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A model of the Ice-d-electron-metal interface

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Il Nuovo Cimento B (1971-1996)

Summary

A qualitative explanation of the different orientations of the growth of ice on Pt(111) and Ag(111) surfaces is proposed. Other physical consequences which follow are discussed and experiments are suggested to test these.

Riassunto

Il lavoro propone una spiegazione qualitativa delle diverse orientazioni di crescita del ghiaccio su superfici (111) di platino e argento. Conseguenze fisiche del modello e loro prove sperimentali sono discusse.

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Authors and Affiliations

  1. Theoretical Chemistry Department, University of Oxford, 1 South Parks Road, OX1 3TG, Oxford, England

    K. R. Painter, P. J. Grout & N. H. March

  2. International Centre for Theoretical Physics, Miramare (Trieste), Italy

    M. P. Tosi

Authors
  1. K. R. Painter
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  2. P. J. Grout
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  3. N. H. March
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  4. M. P. Tosi
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Painter, K.R., Grout, P.J., March, N.H. et al. A model of the Ice-d-electron-metal interface. Nuovo Cimento B 66, 202–206 (1981). https://doi.org/10.1007/BF02721187

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  • DOI: https://doi.org/10.1007/BF02721187

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