Materials Map

Discover the materials research landscape. Find experts, partners, networks.

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The Materials Map is an open tool for improving networking and interdisciplinary exchange within materials research. It enables cross-database search for cooperation and network partners and discovering of the research landscape.

The dashboard provides detailed information about the selected scientist, e.g. publications. The dashboard can be filtered and shows the relationship to co-authors in different diagrams. In addition, a link is provided to find contact information.

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The Materials Map is still under development. In its current state, it is only based on one single data source and, thus, incomplete and contains duplicates. We are working on incorporating new open data sources like ORCID to improve the quality and the timeliness of our data. We will update Materials Map as soon as possible and kindly ask for your patience.

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Topics

Publications (1/1 displayed)

  • 2008Wetting of mixed OH H2 O layers on Pt(111)41citations

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Darling, George R.
1 / 2 shared
Gallagher, Mark E.
1 / 1 shared
Zimbitas, Georgina
1 / 5 shared
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2008

Co-Authors (by relevance)

  • Darling, George R.
  • Gallagher, Mark E.
  • Zimbitas, Georgina
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article

Wetting of mixed OH H2 O layers on Pt(111)

  • Darling, George R.
  • Gallagher, Mark E.
  • Zimbitas, Georgina
  • Hodgson, Andrew
Abstract

<p>We describe the effect of growth temperature and OH H2 O composition on the wetting behavior of Pt(111). Changes to the desorption rate of ice films were measured and correlated to the film morphology using low energy electron diffraction and thermal desorption of chloroform to measure the area of multilayer ice and monolayer OH H2 O exposed. Thin ice films roughen, forming bare (39×39) R16° water monolayer and ice clusters. The size of the clusters depends on growth temperature and determines their kinetic stability, with the desorption rate decreasing when larger clusters are formed by growth at high temperature. Continuous films of more than approximately 50 layers thick stabilize an ordered incommensurate ice film that does not dewet. OH coadsorption pins the first layer into registry with Pt, forming an ordered hexagonal (OH+ H2 O) structure with all the H atoms involved in hydrogen bonding. Although this layer has a similar honeycomb O Hx skeleton to ice Ih, it is unable to reconstruct to match the bulk ice lattice parameter and does not form a stable wetting layer. Water aggregates to expose bare monolayer (OH+ H2 O), forming bulk ice crystallites whose size depend on preparation temperature. Increasing the proportion of water in the first layer provides free OH groups which stabilize the multilayer. The factors influencing multilayer wetting are discussed using density functional theory calculations to compare water adsorption on top of (OH+ H2 O) and on simple models for commensurate water structures. We show that both the (OH+ H2 O) structure and "H-down" water layers are poor proton acceptors, bonding to the first layer being enhanced by the presence of free OH groups. Formation of an ordered ice multilayer requires a water-metal interaction sufficient to wet the surface, but not so strong as to prevent the first layer relaxing to stabilize the interface between the metal and bulk ice.</p>

Topics
  • density
  • impedance spectroscopy
  • surface
  • cluster
  • theory
  • Hydrogen
  • density functional theory
  • forming
  • low energy electron diffraction