Abstract:A thermally induced change in the vibrational properties of a coadsorbed oxygen-water overlayer on Ru(OOl) is attributed to the formation of a local 0-H 2 0 complex. An O-H stretching mode of this complex is observed in electron-energy-loss data, but not in infrared reflection-absorption data available from another laboratory. This provides the first direct experimental evidence of a case in which the surface dipolar selection rule applies in an infrared but not in an energy-loss measurement.PACS numbers: 82.6… Show more
“…After desorption, the exact same amount of O at is present at the surface as before water was adsorbed. In agreement with earlier studies, [2][3][4]12 we find that about five water molecules are affected per oxygen atom.…”
Section: Discussionsupporting
confidence: 94%
“…5,8 In view of the debate over partial dissociation of water on Ru͕0001͖, it is imperative to reevaluate the assumptions made by previous authors who generally assumed that water stays intact when interacting with oxygen. [2][3][4] Only in a recent infrared spectroscopy study by Clay et al 12 was the possibility of water dissociation pointed out when coadsorbed with low coverages of oxygen. Using temperature-programed desorption ͑TPD͒, Doering and Madey found a significant change in the overall shape of the desorption spectra between low and high oxygen coverages with a sharp transition between 0.20 and 0.25 ML O, indicating a change in the interaction of H 2 O and O adatoms on the surface.…”
Section: Introductionmentioning
confidence: 97%
“…After more than 25 years of studying water adsorption on Ru͕0001͖, [1][2][3][4][5][6][7][8][9][10][11][12][13][14][15][16][17] there is still an ongoing debate about the exact nature of the system. Feibelman's recent suggestion that the most stable adsorption structure is in fact a partially dissociated hydrogen-bonded network of H 2 O and OH ͑Ref.…”
The coadsorption of water and preadsorbed oxygen on Ru͕0001͒ was studied by synchrotron-based highresolution x-ray photoelectron spectroscopy. A dramatic change was observed in the interaction of water with oxygen between low and high oxygen precoverages. Low oxygen coverages below 0.18 ML induce partial dissociation, which leads to an adsorbed layer of H 2 O and OH. Around half the oxygen atoms take part in this reaction. All OH recombines upon heating to 200 K and desorbs together with H 2 O. Oxygen coverages between 0.20 and 0.50 ML inhibit dissociation, instead a highly stable intact water species is observed, which desorbs at 220 K. This species is significantly more stable than intact water on the clean surface. The stabilization is most likely due to the formation of hydrogen bonds with neighboring oxygen atoms. For intermediate oxygen coverages around 0.18 ML, the dissociation behavior depends on the preparation conditions, which points toward possible mechanisms and pathways for partial dissociation of water on Ru͕0001͖.
“…After desorption, the exact same amount of O at is present at the surface as before water was adsorbed. In agreement with earlier studies, [2][3][4]12 we find that about five water molecules are affected per oxygen atom.…”
Section: Discussionsupporting
confidence: 94%
“…5,8 In view of the debate over partial dissociation of water on Ru͕0001͖, it is imperative to reevaluate the assumptions made by previous authors who generally assumed that water stays intact when interacting with oxygen. [2][3][4] Only in a recent infrared spectroscopy study by Clay et al 12 was the possibility of water dissociation pointed out when coadsorbed with low coverages of oxygen. Using temperature-programed desorption ͑TPD͒, Doering and Madey found a significant change in the overall shape of the desorption spectra between low and high oxygen coverages with a sharp transition between 0.20 and 0.25 ML O, indicating a change in the interaction of H 2 O and O adatoms on the surface.…”
Section: Introductionmentioning
confidence: 97%
“…After more than 25 years of studying water adsorption on Ru͕0001͖, [1][2][3][4][5][6][7][8][9][10][11][12][13][14][15][16][17] there is still an ongoing debate about the exact nature of the system. Feibelman's recent suggestion that the most stable adsorption structure is in fact a partially dissociated hydrogen-bonded network of H 2 O and OH ͑Ref.…”
The coadsorption of water and preadsorbed oxygen on Ru͕0001͒ was studied by synchrotron-based highresolution x-ray photoelectron spectroscopy. A dramatic change was observed in the interaction of water with oxygen between low and high oxygen precoverages. Low oxygen coverages below 0.18 ML induce partial dissociation, which leads to an adsorbed layer of H 2 O and OH. Around half the oxygen atoms take part in this reaction. All OH recombines upon heating to 200 K and desorbs together with H 2 O. Oxygen coverages between 0.20 and 0.50 ML inhibit dissociation, instead a highly stable intact water species is observed, which desorbs at 220 K. This species is significantly more stable than intact water on the clean surface. The stabilization is most likely due to the formation of hydrogen bonds with neighboring oxygen atoms. For intermediate oxygen coverages around 0.18 ML, the dissociation behavior depends on the preparation conditions, which points toward possible mechanisms and pathways for partial dissociation of water on Ru͕0001͖.
“…Dissociation is observed at low oxygen coverage ͑ Ͻ 0.2 ML͒ while it is inhibited at larger O coverage ͑ = 0.25-0.5 ML͒ contrary to studies that assume that water remains intact when interacting with oxygen. [6][7][8][9] Preadsorbed oxygen on the ruthenium surface does not only influence the dissociation characteristics of water but also its structure. On the p͑2 ϫ 2͒ oxygen terminated surface, water adsorbs in a p͑2 ϫ 2͒ symmetry, 4,10 compared to a hexagonal arrangement ͑ͱ3 ϫ ͱ 3͒R30°observed on clean hexagonalclose-packed metal surfaces.…”
Low-temperature scanning tunneling microscopy and density-functional theory ͑DFT͒ were used to study the adsorption of water on a Ru͑0001͒ surface covered with half monolayer of oxygen. The oxygen atoms occupy hcp sites in an ordered structure with ͑2 ϫ 1͒ periodicity. DFT predicts that water is weakly bound to the unmodified surface, 86 meV compared to the ϳ200 meV water-water H bond. Instead, we found that water adsorption causes a shift of half of the oxygen atoms from hcp sites to fcc sites, creating a honeycomb structure where water molecules bind strongly to the exposed Ru atoms. The energy cost of reconstructing the oxygen overlayer, around 230 meV per displaced oxygen atom, is more than compensated by the larger adsorption energy of water on the newly exposed Ru atoms. Water forms hydrogen bonds with the fcc O atoms in a ͑4 ϫ 2͒ superstructure due to alternating orientations of the molecules. Heating to 185 K results in the complete desorption of the water layer, leaving behind the oxygen-honeycomb structure, which is metastable relative to the original ͑2 ϫ 1͒. This stable structure is not recovered until after heating to temperatures close to 260 K.
“…Very extensive and revealing studies of water interaction with the Ru(0001) surface were performed by Thiel et al [130,131] using a variety of techniques (TDS, AES, HREELS, UPS, and ESDIAD = electron-stimulated desorption ion angular distribution). The authors observed several binding states in their TD spectra which develop simultaneously with H 2 O exposure, again indicating that a first and a second water layer grow at the same time, whereby the second layer is H-bonded to the first layer.…”
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.