Analyzing the Spatial Occurrence of High-Alumina Clays (Brazil) Using Electrical Resistivity Tomography (ERT)

Detalhes bibliográficos
Autor(a) principal: Coelho, C. V.S. [UNESP]
Data de Publicação: 2020
Outros Autores: Moreira, C. A. [UNESP], Rosolen, V. [UNESP], Bueno, G. T., Salles, J., Furlan, L. M. [UNESP], Govone, J. S. [UNESP]
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UNESP
Texto Completo: http://dx.doi.org/10.1007/s00024-020-02444-w
http://hdl.handle.net/11449/200087
Resumo: Mottled and high-alumina clay horizons (Gleysols) above dismantled iron crusts (Ferralsols) are widespread in the soils that developed on the flat sedimentary plateau located in western Minas Gerais State (Brazil). Field exploration shows that the deposits of high-alumina clays are located at a lower topographic position, mottled horizons suggesting a lateral transformation system. Two-dimensional and pseudo-three-dimensional electrical resistivity tomography (ERT) techniques have been tested to investigate the distribution of high-alumina clay layers in a thick lateritic mantle, and to assess the potential of the technique to delimitate ore reserves. The figures of resistivity, based on spatial variations of electrical properties of the weathering layers, showed spatial changes in the subsurface structure of weathering mantle, expanding the distribution of iron crust and the high-alumina clay layers, which are strongly influenced by aquifer. Combining 2D and pseudo-3D geophysical images with soil morphology and geochemistry, we delimitate the high-alumina clay layer and discuss its genesis. The ore is located exclusively on the edge of the plateau and is closely linked to the development of hydromorphic soils, exactly where the vertical water flow is restrained by the iron crust. This distinct water regime defines the geochemical transfers in soil mantle, depleting Fe2O3 from Gleysol and correspondingly increasing Al2O3 and SiO2. This study aimed to evaluate the potential of ERT as a prospecting tool for supergene ore, and as a technique with reduced environmental impact in the mineral research, when compared to the pre-existing exploration methods (trenches, drill holes and extraction) that are applied on this sensitive wetland system in which high-alumina clays may occur.
id UNSP_2ccc558db3ad732f2876960a40bc87b4
oai_identifier_str oai:repositorio.unesp.br:11449/200087
network_acronym_str UNSP
network_name_str Repositório Institucional da UNESP
repository_id_str 2946
spelling Analyzing the Spatial Occurrence of High-Alumina Clays (Brazil) Using Electrical Resistivity Tomography (ERT)ferralsolsgleysolshydromorphic soilssedimentary plateauWetlandsMottled and high-alumina clay horizons (Gleysols) above dismantled iron crusts (Ferralsols) are widespread in the soils that developed on the flat sedimentary plateau located in western Minas Gerais State (Brazil). Field exploration shows that the deposits of high-alumina clays are located at a lower topographic position, mottled horizons suggesting a lateral transformation system. Two-dimensional and pseudo-three-dimensional electrical resistivity tomography (ERT) techniques have been tested to investigate the distribution of high-alumina clay layers in a thick lateritic mantle, and to assess the potential of the technique to delimitate ore reserves. The figures of resistivity, based on spatial variations of electrical properties of the weathering layers, showed spatial changes in the subsurface structure of weathering mantle, expanding the distribution of iron crust and the high-alumina clay layers, which are strongly influenced by aquifer. Combining 2D and pseudo-3D geophysical images with soil morphology and geochemistry, we delimitate the high-alumina clay layer and discuss its genesis. The ore is located exclusively on the edge of the plateau and is closely linked to the development of hydromorphic soils, exactly where the vertical water flow is restrained by the iron crust. This distinct water regime defines the geochemical transfers in soil mantle, depleting Fe2O3 from Gleysol and correspondingly increasing Al2O3 and SiO2. This study aimed to evaluate the potential of ERT as a prospecting tool for supergene ore, and as a technique with reduced environmental impact in the mineral research, when compared to the pre-existing exploration methods (trenches, drill holes and extraction) that are applied on this sensitive wetland system in which high-alumina clays may occur.Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)Departamento de Petrologia e Metalogenia (DPM) Universidade Estadual Paulista (UNESP), Av. 24A, 1515, Bela Vista, CP: 178Departamento de Geologia Aplicada (DGA) Universidade Estadual Paulista (UNESP), Av. 24A, 1515, Bela VistaInstituto de Estudos Sócio-Ambiental (IESA) Universidade Federal Goiás (UFG)Centro de Estudos Ambientais (CEA) Universidade Estadual Paulista (UNESP), Av. 24A, 1515, Bela VistaDepartamento de Petrologia e Metalogenia (DPM) Universidade Estadual Paulista (UNESP), Av. 24A, 1515, Bela Vista, CP: 178Departamento de Geologia Aplicada (DGA) Universidade Estadual Paulista (UNESP), Av. 24A, 1515, Bela VistaCentro de Estudos Ambientais (CEA) Universidade Estadual Paulista (UNESP), Av. 24A, 1515, Bela VistaFAPESP: 2014/01131-4Universidade Estadual Paulista (Unesp)Universidade Federal Goiás (UFG)Coelho, C. V.S. [UNESP]Moreira, C. A. [UNESP]Rosolen, V. [UNESP]Bueno, G. T.Salles, J.Furlan, L. M. [UNESP]Govone, J. S. [UNESP]2020-12-12T01:57:20Z2020-12-12T01:57:20Z2020-08-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/article3943-3960http://dx.doi.org/10.1007/s00024-020-02444-wPure and Applied Geophysics, v. 177, n. 8, p. 3943-3960, 2020.1420-91360033-4553http://hdl.handle.net/11449/20008710.1007/s00024-020-02444-w2-s2.0-8507973629690868573123910800000-0002-6949-6679Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengPure and Applied Geophysicsinfo:eu-repo/semantics/openAccess2021-10-23T11:59:56Zoai:repositorio.unesp.br:11449/200087Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462021-10-23T11:59:56Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false
