Mineralogical Appraisal of Bauxite Overburdens from Brazil

Mineralogical appraisal is an important tool for both mining and industrial processes. X-ray powder diffraction analysis (XRPD) can deliver fast and reliable mineralogical quantification results to aid industrial processes and improve ore recoveries. Furthermore, X-ray fluorescence (XRF) chemical da...

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Main Authors: Leonardo Boiadeiro Ayres Negrão, Herbert Pöllmann, Tiago Kalil Cortinhas Alves
Format: Article
Language:English
Published: MDPI AG 2021-06-01
Series:Minerals
Subjects:
Online Access:https://www.mdpi.com/2075-163X/11/7/677
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spelling doaj-721867cb24cc45a9aa003659bedd690a2021-07-23T13:55:41ZengMDPI AGMinerals2075-163X2021-06-011167767710.3390/min11070677Mineralogical Appraisal of Bauxite Overburdens from BrazilLeonardo Boiadeiro Ayres Negrão0Herbert Pöllmann1Tiago Kalil Cortinhas Alves2Department of Mineralogy, Institute of Geosciences and Geography, Martin-Luther Halle-Wittenberg University, 06108 Halle, GermanyDepartment of Mineralogy, Institute of Geosciences and Geography, Martin-Luther Halle-Wittenberg University, 06108 Halle, GermanyDepartment of Mineralogy, Institute of Geosciences and Geography, Martin-Luther Halle-Wittenberg University, 06108 Halle, GermanyMineralogical appraisal is an important tool for both mining and industrial processes. X-ray powder diffraction analysis (XRPD) can deliver fast and reliable mineralogical quantification results to aid industrial processes and improve ore recoveries. Furthermore, X-ray fluorescence (XRF) chemical data, thermal analysis (TA), and Fourier-transformed infrared spectroscopy (FTIR) can be used to validate and refine XRPD results. Mineralogical assessment of non-traditional ores, such as mining wastes, is also an important step to consider them for near-future industries. In the Brazilian Amazon, alumina-rich clays cover the largest and most important bauxitic deposits of the region and have been considered as a possible raw material for the local cement and ceramic industry. In this work, a mineralogical evaluation of these clays (Belterra Clays) is performed using XRPD, XRF, TA, and FTIR. XRPD-Rietveld quantification confirmed that kaolinite is the main phase of the clay overburden, followed by variable contents of gibbsite and goethite and minor quantities of hematite, anatase, and quartz. The chemistry derived from Rietveld, based on stoichiometric phase compositions, presents a good correlation with the XRF data and is also supported by the TA and FTIR data. The initially assumed homogeneous composition of Belterra Clay is revealed to be variable by the present mineralogical study.https://www.mdpi.com/2075-163X/11/7/677bauxite overburdenBelterra Claymineralogical quantificationRietveld analysis
collection DOAJ
language English
format Article
sources DOAJ
author Leonardo Boiadeiro Ayres Negrão
Herbert Pöllmann
Tiago Kalil Cortinhas Alves
spellingShingle Leonardo Boiadeiro Ayres Negrão
Herbert Pöllmann
Tiago Kalil Cortinhas Alves
Mineralogical Appraisal of Bauxite Overburdens from Brazil
Minerals
bauxite overburden
Belterra Clay
mineralogical quantification
Rietveld analysis
author_facet Leonardo Boiadeiro Ayres Negrão
Herbert Pöllmann
Tiago Kalil Cortinhas Alves
author_sort Leonardo Boiadeiro Ayres Negrão
title Mineralogical Appraisal of Bauxite Overburdens from Brazil
title_short Mineralogical Appraisal of Bauxite Overburdens from Brazil
title_full Mineralogical Appraisal of Bauxite Overburdens from Brazil
title_fullStr Mineralogical Appraisal of Bauxite Overburdens from Brazil
title_full_unstemmed Mineralogical Appraisal of Bauxite Overburdens from Brazil
title_sort mineralogical appraisal of bauxite overburdens from brazil
publisher MDPI AG
series Minerals
issn 2075-163X
publishDate 2021-06-01
description Mineralogical appraisal is an important tool for both mining and industrial processes. X-ray powder diffraction analysis (XRPD) can deliver fast and reliable mineralogical quantification results to aid industrial processes and improve ore recoveries. Furthermore, X-ray fluorescence (XRF) chemical data, thermal analysis (TA), and Fourier-transformed infrared spectroscopy (FTIR) can be used to validate and refine XRPD results. Mineralogical assessment of non-traditional ores, such as mining wastes, is also an important step to consider them for near-future industries. In the Brazilian Amazon, alumina-rich clays cover the largest and most important bauxitic deposits of the region and have been considered as a possible raw material for the local cement and ceramic industry. In this work, a mineralogical evaluation of these clays (Belterra Clays) is performed using XRPD, XRF, TA, and FTIR. XRPD-Rietveld quantification confirmed that kaolinite is the main phase of the clay overburden, followed by variable contents of gibbsite and goethite and minor quantities of hematite, anatase, and quartz. The chemistry derived from Rietveld, based on stoichiometric phase compositions, presents a good correlation with the XRF data and is also supported by the TA and FTIR data. The initially assumed homogeneous composition of Belterra Clay is revealed to be variable by the present mineralogical study.
topic bauxite overburden
Belterra Clay
mineralogical quantification
Rietveld analysis
url https://www.mdpi.com/2075-163X/11/7/677
work_keys_str_mv AT leonardoboiadeiroayresnegrao mineralogicalappraisalofbauxiteoverburdensfrombrazil
AT herbertpollmann mineralogicalappraisalofbauxiteoverburdensfrombrazil
AT tiagokalilcortinhasalves mineralogicalappraisalofbauxiteoverburdensfrombrazil
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