Micromagnetic Determination of the FORC Response of Paleomagnetically Significant Magnetite Assemblages

Autores
Nagy, Lesleis; Moreno, Roberto; Muxworthy, Adrian R.; Williams, Wyn; Paterson, Greig A.; Tauxe, Lisa; Valdez‐Grijalva, Miguel A.
Año de publicación
2024
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Fil: Nagy, Lesleis. University of Liverpool. Department of Earth, Ocean and Ecological Sciences; United Kingdom.
Fil: Moreno, Roberto. University of Edinburgh. School of GeoSciences; United Kingdom.
Fil: Moreno, Roberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Física Enrique Gaviola; Argentina.
Fil: Muxworthy, Adrian R. Imperial College London. Department of Earth Science and Engineering; United Kingdom.
Fil: Muxworthy, Adrian R. University College London. Department of Earth Sciences; United Kingdom.
Fil: Williams, Wyn. University of Edinburgh. School of GeoSciences; United Kingdom.
Fil: Paterson, Greig A. University of Liverpool. Department of Earth, Ocean and Ecological Sciences; United Kingdom.
Fil: Tauxe, Lisa. University of California San Diego. Scripps Institution of Oceanography; United States of America.
Fil: Valdez‐Grijalva, Miguel A. Instituto Mexicano del Petróleo; México.
Micromagnetic modeling allows the systematic study of the effects of particle size and shape onthe first‐order reversal curve (FORC) magnetic hysteresis response for magnetite particles in the single‐domain(SD) and pseudo‐single domain (PSD) particle size range. The interpretation of FORCs, though widely used,has been highly subjective. Here, we use micromagnetics to model randomly oriented distributions of particlesto allow more physically meaningful interpretations. We show that one commonly found type of PSD particle—namely the single vortex (SV) particle—has far more complex signals than SD particles, with multiple peaksand troughs in the FORC distribution, where the peaks have higher switching fields for larger SV particles.Particles in the SD to SV transition zone have the lowest switching fields. Symmetrical and prolate particlesdisplay similar behavior, with distinctive peaks forming near the vertical axis of the FORC diagram. In contrast,highly oblate particles produce “butterfly” structures, suggesting that these are potentially diagnostic of particlemorphology. We also consider FORC diagrams for distributions of particle sizes and shapes and produce anonline application that users can use to build their own FORC distributions. There is good agreement betweenthe model predictions for distributions of particle sizes and shapes, and the published experimental literature.
info:eu-repo/semantics/publishedVersion
Fil: Nagy, Lesleis. University of Liverpool. Department of Earth, Ocean and Ecological Sciences; United Kingdom.
Fil: Moreno, Roberto. University of Edinburgh. School of GeoSciences; United Kingdom.
Fil: Moreno, Roberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Física Enrique Gaviola; Argentina.
Fil: Muxworthy, Adrian R. Imperial College London. Department of Earth Science and Engineering; United Kingdom.
Fil: Muxworthy, Adrian R. University College London. Department of Earth Sciences; United Kingdom.
Fil: Williams, Wyn. University of Edinburgh. School of GeoSciences; United Kingdom.
Fil: Paterson, Greig A. University of Liverpool. Department of Earth, Ocean and Ecological Sciences; United Kingdom.
Fil: Tauxe, Lisa. University of California San Diego. Scripps Institution of Oceanography; United States of America.
Fil: Valdez‐Grijalva, Miguel A. Instituto Mexicano del Petróleo; México.
