7], different authors have studied variants of the ZGB model [12][13][14][15][16][17][18][19][20][21][22][23][24][25][26][27] .…”
Section: Introductionmentioning
confidence: 99%
“…The studies of the reaction fronts formed during the chemical reaction on single crystal surface have been considered as a first step in the comprehension and in the formulation of realistic models [71,72]. As discussed below, an impressive variety of different chemical wave patterns has been found in recent years [73,74]. Moreover the temporal resolution of PEEM (few ms) is always sufficient for the observed dynamical process.…”
Section: The Spectromiscroscopymentioning
confidence: 99%