dor_id: 4133312

506.#.#.a: Público

590.#.#.d: Los artículos enviados a la revista "Geofísica Internacional", se juzgan por medio de un proceso de revisión por pares

510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT); Scientific Electronic Library Online (SciELO); SCOPUS, Dialnet, Directory of Open Access Journals (DOAJ); Geobase

561.#.#.u: https://www.geofisica.unam.mx/

650.#.4.x: Físico Matemáticas y Ciencias de la Tierra

336.#.#.b: article

336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

351.#.#.6: http://revistagi.geofisica.unam.mx/index.php/RGI

351.#.#.b: Geofísica Internacional

351.#.#.a: Artículos

harvesting_group: RevistasUNAM

270.1.#.p: Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

590.#.#.c: Open Journal Systems (OJS)

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883.#.#.1: https://www.publicaciones.unam.mx/

883.#.#.q: Dirección General de Publicaciones y Fomento Editorial

850.#.#.a: Universidad Nacional Autónoma de México

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/329/314

100.1.#.a: Rico, Y.; Bidegain, J. C.; Elsner, C. I.

524.#.#.a: Rico, Y., et al. (2009). Synthetic and natural Iron oxide characterization through microparticle voltammetry. Geofísica Internacional; Vol. 48 Núm. 2: Abril 1, 2009; 221-236. Recuperado de https://repositorio.unam.mx/contenidos/4133312

245.1.0.a: Synthetic and natural Iron oxide characterization through microparticle voltammetry

502.#.#.c: Universidad Nacional Autónoma de México

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2009

264.#.1.c: 2009-04-01

653.#.#.a: Voltametría de micropartículas; potencial de pico de corriente; óxidos y oxihidróxidos de hierro; Microparticle voltammetry; current peak potential; Iron oxides and oxy–hydroxides

506.1.#.a: La titularidad de los derechos patrimoniales de esta obra pertenece a las instituciones editoras. Su uso se rige por una licencia Creative Commons BY-NC-SA 4.0 Internacional, https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/329

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041.#.7.h: spa

520.3.#.a: We are hereby presenting the results obtained from a study on using Microparticle Voltammetry (MPV) for identifying Iron oxides and oxy–hydroxides. This technique allowed us to distinguish different mineral species, such as hematite, goethite, magnetite and maghemite, in both synthetic and natural samples. By measuring synthetic pigments at different temperatures, evidence was found of an electrochemical behavioral pattern which allowed differenciating them. The current peak location (potential value) proved to vary according to the mineral species, grain size and chrystallinity degree. The area varies in terms of electroactive concentration of the species given. Width varies according to particle size distribution. In high iron oxide and oxy–hydroxide concentration samples, peaks were defined at current values of mA (milliampers) and in paleosol samples having an overall iron content lower than 6%, peaks were recorded at currents of µA (microampers). Therefore, a possibility arises of applying this technique to environmental and palaeo–environmental studies of these minerals.MPVs main advantages compared to conventional methods are speed and simplicity as well as the fact that it allows processing a few sample grains, in spite of its chrystallinity degree. Unlike magnetic methods – strongly influenced by the presence of magnetite– MPV is highly sensitive for detecting weakly magnetic species.doi: https://doi.org/10.22201/igeof.00167169p.2009.48.2.2140

773.1.#.t: Geofísica Internacional; Vol. 48 Núm. 2: Abril 1, 2009; 221-236

773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI

022.#.#.a: ISSN-L: 2954-436X; ISSN impreso: 0016-7169

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300.#.#.a: Páginas: 221-236

264.#.1.b: Instituto de Geofísica, UNAM

doi: https://doi.org/10.22201/igeof.00167169p.2009.48.2.2140

handle: 1e0c19d2872e1c7e

harvesting_date: 2023-06-20 16:00:00.0

856.#.0.q: application/pdf

file_creation_date: 2009-03-25 19:42:33.0

file_modification_date: 2022-05-30 14:42:41.0

file_creator: Rico Y.

file_name: 2cdf419d873aa83cebef76aa2a7dc344dd41385889f8481a57c2b954b929aaa0.pdf

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245.1.0.b: Synthetic and natural Iron oxide characterization through microparticle voltammetry

last_modified: 2023-06-20 16:00:00

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Artículo

Synthetic and natural Iron oxide characterization through microparticle voltammetry

Rico, Y.; Bidegain, J. C.; Elsner, C. I.

Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Geofísica, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Rico, Y., et al. (2009). Synthetic and natural Iron oxide characterization through microparticle voltammetry. Geofísica Internacional; Vol. 48 Núm. 2: Abril 1, 2009; 221-236. Recuperado de https://repositorio.unam.mx/contenidos/4133312

Descripción del recurso

Autor(es)
Rico, Y.; Bidegain, J. C.; Elsner, C. I.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Synthetic and natural Iron oxide characterization through microparticle voltammetry
Fecha
2009-04-01
Resumen
We are hereby presenting the results obtained from a study on using Microparticle Voltammetry (MPV) for identifying Iron oxides and oxy–hydroxides. This technique allowed us to distinguish different mineral species, such as hematite, goethite, magnetite and maghemite, in both synthetic and natural samples. By measuring synthetic pigments at different temperatures, evidence was found of an electrochemical behavioral pattern which allowed differenciating them. The current peak location (potential value) proved to vary according to the mineral species, grain size and chrystallinity degree. The area varies in terms of electroactive concentration of the species given. Width varies according to particle size distribution. In high iron oxide and oxy–hydroxide concentration samples, peaks were defined at current values of mA (milliampers) and in paleosol samples having an overall iron content lower than 6%, peaks were recorded at currents of µA (microampers). Therefore, a possibility arises of applying this technique to environmental and palaeo–environmental studies of these minerals.MPVs main advantages compared to conventional methods are speed and simplicity as well as the fact that it allows processing a few sample grains, in spite of its chrystallinity degree. Unlike magnetic methods – strongly influenced by the presence of magnetite– MPV is highly sensitive for detecting weakly magnetic species.doi: https://doi.org/10.22201/igeof.00167169p.2009.48.2.2140
Tema
Voltametría de micropartículas; potencial de pico de corriente; óxidos y oxihidróxidos de hierro; Microparticle voltammetry; current peak potential; Iron oxides and oxy–hydroxides
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces