Steffen Tober, Jan-Christian Schober, Marcus Creutzburg, Esko Erik Beck, Guilherme Dalla Lana Semione, Simon Chung, Leon Jacobse, Björn Arndt, Alina Vlad, René Steinbrügge, Hans-Christian Wille, Ilya Sergueev, Heshmat Noei, Kai Schlage, Olaf Leupold, Vedran Vonk, Andreas Stierle
{"title":"Site-Resolved Near-Surface Cation Diffusion in Magnetite","authors":"Steffen Tober, Jan-Christian Schober, Marcus Creutzburg, Esko Erik Beck, Guilherme Dalla Lana Semione, Simon Chung, Leon Jacobse, Björn Arndt, Alina Vlad, René Steinbrügge, Hans-Christian Wille, Ilya Sergueev, Heshmat Noei, Kai Schlage, Olaf Leupold, Vedran Vonk, Andreas Stierle","doi":"10.1103/physrevlett.134.236203","DOIUrl":null,"url":null,"abstract":"nuclear forward scattering shows a thermally induced cation exchange between a Fe</a:mi></a:mrow>57</a:mn></a:mrow></a:mmultiscripts></a:mrow>3</a:mn></a:mrow></a:msub>O</a:mi>4</a:mn></a:msub></a:math> thin-film and a <d:math xmlns:d=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><d:msub><d:mi>Fe</d:mi><d:mn>3</d:mn></d:msub><d:msub><d:mi mathvariant=\"normal\">O</d:mi><d:mn>4</d:mn></d:msub></d:math> (001) substrate predominantly in the octahedral sublattice for a temperature range between 470 and 710 K. The overall activation barrier in this temperature range is found to be <g:math xmlns:g=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><g:mrow><g:mn>19</g:mn><g:mo>±</g:mo><g:mn>32</g:mn><g:mtext> </g:mtext><g:mtext> </g:mtext><g:mi>kJ</g:mi><g:mo>/</g:mo><g:mi>mol</g:mi></g:mrow></g:math>, which is significantly lower than expected from extrapolating a bulk diffusion model. This observation can be attributed to the large out-of-equilibrium cation deficit as determined by surface x-ray diffraction. Despite the relatively low hopping barrier, the diffusion constant is about 5 orders of magnitude lower than expected for magnetite having an equilibrium cation stoichiometry. The results are relevant for applications relying on the near-surface structure and stoichiometry of magnetite, and we argue that the correlation between cation diffusion and stoichiometry may play a role for a wider range of oxide materials. <jats:supplementary-material> <jats:copyright-statement>Published by the American Physical Society</jats:copyright-statement> <jats:copyright-year>2025</jats:copyright-year> </jats:permissions> </jats:supplementary-material>","PeriodicalId":20069,"journal":{"name":"Physical review letters","volume":"8 1","pages":""},"PeriodicalIF":8.1000,"publicationDate":"2025-06-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physical review letters","FirstCategoryId":"101","ListUrlMain":"https://doi.org/10.1103/physrevlett.134.236203","RegionNum":1,"RegionCategory":"物理与天体物理","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"PHYSICS, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
nuclear forward scattering shows a thermally induced cation exchange between a Fe573O4 thin-film and a Fe3O4 (001) substrate predominantly in the octahedral sublattice for a temperature range between 470 and 710 K. The overall activation barrier in this temperature range is found to be 19±32kJ/mol, which is significantly lower than expected from extrapolating a bulk diffusion model. This observation can be attributed to the large out-of-equilibrium cation deficit as determined by surface x-ray diffraction. Despite the relatively low hopping barrier, the diffusion constant is about 5 orders of magnitude lower than expected for magnetite having an equilibrium cation stoichiometry. The results are relevant for applications relying on the near-surface structure and stoichiometry of magnetite, and we argue that the correlation between cation diffusion and stoichiometry may play a role for a wider range of oxide materials. Published by the American Physical Society2025
期刊介绍:
Physical review letters(PRL)covers the full range of applied, fundamental, and interdisciplinary physics research topics:
General physics, including statistical and quantum mechanics and quantum information
Gravitation, astrophysics, and cosmology
Elementary particles and fields
Nuclear physics
Atomic, molecular, and optical physics
Nonlinear dynamics, fluid dynamics, and classical optics
Plasma and beam physics
Condensed matter and materials physics
Polymers, soft matter, biological, climate and interdisciplinary physics, including networks