Ferrodistortive instability at the (001) surface of half-metallic manganites

Physics – Condensed Matter – Materials Science

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

4 pages, 2 figures

Scientific paper

10.1103/PhysRevLett.99.226101

We present the structure of the fully relaxed (001) surface of the half-metallic manganite La0.7Sr0.3MnO3, calculated using density functional theory within the generalized gradient approximation (GGA). Two relevant ferroelastic order parameters are identified and characterized: The tilting of the oxygen octahedra, which is present in the bulk phase, oscillates and decreases towards the surface, and an additional ferrodistortive Mn off-centering, triggered by the surface, decays monotonically into the bulk. The narrow d-like energy band that is characteristic of unrelaxed manganite surfaces is shifted down in energy by these structural distortions, retaining its uppermost layer localization. The magnitude of the zero-temperature magnetization is unchanged from its bulk value, but the effective spin-spin interactions are reduced at the surface.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Ferrodistortive instability at the (001) surface of half-metallic manganites does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Ferrodistortive instability at the (001) surface of half-metallic manganites, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Ferrodistortive instability at the (001) surface of half-metallic manganites will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-675279

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.