Internal magnetic field gradients in paramagnetic shale pores
- Autores
- Ramia, Máximo Elías; Martín, Carlos Alberto
- Año de publicación
- 2017
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Fil: Ramia, Máximo Elías. Universidad Nacional de Córdoba. Facultad de Matemática, Astronomía, Física y Computación; Argentina.
Fil: Martín, Carlos Alberto. Universidad Nacional de Córdoba. Facultad de Matemática, Astronomía, Física y Computación; Argentina.
The present work involves a comprehensive study to provide a theoretical model of the internal magnetic field gradients, present in paramagnetic shale pores, to explain the main relaxation features observed by nuclear magnetic resonance transversal relaxation measurements. In the systematic analysis process of relaxation data it is necessary to know up to what extent the magnetic field gradients are generated by the logging tool and/or arise internally in the rock due to their paramagnetic impurities content. The physical model to explain the relaxation features is based on the calculation of field gradients in a planar pore with and without relaxatives walls. The results reproduce the features of the relaxation parameters in pores due to paramagnetic and tortuous walls. The mechanism that drives the relaxation process is governed by anomalous diffusion within micro-pores. These relaxation processes arise from the interactions between the protons, belonging to the liquid molecules and the pore walls, whose structure is characterized by both large tortuosity and abundance of paramagnetic impurities, giving rise to local strong time dependent magnetic field gradients. The theoretical results are compared with those obtained experimentally to validate the relaxation model. The experimental data were gathered from a sample belonging to the “Vaca Muerta” formation of the Neuquén basin, Argentina.
info:eu-repo/semantics/publishedVersion
Fil: Ramia, Máximo Elías. Universidad Nacional de Córdoba. Facultad de Matemática, Astronomía, Física y Computación; Argentina.
Fil: Martín, Carlos Alberto. Universidad Nacional de Córdoba. Facultad de Matemática, Astronomía, Física y Computación; Argentina.
Física de los Materiales Condensados - Materia
-
Nuclear magnetic resonance
Petrophysics
Shales - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- Repositorio
.jpg)
- Institución
- Universidad Nacional de Córdoba
- OAI Identificador
- oai:rdu.unc.edu.ar:11086/562617
Ver los metadatos del registro completo
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Internal magnetic field gradients in paramagnetic shale poresRamia, Máximo ElíasMartín, Carlos AlbertoNuclear magnetic resonancePetrophysicsShalesFil: Ramia, Máximo Elías. Universidad Nacional de Córdoba. Facultad de Matemática, Astronomía, Física y Computación; Argentina.Fil: Martín, Carlos Alberto. Universidad Nacional de Córdoba. Facultad de Matemática, Astronomía, Física y Computación; Argentina.The present work involves a comprehensive study to provide a theoretical model of the internal magnetic field gradients, present in paramagnetic shale pores, to explain the main relaxation features observed by nuclear magnetic resonance transversal relaxation measurements. In the systematic analysis process of relaxation data it is necessary to know up to what extent the magnetic field gradients are generated by the logging tool and/or arise internally in the rock due to their paramagnetic impurities content. The physical model to explain the relaxation features is based on the calculation of field gradients in a planar pore with and without relaxatives walls. The results reproduce the features of the relaxation parameters in pores due to paramagnetic and tortuous walls. The mechanism that drives the relaxation process is governed by anomalous diffusion within micro-pores. These relaxation processes arise from the interactions between the protons, belonging to the liquid molecules and the pore walls, whose structure is characterized by both large tortuosity and abundance of paramagnetic impurities, giving rise to local strong time dependent magnetic field gradients. The theoretical results are compared with those obtained experimentally to validate the relaxation model. The experimental data were gathered from a sample belonging to the “Vaca Muerta” formation of the Neuquén basin, Argentina.info:eu-repo/semantics/publishedVersionFil: Ramia, Máximo Elías. Universidad Nacional de Córdoba. Facultad de Matemática, Astronomía, Física y Computación; Argentina.Fil: Martín, Carlos Alberto. Universidad Nacional de Córdoba. Facultad de Matemática, Astronomía, Física y Computación; Argentina.Física de los Materiales Condensados2017info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfRamia, M. E. y Martín, C. A. (2017). Internal magnetic field gradients in paramagnetic shale pores. Applied Magnetic Resonance, 48 (10), 1075–1091. https://doi.org/10.1007/s00723-017-0922-90937-9347http://hdl.handle.net/11086/5626171613-7507https://doi.org/10.1007/s00723-017-0922-9enginfo:eu-repo/semantics/openAccessreponame:Repositorio Digital Universitario (UNC)instname:Universidad Nacional de Córdobainstacron:UNC2026-10-01T10:22:08Zoai:rdu.unc.edu.ar:11086/562617Institucionalhttps://rdu.unc.edu.ar/Universidad públicaNo correspondehttp://rdu.unc.edu.ar/oai/snrdoca.unc@gmail.comArgentinaNo correspondeNo correspondeNo correspondeopendoar:25722026-10-01 10:22:09.948Repositorio Digital Universitario (UNC) - Universidad Nacional de Córdobafalse |
