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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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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