Materia
First‐order reversalcurve
Magnetite
Single‐vortex particles
FORC
Nivel de accesibilidad
acceso abierto
Condiciones de uso
Repositorio
Repositorio Digital Universitario (UNC)
Institución
Universidad Nacional de Córdoba
OAI Identificador
oai:rdu.unc.edu.ar:11086/554095
Acceder
id RDUUNC_d3539925a9a30a2140267a3baccfd906
oai_identifier_str oai:rdu.unc.edu.ar:11086/554095
network_acronym_str RDUUNC
repository_id_str 2572
network_name_str Repositorio Digital Universitario (UNC)
spelling Micromagnetic Determination of the FORC Response of Paleomagnetically Significant Magnetite AssemblagesNagy, LesleisMoreno, RobertoMuxworthy, Adrian R.Williams, WynPaterson, Greig A.Tauxe, LisaValdez‐Grijalva, Miguel A.First‐order reversalcurveMagnetiteSingle‐vortex particlesFORCFil: Nagy, Lesleis. University of Liverpool. Department of Earth, Ocean and Ecological Sciences; United Kingdom.Fil: Moreno, Roberto. University of Edinburgh. School of GeoSciences; United Kingdom.Fil: Moreno, Roberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Física Enrique Gaviola; Argentina.Fil: Muxworthy, Adrian R. Imperial College London. Department of Earth Science and Engineering; United Kingdom.Fil: Muxworthy, Adrian R. University College London. Department of Earth Sciences; United Kingdom.Fil: Williams, Wyn. University of Edinburgh. School of GeoSciences; United Kingdom.Fil: Paterson, Greig A. University of Liverpool. Department of Earth, Ocean and Ecological Sciences; United Kingdom.Fil: Tauxe, Lisa. University of California San Diego. Scripps Institution of Oceanography; United States of America.Fil: Valdez‐Grijalva, Miguel A. Instituto Mexicano del Petróleo; México.Micromagnetic modeling allows the systematic study of the effects of particle size and shape onthe first‐order reversal curve (FORC) magnetic hysteresis response for magnetite particles in the single‐domain(SD) and pseudo‐single domain (PSD) particle size range. The interpretation of FORCs, though widely used,has been highly subjective. Here, we use micromagnetics to model randomly oriented distributions of particlesto allow more physically meaningful interpretations. We show that one commonly found type of PSD particle—namely the single vortex (SV) particle—has far more complex signals than SD particles, with multiple peaksand troughs in the FORC distribution, where the peaks have higher switching fields for larger SV particles.Particles in the SD to SV transition zone have the lowest switching fields. Symmetrical and prolate particlesdisplay similar behavior, with distinctive peaks forming near the vertical axis of the FORC diagram. In contrast,highly oblate particles produce “butterfly” structures, suggesting that these are potentially diagnostic of particlemorphology. We also consider FORC diagrams for distributions of particle sizes and shapes and produce anonline application that users can use to build their own FORC distributions. There is good agreement betweenthe model predictions for distributions of particle sizes and shapes, and the published experimental literature.info:eu-repo/semantics/publishedVersionFil: Nagy, Lesleis. University of Liverpool. Department of Earth, Ocean and Ecological Sciences; United Kingdom.Fil: Moreno, Roberto. University of Edinburgh. School of GeoSciences; United Kingdom.Fil: Moreno, Roberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Física Enrique Gaviola; Argentina.Fil: Muxworthy, Adrian R. Imperial College London. Department of Earth Science and Engineering; United Kingdom.Fil: Muxworthy, Adrian R. University College London. Department of Earth Sciences; United Kingdom.Fil: Williams, Wyn. University of Edinburgh. School of GeoSciences; United Kingdom.Fil: Paterson, Greig A. University of Liverpool. Department of Earth, Ocean and Ecological Sciences; United Kingdom.Fil: Tauxe, Lisa. University of California San Diego. Scripps Institution of Oceanography; United States of America.Fil: Valdez‐Grijalva, Miguel A. Instituto Mexicano del