Orientation variation of surface strain

R. Harder, M. A. Pfeifer, G. J. Williams, I. A. Vartaniants, and I. K. Robinson
Phys. Rev. B 76, 115425 – Published 20 September 2007

Abstract

Expansion of the surface layers of a facetted hemispherical nanocrystal of Pb is reported at a temperature just below the melting point. Inversion of the coherent x-ray diffraction pattern yields quantitative three-dimensional maps of the deformation of the crystal from its equilibrium lattice spacing. Most of the surface of the crystal has a clear outward displacement, which decays exponentially into the bulk. This is suppressed on the (111) facet itself and is stronger on the spherical regions, suggesting that it arises from the orientational variation of the underlying surface stress.

  • Figure
  • Figure
  • Received 2 July 2007

DOI:https://doi.org/10.1103/PhysRevB.76.115425

©2007 American Physical Society

Authors & Affiliations

R. Harder1, M. A. Pfeifer2, G. J. Williams3, I. A. Vartaniants4, and I. K. Robinson1

  • 1London Center for Nanotechnology, Department of Physics and Astronomy, University College, London WC1E 6BT, United Kingdom
  • 2Department of Physics, La Trobe University, Victoria 3086, Australia
  • 3School of Physics, University of Melbourne, Victoria 3010, Australia
  • 4HASYLAB, DESY, Notkestrasse 85, D-22607 Hamburg, Germany

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Issue

Vol. 76, Iss. 11 — 15 September 2007

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