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Identification and quantification of iron oxides by diffuse reflectance spectroscopy with Praying Mantis accessory and integration sphere

dc.contributor.authorCanton, Leila Cristina
dc.contributor.authorSouza Júnior, Ivan Granemann de
dc.contributor.authorSilva, Laércio Santos [UNESP]
dc.contributor.authorMarques Júnior, José [UNESP]
dc.contributor.authorCosta, Antonio Carlos Saraiva da
dc.contributor.institutionUniversidade Estadual de Maringá (UEM)
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.date.accessioned2021-06-25T10:33:53Z
dc.date.available2021-06-25T10:33:53Z
dc.date.issued2021-01-01
dc.description.abstractSoil color is one of the main attributes used in the Brazilian System of Soil Classification and is related to the presence and concentration of iron oxides. This work aimed to identify and quantify the iron oxides (hematite, goethite and maghemite) present in soils and synthetic minerals and compare the diffuse reflectance spectroscopy (DRS) data equipped with the Integration Sphere (DRS-IS) or the Praying Mantis (DRS-PM) accessories with reference values obtained by XRD. Four samples of synthetic iron oxides (hematite, goethite, maghemite, magnetite) and two samples of aluminosilicates (kaolinite and smectite) were selected along with the A and Bw Horizons from 6 Oxisols of the State of Paraná-Brazil. The soils were characterized on their physical and mineralogical attributes and organic carbon content. All minerals, soil samples, soils clay fractions treated and not treated with the boiling 5 M NaOH procedure and with 1.8 M H2SO4 were analyzed using the integration sphere, the Praying Mantis accessory and color determined in the Munsell scale using a Minolta CR 400 spectroradiometer. The DRS-PM, by means of the second derivative of Kubelka-Munk function was very promising for identification and quantification of hematite for presenting results close to those obtained by XRD. Otherwise, the quantification of goethite was overestimated in both DRS's measurements due to the presence of organic matter. It was not possible to identify and quantify the presence of maghemite in soils and mixture minerals samples using both DRSs accessories due to the superposition of secondary bands of goethite, hematite, and the magnetite on the maghemite spectrum. The presence of maghemite in the soil material induces an overestimation of hematite content by DRS. The estimation of the Hm/(Hm + Gt) and Gt/(Gt + Hm) ratios by both accessories presented good correlation with data obtained by XRD.en
dc.description.affiliationDepartment of Agronomy State University of Maringá (UEM) Department of Agronomy, Avenida Colombo 5790, Maringá
dc.description.affiliationDepartment of Soils and Fertilizers Faculty of Agrarian and Veterinary Sciences São Paulo State University (FCAV/UNESP), Jaboticabal
dc.description.affiliationUnespDepartment of Soils and Fertilizers Faculty of Agrarian and Veterinary Sciences São Paulo State University (FCAV/UNESP), Jaboticabal
dc.description.sponsorshipCoordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
dc.description.sponsorshipConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.description.sponsorshipFundação Araucária
dc.identifierhttp://dx.doi.org/10.1016/j.catena.2020.104899
dc.identifier.citationCatena, v. 196.
dc.identifier.doi10.1016/j.catena.2020.104899
dc.identifier.issn0341-8162
dc.identifier.scopus2-s2.0-85091252630
dc.identifier.urihttp://hdl.handle.net/11449/206536
dc.language.isoeng
dc.relation.ispartofCatena
dc.sourceScopus
dc.subjectGoethite
dc.subjectHematite
dc.subjectMaghemite
dc.subjectSoil color
dc.subjectSoil mineralogy
dc.subjectX-rays diffraction
dc.titleIdentification and quantification of iron oxides by diffuse reflectance spectroscopy with Praying Mantis accessory and integration sphereen
dc.typeArtigo
dspace.entity.typePublication
unesp.departmentSolos e Adubos - FCAVpt

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