Petróleo; México.orcid.org/0000-0002-5104-7680orcid.org/0000-0002-9799-4210orcid.org/0000-0002-3070-4477orcid.org/0000-0001-9210-7574orcid.org/0000-0002-6864-7420orcid.org/0000-0002-4837-82002024-07-25info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfNagy, L., Moreno, R., Muxworthy, A. R., Williams, W., Paterson, G. A., Tauxe, L., & Valdez-Grijalva, M. A. (2024). Micromagnetic determination of the FORC response of paleomagnetically significant magnetite assemblages. Geochemistry, Geophysics, Geosystems, 25, e2024GC011465. https://doi.org/10.1029/2024GC01146515252027http://hdl.handle.net/11086/554095https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2024GC011465https://doi.org/10.1029/2024GC011465enginfo:eu-repo/semantics/openAccessreponame:Repositorio Digital Universitario (UNC)instname:Universidad Nacional de Córdobainstacron:UNC2025-09-29T13:44:38Zoai:rdu.unc.edu.ar:11086/554095Institucionalhttps://rdu.unc.edu.ar/Universidad públicaNo correspondehttp://rdu.unc.edu.ar/oai/snrdoca.unc@gmail.comArgentinaNo correspondeNo correspondeNo correspondeopendoar:25722025-09-29 13:44:38.346Repositorio Digital Universitario (UNC) - Universidad Nacional de Córdobafalse
dc.title.none.fl_str_mv Micromagnetic Determination of the FORC Response of Paleomagnetically Significant Magnetite Assemblages
title Micromagnetic Determination of the FORC Response of Paleomagnetically Significant Magnetite Assemblages
spellingShingle Micromagnetic Determination of the FORC Response of Paleomagnetically Significant Magnetite Assemblages
Nagy, Lesleis
First‐order reversalcurve
Magnetite
Single‐vortex particles
FORC
title_short Micromagnetic Determination of the FORC Response of Paleomagnetically Significant Magnetite Assemblages
title_full Micromagnetic Determination of the FORC Response of Paleomagnetically Significant Magnetite Assemblages
title_fullStr Micromagnetic Determination of the FORC Response of Paleomagnetically Significant Magnetite Assemblages
title_full_unstemmed Micromagnetic Determination of the FORC Response of Paleomagnetically Significant Magnetite Assemblages
title_sort Micromagnetic Determination of the FORC Response of Paleomagnetically Significant Magnetite Assemblages
dc.creator.none.fl_str_mv Nagy, Lesleis
Moreno, Roberto
Muxworthy, Adrian R.
Williams, Wyn
Paterson, Greig A.
Tauxe, Lisa
Valdez‐Grijalva, Miguel A.
author Nagy, Lesleis
author_facet Nagy, Lesleis
Moreno, Roberto
Muxworthy, Adrian R.
Williams, Wyn
Paterson, Greig A.
Tauxe, Lisa
Valdez‐Grijalva, Miguel A.
author_role author
author2 Moreno, Roberto
Muxworthy, Adrian R.
Williams, Wyn
Paterson, Greig A.
Tauxe, Lisa
Valdez‐Grijalva, Miguel A.
author2_role author
author
author
author
author
author
dc.contributor.none.fl_str_mv orcid.org/0000-0002-5104-7680
orcid.org/0000-0002-9799-4210
orcid.org/0000-0002-3070-4477
orcid.org/0000-0001-9210-7574
orcid.org/0000-0002-6864-7420
orcid.org/0000-0002-4837-8200
dc.subject.none.fl_str_mv First‐order reversalcurve
Magnetite
Single‐vortex particles
FORC
topic First‐order reversalcurve
Magnetite
Single‐vortex particles
FORC
dc.description.none.fl_txt_mv Fil: Nagy, Lesleis. University of Liverpool. Department of Earth, Ocean and Ecological Sciences; United Kingdom.
Fil: Moreno, Roberto. University of Edinburgh. School of GeoSciences; United Kingdom.
Fil: Moreno, Roberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Física Enrique Gaviola; Argentina.
Fil: Muxworthy, Adrian R. Imperial College London. Department of Earth Science and Engineering; United Kingdom.
Fil: Muxworthy, Adrian R. University College London. Department of Earth Sciences; United Kingdom.
Fil: Williams, Wyn. University of Edinburgh. School of GeoSciences; United Kingdom.
Fil: Paterson, Greig A. University of Liverpool. Department of Earth, Ocean and Ecological Sciences; United Kingdom.
Fil: Tauxe, Lisa. University of California San Diego. Scripps Institution of Oceanography; United States of America.
Fil: Valdez‐Grijalva, Miguel A. Instituto Mexicano del Petróleo; México.
