Complexions and stoichiometry of the ...
Document type :
Article dans une revue scientifique: Article original
DOI :
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Title :
Complexions and stoichiometry of the 60.8°//[100](011) symmetrical tilt grain boundary in Mg2SiO4 forsterite: a combined empirical potential and first-principles study
Author(s) :
Furstoss, Jean [Auteur]
Unité Matériaux et Transformations (UMET) - UMR 8207
Hirel, Pierre [Auteur]
Unité Matériaux et Transformations (UMET) - UMR 8207
Carrez, Philippe [Auteur]
Unité Matériaux et Transformations (UMET) - UMR 8207
Cordier, Patrick [Auteur]
Unité Matériaux et Transformations (UMET) - UMR 8207
Unité Matériaux et Transformations (UMET) - UMR 8207
Hirel, Pierre [Auteur]
Unité Matériaux et Transformations (UMET) - UMR 8207
Carrez, Philippe [Auteur]
Unité Matériaux et Transformations (UMET) - UMR 8207
Cordier, Patrick [Auteur]
Unité Matériaux et Transformations (UMET) - UMR 8207
Journal title :
American Mineralogist
Publication date :
2022-04-13
ISSN :
0003-004X
HAL domain(s) :
Physique [physics]/Matière Condensée [cond-mat]/Science des matériaux [cond-mat.mtrl-sci]
Planète et Univers [physics]/Sciences de la Terre
Planète et Univers [physics]/Sciences de la Terre
English abstract : [en]
In this work we explore the low energy complexions of the symmetrical tilt grain boundary (GB) 60.8°//[100](011) in forsterite through molecular dynamics and first principles calculations. Using conservative sampling, we ...
Show more >In this work we explore the low energy complexions of the symmetrical tilt grain boundary (GB) 60.8°//[100](011) in forsterite through molecular dynamics and first principles calculations. Using conservative sampling, we find six stoichiometric complexions with energies ranging from 0.66 to 1.25 J.m−2. We investigate the segregation of MgO vacancy pairs, and find that in most cases it is more favorable for vacancies to lie within the GBs than in the surrounding crystals, leading to new atomic structures. From these results we infer that at finite temperature when vacancies are present in the system, GBs are likely to absorb them and to be non-stoichiometric. We find many GB complexions containing a free oxygen ion, which may have profound implications for geological processes.Show less >
Show more >In this work we explore the low energy complexions of the symmetrical tilt grain boundary (GB) 60.8°//[100](011) in forsterite through molecular dynamics and first principles calculations. Using conservative sampling, we find six stoichiometric complexions with energies ranging from 0.66 to 1.25 J.m−2. We investigate the segregation of MgO vacancy pairs, and find that in most cases it is more favorable for vacancies to lie within the GBs than in the surrounding crystals, leading to new atomic structures. From these results we infer that at finite temperature when vacancies are present in the system, GBs are likely to absorb them and to be non-stoichiometric. We find many GB complexions containing a free oxygen ion, which may have profound implications for geological processes.Show less >
Language :
Anglais
Peer reviewed article :
Oui
Audience :
Internationale
Popular science :
Non
European Project :
Administrative institution(s) :
Université de Lille
CNRS
INRAE
ENSCL
CNRS
INRAE
ENSCL
Collections :
Research team(s) :
Plasticité
Submission date :
2022-05-09T16:08:40Z
2022-05-10T15:25:45Z
2022-11-07T15:04:53Z
2022-11-07T15:07:15Z
2022-05-10T15:25:45Z
2022-11-07T15:04:53Z
2022-11-07T15:07:15Z
Files
- Furstoss-et-al(2022)ComplexionsSTGB-Mg2SiO4-Forsterite.pdf
- Version éditeur
- Open access
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Annexes
- 8420HirelPreprint.pdf
- N/A
- Open access
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