Synthesis and characterization of hematite particles (α-Fe2O3) obtained by thermal treatment of FeSO4 with sugar
Descripción del Articulo
Hematite particles were synthesized by thermal treatment of FeSO4 with different concentrations of sugar. The powder mix of FeSO4 and simple sugar was held at 600 °C for 14 h in a furnace. Using ratios of 1 g and 3 g of FeSO4, to 0.1 g, 0.2 g and 0.3 g of simple sugar respectively. The analysis of t...
Autores: | , , |
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Formato: | artículo |
Fecha de Publicación: | 2022 |
Institución: | Universidad Nacional Mayor de San Marcos |
Repositorio: | Revistas - Universidad Nacional Mayor de San Marcos |
Lenguaje: | inglés |
OAI Identifier: | oai:ojs.csi.unmsm:article/21240 |
Enlace del recurso: | https://revistasinvestigacion.unmsm.edu.pe/index.php/fisica/article/view/21240 |
Nivel de acceso: | acceso abierto |
Materia: | Método de reacción en estado sólido difracción de rayos X espectroscopia Mössbauer por transmisión magnetometría solid-state reaction method X ray diffractometry transmission Mössbauer spectroscopy magnetometry |
Sumario: | Hematite particles were synthesized by thermal treatment of FeSO4 with different concentrations of sugar. The powder mix of FeSO4 and simple sugar was held at 600 °C for 14 h in a furnace. Using ratios of 1 g and 3 g of FeSO4, to 0.1 g, 0.2 g and 0.3 g of simple sugar respectively. The analysis of the macroscopic magnetic properties of the samples was made with an alternating field magnetometer. For the structural characterization of the samples, X-ray diffractometry (XRD) and transmission Mössbauer spectroscopy (TMS) were used. Depending on the concentrations of sugar used, the presence of hematite or butlerite was observed by XRD. The sole presence of the hematite phase was observed when the ratios of 1 g of FeSO4 to 0.1 g, 0.2 g and 0.3 g of sugar were used. The hematite phase was not observed for the ratios of 3 g FeSO4 to 0.1 g, 0.2 g and 0.3 g of sugar; in these cases the crystalline phase of butlerita (Fe(SO4)(OH)(H2O)2) was obtained. Through the Mössbauer hyperfine parameters measured by TMS, the mineralogical phase was determined by the presence of the magnetic sextet of hematite for the mixtures with 1 g of FeSO4; and in the cases of 3 g FeSO4 by the presence of two paramagnetic doublets assigned to iron cations having 3+ oxidation state. These results allowed us to correlate them with those obtained by XRD. |
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La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).
La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).