The surface stress, which characterizes the state of stress at the surface of a macroscopic crystal, is calculated from first principles by two methods for Mo(001) to be 3.1 mRyd bohr -2 = 2.4 J m -2 . Both methods use the energy of a fully relaxed seven-layer slab as a function of the in-plane lattice parameter a . One method uses the slope and the other the curvature at particular values of a . Fully relaxed energies give surface stress values 40% smaller than partially relaxed energies which have relaxed just a single common layer spacing. The slab is divided into bulk and surface regions with different parameters. Estimates are made of the surface region parameters including its equilibrium in-plane lattice constant, its epitaxial elastic constant, its Poisson ratio for in-plane strains and its thickness.
%0 Journal Article
%1 Marcus2000
%A Marcus, P M
%A Qian, Xianghong
%A Hübner, Wolfgang
%D 2000
%J Journal of Physics: Condensed Matter
%K DFT surface_stress
%N 26
%P 5541
%T Surface stress and relaxation in metals
%U http://stacks.iop.org/0953-8984/12/i=26/a=302
%V 12
%X The surface stress, which characterizes the state of stress at the surface of a macroscopic crystal, is calculated from first principles by two methods for Mo(001) to be 3.1 mRyd bohr -2 = 2.4 J m -2 . Both methods use the energy of a fully relaxed seven-layer slab as a function of the in-plane lattice parameter a . One method uses the slope and the other the curvature at particular values of a . Fully relaxed energies give surface stress values 40% smaller than partially relaxed energies which have relaxed just a single common layer spacing. The slab is divided into bulk and surface regions with different parameters. Estimates are made of the surface region parameters including its equilibrium in-plane lattice constant, its epitaxial elastic constant, its Poisson ratio for in-plane strains and its thickness.
@article{Marcus2000,
abstract = {The surface stress, which characterizes the state of stress at the surface of a macroscopic crystal, is calculated from first principles by two methods for Mo(001) to be 3.1 mRyd bohr -2 = 2.4 J m -2 . Both methods use the energy of a fully relaxed seven-layer slab as a function of the in-plane lattice parameter a . One method uses the slope and the other the curvature at particular values of a . Fully relaxed energies give surface stress values 40% smaller than partially relaxed energies which have relaxed just a single common layer spacing. The slab is divided into bulk and surface regions with different parameters. Estimates are made of the surface region parameters including its equilibrium in-plane lattice constant, its epitaxial elastic constant, its Poisson ratio for in-plane strains and its thickness.},
added-at = {2012-03-23T14:41:16.000+0100},
author = {Marcus, P M and Qian, Xianghong and H\"ubner, Wolfgang},
biburl = {https://www.bibsonomy.org/bibtex/2fc3f2ab89a15da34d8ebae0f7e608248/pmd},
description = {Surface stress and relaxation in metals},
interhash = {79c70db0cbeba6150482cdeb20e1c357},
intrahash = {fc3f2ab89a15da34d8ebae0f7e608248},
journal = {Journal of Physics: Condensed Matter},
keywords = {DFT surface_stress},
number = 26,
pages = 5541,
timestamp = {2012-03-23T14:41:16.000+0100},
title = {Surface stress and relaxation in metals},
url = {http://stacks.iop.org/0953-8984/12/i=26/a=302},
volume = 12,
year = 2000
}