dc.title.none.fl_str_mv Analyzing the Spatial Occurrence of High-Alumina Clays (Brazil) Using Electrical Resistivity Tomography (ERT)
title Analyzing the Spatial Occurrence of High-Alumina Clays (Brazil) Using Electrical Resistivity Tomography (ERT)
spellingShingle Analyzing the Spatial Occurrence of High-Alumina Clays (Brazil) Using Electrical Resistivity Tomography (ERT)
Coelho, C. V.S. [UNESP]
ferralsols
gleysols
hydromorphic soils
sedimentary plateau
Wetlands
title_short Analyzing the Spatial Occurrence of High-Alumina Clays (Brazil) Using Electrical Resistivity Tomography (ERT)
title_full Analyzing the Spatial Occurrence of High-Alumina Clays (Brazil) Using Electrical Resistivity Tomography (ERT)
title_fullStr Analyzing the Spatial Occurrence of High-Alumina Clays (Brazil) Using Electrical Resistivity Tomography (ERT)
title_full_unstemmed Analyzing the Spatial Occurrence of High-Alumina Clays (Brazil) Using Electrical Resistivity Tomography (ERT)
title_sort Analyzing the Spatial Occurrence of High-Alumina Clays (Brazil) Using Electrical Resistivity Tomography (ERT)
author Coelho, C. V.S. [UNESP]
author_facet Coelho, C. V.S. [UNESP]
Moreira, C. A. [UNESP]
Rosolen, V. [UNESP]
Bueno, G. T.
Salles, J.
Furlan, L. M. [UNESP]
Govone, J. S. [UNESP]
author_role author
author2 Moreira, C. A. [UNESP]
Rosolen, V. [UNESP]
Bueno, G. T.
Salles, J.
Furlan, L. M. [UNESP]
Govone, J. S. [UNESP]
author2_role author
author
author
author
author
author
dc.contributor.none.fl_str_mv Universidade Estadual Paulista (Unesp)
Universidade Federal Goiás (UFG)
dc.contributor.author.fl_str_mv Coelho, C. V.S. [UNESP]
Moreira, C. A. [UNESP]
Rosolen, V. [UNESP]
Bueno, G. T.
Salles, J.
Furlan, L. M. [UNESP]
Govone, J. S. [UNESP]
dc.subject.por.fl_str_mv ferralsols
gleysols
hydromorphic soils
sedimentary plateau
Wetlands
topic ferralsols
gleysols
hydromorphic soils
sedimentary plateau
Wetlands
description Mottled and high-alumina clay horizons (Gleysols) above dismantled iron crusts (Ferralsols) are widespread in the soils that developed on the flat sedimentary plateau located in western Minas Gerais State (Brazil). Field exploration shows that the deposits of high-alumina clays are located at a lower topographic position, mottled horizons suggesting a lateral transformation system. Two-dimensional and pseudo-three-dimensional electrical resistivity tomography (ERT) techniques have been tested to investigate the distribution of high-alumina clay layers in a thick lateritic mantle, and to assess the potential of the technique to delimitate ore reserves. The figures of resistivity, based on spatial variations of electrical properties of the weathering layers, showed spatial changes in the subsurface structure of weathering mantle, expanding the distribution of iron crust and the high-alumina clay layers, which are strongly influenced by aquifer. Combining 2D and pseudo-3D geophysical images with soil morphology and geochemistry, we delimitate the high-alumina clay layer and discuss its genesis. The ore is located exclusively on the edge of the plateau and is closely linked to the development of hydromorphic soils, exactly where the vertical water flow is restrained by the iron crust. This distinct water regime defines the geochemical transfers in soil mantle, depleting Fe2O3 from Gleysol and correspondingly increasing Al2O3 and SiO2. This study aimed to evaluate the potential of ERT as a prospecting tool for supergene ore, and as a technique with reduced environmental impact in the mineral research, when compared to the pre-existing exploration methods (trenches, drill holes and extraction) that are applied on this sensitive wetland system in which high-alumina clays may occur.
publishDate 2020
dc.date.none.fl_str_mv 2020-12-12T01:57:20Z
2020-12-12T01:57:20Z
2020-08-01
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://dx.doi.org/10.1007/s00024-020-02444-w
Pure and Applied Geophysics, v. 177, n. 8, p. 3943-3960, 2020.
1420-9136
0033-4553
http://hdl.handle.net/11449/200087
10.1007/s00024-020-02444-w
2-s2.0-85079736296
9086857312391080
0000-0002-6949-6679
url http://dx.doi.org/10.1007/s00024-020-02444-w
http://hdl.handle.net/11449/200087
identifier_str_mv Pure and Applied Geophysics, v. 177, n. 8, p. 3943-3960, 2020.
1420-9136
0033-4553
10.1007/s00024-020-02444-w
2-s2.0-85079736296
9086857312391080
0000-0002-6949-6679
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Pure and Applied Geophysics
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv 3943-3960
dc.source.none.fl_str_mv Scopus
reponame:Repositório Institucional da UNESP
instname:Universidade Estadual Paulista (UNESP)
instacron:UNESP
instname_str Universidade Estadual Paulista (UNESP)
instacron_str UNESP
institution UNESP
reponame_str Repositório Institucional da UNESP
collection Repositório Institucional da UNESP
repository.name.fl_str_mv Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)
repository.mail.fl_str_mv
_version_ 1803046318188265472