| dc.title.none.fl_str_mv |
Internal magnetic field gradients in paramagnetic shale pores |
| title |
Internal magnetic field gradients in paramagnetic shale pores |
| spellingShingle |
Internal magnetic field gradients in paramagnetic shale pores Ramia, Máximo Elías Nuclear magnetic resonance Petrophysics Shales |
| title_short |
Internal magnetic field gradients in paramagnetic shale pores |
| title_full |
Internal magnetic field gradients in paramagnetic shale pores |
| title_fullStr |
Internal magnetic field gradients in paramagnetic shale pores |
| title_full_unstemmed |
Internal magnetic field gradients in paramagnetic shale pores |
| title_sort |
Internal magnetic field gradients in paramagnetic shale pores |
| dc.creator.none.fl_str_mv |
Ramia, Máximo Elías Martín, Carlos Alberto |
| author |
Ramia, Máximo Elías |
| author_facet |
Ramia, Máximo Elías Martín, Carlos Alberto |
| author_role |
author |
| author2 |
Martín, Carlos Alberto |
| author2_role |
author |
| dc.subject.none.fl_str_mv |
Nuclear magnetic resonance Petrophysics Shales |
| topic |
Nuclear magnetic resonance Petrophysics Shales |
| dc.description.none.fl_txt_mv |
Fil: Ramia, Máximo Elías. Universidad Nacional de Córdoba. Facultad de Matemática, Astronomía, Física y Computación; Argentina. Fil: Martín, Carlos Alberto. Universidad Nacional de Córdoba. Facultad de Matemática, Astronomía, Física y Computación; Argentina. The present work involves a comprehensive study to provide a theoretical model of the internal magnetic field gradients, present in paramagnetic shale pores, to explain the main relaxation features observed by nuclear magnetic resonance transversal relaxation measurements. In the systematic analysis process of relaxation data it is necessary to know up to what extent the magnetic field gradients are generated by the logging tool and/or arise internally in the rock due to their paramagnetic impurities content. The physical model to explain the relaxation features is based on the calculation of field gradients in a planar pore with and without relaxatives walls. The results reproduce the features of the relaxation parameters in pores due to paramagnetic and tortuous walls. The mechanism that drives the relaxation process is governed by anomalous diffusion within micro-pores. These relaxation processes arise from the interactions between the protons, belonging to the liquid molecules and the pore walls, whose structure is characterized by both large tortuosity and abundance of paramagnetic impurities, giving rise to local strong time dependent magnetic field gradients. The theoretical results are compared with those obtained experimentally to validate the relaxation model. The experimental data were gathered from a sample belonging to the “Vaca Muerta” formation of the Neuquén basin, Argentina. info:eu-repo/semantics/publishedVersion Fil: Ramia, Máximo Elías. Universidad Nacional de Córdoba. Facultad de Matemática, Astronomía, Física y Computación; Argentina. Fil: Martín, Carlos Alberto. Universidad Nacional de Córdoba. Facultad de Matemática, Astronomía, Física y Computación; Argentina. Física de los Materiales Condensados |
| description |
Fil: Ramia, Máximo Elías. Universidad Nacional de Córdoba. Facultad de Matemática, Astronomía, Física y Computación; Argentina. |
| publishDate |
2017 |
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2017 |
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info:eu-repo/semantics/publishedVersion info:eu-repo/semantics/article http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
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publishedVersion |
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article |
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Ramia, M. E. y Martín, C. A. (2017). Internal magnetic field gradients in paramagnetic shale pores. Applied Magnetic Resonance, 48 (10), 1075–1091. https://doi.org/10.1007/s00723-017-0922-9 0937-9347 http://hdl.handle.net/11086/562617 1613-7507 https://doi.org/10.1007/s00723-017-0922-9 |
| identifier_str_mv |
Ramia, M. E. y Martín, C. A. (2017). Internal magnetic field gradients in paramagnetic shale pores. Applied Magnetic Resonance, 48 (10), 1075–1091. https://doi.org/10.1007/s00723-017-0922-9 0937-9347 1613-7507 |
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http://hdl.handle.net/11086/562617 https://doi.org/10.1007/s00723-017-0922-9 |
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eng |
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eng |
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