Characterization of Magnetic Tailings from Phosphate-Ore Processing in Alto Paranaíba

Detalhes bibliográficos
Autor(a) principal: Silva,Fernando Brandão Rodrigues da
Data de Publicação: 2022
Outros Autores: Araújo,Fernando Gabriel Silva, von Krüger,Fernando Leopoldo, Silva,Guilherme Jorge Brigolini, Batista,Ronaldo Junio Campos, Manhabosco,Taíse Matte
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Materials research (São Carlos. Online)
Texto Completo: http://old.scielo.br/scielo.php?script=sci_arttext&pid=S1516-14392022000100334
Resumo: The characterization studies of tailings from mining are crucial for the development of its reuse processes and the reduction of impacts caused by its conditioning on the earth’s surface. This study characterizes the magnetic tailings from phosphate-rock processing using X-ray diffraction, X-ray fluorescence spectrometry and quantitative electron microscopy techniques. Samples were obtained from the magnetic tailings deposit of a mining company in the Alto Paranaíba region, Minas Gerais. The tailings are mainly composed of hematite/magnetite (74.92%), ilmenite (8.91%), fluorapatite (8.8%), anatase (3.07%), calcite (1.67%), goethite (1.62%), and quartz (1.02%). The particle size of the tailings is smaller than that specified for the production of sinter feed. The hematite/magnetite phase is strongly associated with ilmenite and fluorapatite. New stages of comminution and separation are needed due to the low degree of liberation of these minerals for a possible reuse of the components.
id ABMABCABPOL-1_a4e309fe81c34e45955089bc3f0d97e0
oai_identifier_str oai:scielo:S1516-14392022000100334
network_acronym_str ABMABCABPOL-1
network_name_str Materials research (São Carlos. Online)
repository_id_str
spelling Characterization of Magnetic Tailings from Phosphate-Ore Processing in Alto ParanaíbaMagnetic tailingCharacterizationQEMThe characterization studies of tailings from mining are crucial for the development of its reuse processes and the reduction of impacts caused by its conditioning on the earth’s surface. This study characterizes the magnetic tailings from phosphate-rock processing using X-ray diffraction, X-ray fluorescence spectrometry and quantitative electron microscopy techniques. Samples were obtained from the magnetic tailings deposit of a mining company in the Alto Paranaíba region, Minas Gerais. The tailings are mainly composed of hematite/magnetite (74.92%), ilmenite (8.91%), fluorapatite (8.8%), anatase (3.07%), calcite (1.67%), goethite (1.62%), and quartz (1.02%). The particle size of the tailings is smaller than that specified for the production of sinter feed. The hematite/magnetite phase is strongly associated with ilmenite and fluorapatite. New stages of comminution and separation are needed due to the low degree of liberation of these minerals for a possible reuse of the components.ABM, ABC, ABPol2022-01-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S1516-14392022000100334Materials Research v.25 2022reponame:Materials research (São Carlos. Online)instname:Universidade Federal de São Carlos (UFSCAR)instacron:ABM ABC ABPOL10.1590/1980-5373-mr-2021-0621info:eu-repo/semantics/openAccessSilva,Fernando Brandão Rodrigues daAraújo,Fernando Gabriel Silvavon Krüger,Fernando LeopoldoSilva,Guilherme Jorge BrigoliniBatista,Ronaldo Junio CamposManhabosco,Taíse Matteeng2022-08-01T00:00:00Zoai:scielo:S1516-14392022000100334Revistahttp://www.scielo.br/mrPUBhttps://old.scielo.br/oai/scielo-oai.phpdedz@power.ufscar.br1980-53731516-1439opendoar:2022-08-01T00:00Materials research (São Carlos. Online) - Universidade Federal de São Carlos (UFSCAR)false
dc.title.none.fl_str_mv Characterization of Magnetic Tailings from Phosphate-Ore Processing in Alto Paranaíba
title Characterization of Magnetic Tailings from Phosphate-Ore Processing in Alto Paranaíba
spellingShingle Characterization of Magnetic Tailings from Phosphate-Ore Processing in Alto Paranaíba
Silva,Fernando Brandão Rodrigues da
Magnetic tailing
Characterization
QEM
title_short Characterization of Magnetic Tailings from Phosphate-Ore Processing in Alto Paranaíba
title_full Characterization of Magnetic Tailings from Phosphate-Ore Processing in Alto Paranaíba
title_fullStr Characterization of Magnetic Tailings from Phosphate-Ore Processing in Alto Paranaíba
title_full_unstemmed Characterization of Magnetic Tailings from Phosphate-Ore Processing in Alto Paranaíba
title_sort Characterization of Magnetic Tailings from Phosphate-Ore Processing in Alto Paranaíba
author Silva,Fernando Brandão Rodrigues da
author_facet Silva,Fernando Brandão Rodrigues da
Araújo,Fernando Gabriel Silva
von Krüger,Fernando Leopoldo
Silva,Guilherme Jorge Brigolini
Batista,Ronaldo Junio Campos
Manhabosco,Taíse Matte
author_role author
author2 Araújo,Fernando Gabriel Silva
von Krüger,Fernando Leopoldo
Silva,Guilherme Jorge Brigolini
Batista,Ronaldo Junio Campos
Manhabosco,Taíse Matte
author2_role author
author
author
author
author
dc.contributor.author.fl_str_mv Silva,Fernando Brandão Rodrigues da
Araújo,Fernando Gabriel Silva
von Krüger,Fernando Leopoldo
Silva,Guilherme Jorge Brigolini
Batista,Ronaldo Junio Campos
Manhabosco,Taíse Matte
dc.subject.por.fl_str_mv Magnetic tailing
Characterization
QEM
topic Magnetic tailing
Characterization
QEM
description The characterization studies of tailings from mining are crucial for the development of its reuse processes and the reduction of impacts caused by its conditioning on the earth’s surface. This study characterizes the magnetic tailings from phosphate-rock processing using X-ray diffraction, X-ray fluorescence spectrometry and quantitative electron microscopy techniques. Samples were obtained from the magnetic tailings deposit of a mining company in the Alto Paranaíba region, Minas Gerais. The tailings are mainly composed of hematite/magnetite (74.92%), ilmenite (8.91%), fluorapatite (8.8%), anatase (3.07%), calcite (1.67%), goethite (1.62%), and quartz (1.02%). The particle size of the tailings is smaller than that specified for the production of sinter feed. The hematite/magnetite phase is strongly associated with ilmenite and fluorapatite. New stages of comminution and separation are needed due to the low degree of liberation of these minerals for a possible reuse of the components.
publishDate 2022
dc.date.none.fl_str_mv 2022-01-01
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://old.scielo.br/scielo.php?script=sci_arttext&pid=S1516-14392022000100334
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S1516-14392022000100334
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 10.1590/1980-5373-mr-2021-0621
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv text/html
dc.publisher.none.fl_str_mv ABM, ABC, ABPol
publisher.none.fl_str_mv ABM, ABC, ABPol
dc.source.none.fl_str_mv Materials Research v.25 2022
reponame:Materials research (São Carlos. Online)
instname:Universidade Federal de São Carlos (UFSCAR)
instacron:ABM ABC ABPOL
instname_str Universidade Federal de São Carlos (UFSCAR)
instacron_str ABM ABC ABPOL
institution ABM ABC ABPOL
reponame_str Materials research (São Carlos. Online)
collection Materials research (São Carlos. Online)
repository.name.fl_str_mv Materials research (São Carlos. Online) - Universidade Federal de São Carlos (UFSCAR)
repository.mail.fl_str_mv dedz@power.ufscar.br
_version_ 1754212681353527296