Micromagnetic modeling allows the systematic study of the effects of particle size and shape onthe first‐order reversal curve (FORC) magnetic hysteresis response for magnetite particles in the single‐domain(SD) and pseudo‐single domain (PSD) particle size range. The interpretation of FORCs, though widely used,has been highly subjective. Here, we use micromagnetics to model randomly oriented distributions of particlesto allow more physically meaningful interpretations. We show that one commonly found type of PSD particle—namely the single vortex (SV) particle—has far more complex signals than SD particles, with multiple peaksand troughs in the FORC distribution, where the peaks have higher switching fields for larger SV particles.Particles in the SD to SV transition zone have the lowest switching fields. Symmetrical and prolate particlesdisplay similar behavior, with distinctive peaks forming near the vertical axis of the FORC diagram. In contrast,highly oblate particles produce “butterfly” structures, suggesting that these are potentially diagnostic of particlemorphology. We also consider FORC diagrams for distributions of particle sizes and shapes and produce anonline application that users can use to build their own FORC distributions. There is good agreement betweenthe model predictions for distributions of particle sizes and shapes, and the published experimental literature.
info:eu-repo/semantics/publishedVersion
Fil: Nagy, Lesleis. University of Liverpool. Department of Earth, Ocean and Ecological Sciences; United Kingdom.
Fil: Moreno, Roberto. University of Edinburgh. School of GeoSciences; United Kingdom.
Fil: Moreno, Roberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Instituto de Física Enrique Gaviola; Argentina.
Fil: Muxworthy, Adrian R. Imperial College London. Department of Earth Science and Engineering; United Kingdom.
Fil: Muxworthy, Adrian R. University College London. Department of Earth Sciences; United Kingdom.
Fil: Williams, Wyn. University of Edinburgh. School of GeoSciences; United Kingdom.
Fil: Paterson, Greig A. University of Liverpool. Department of Earth, Ocean and Ecological Sciences; United Kingdom.
Fil: Tauxe, Lisa. University of California San Diego. Scripps Institution of Oceanography; United States of America.
Fil: Valdez‐Grijalva, Miguel A. Instituto Mexicano del Petróleo; México.
description Fil: Nagy, Lesleis. University of Liverpool. Department of Earth, Ocean and Ecological Sciences; United Kingdom.
publishDate 2024
dc.date.none.fl_str_mv 2024-07-25
dc.type.none.fl_str_mv info:eu-repo/semantics/publishedVersion
info:eu-repo/semantics/article
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
status_str publishedVersion
format article
dc.identifier.none.fl_str_mv Nagy, L., Moreno, R., Muxworthy, A. R., Williams, W., Paterson, G. A., Tauxe, L., & Valdez-Grijalva, M. A. (2024). Micromagnetic determination of the FORC response of paleomagnetically significant magnetite assemblages. Geochemistry, Geophysics, Geosystems, 25, e2024GC011465. https://doi.org/10.1029/2024GC011465
15252027
http://hdl.handle.net/11086/554095
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2024GC011465
https://doi.org/10.1029/2024GC011465
identifier_str_mv Nagy, L., Moreno, R., Muxworthy, A. R., Williams, W., Paterson, G. A., Tauxe, L., & Valdez-Grijalva, M. A. (2024). Micromagnetic determination of the FORC response of paleomagnetically significant magnetite assemblages. Geochemistry, Geophysics, Geosystems, 25, e2024GC011465. https://doi.org/10.1029/2024GC011465
15252027
url http://hdl.handle.net/11086/554095
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2024GC011465
https://doi.org/10.1029/2024GC011465
dc.language.none.fl_str_mv eng
language eng
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.source.none.fl_str_mv reponame:Repositorio Digital Universitario (UNC)
instname:Universidad Nacional de Córdoba
instacron:UNC
reponame_str Repositorio Digital Universitario (UNC)
collection Repositorio Digital Universitario (UNC)
instname_str Universidad Nacional de Córdoba
instacron_str UNC
institution UNC
repository.name.fl_str_mv Repositorio Digital Universitario (UNC) - Universidad Nacional de Córdoba
repository.mail.fl_str_mv oca.unc@gmail.com
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score 13.070432

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