The origin of gley colors in hydromorphic vertisols : The study case of the coastal plain of the Río de la Plata estuary

Autores
Gómez Samus, Mauro Leandro; Comerio, Marcos Alejandro; Montes, María Luciana; Boff, Laura Daniela; Löffler, Julia; Mercader, Roberto Carlos; Bidegain, Juan Carlos
Año de publicación
2021
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
This work aims to contribute to the interpretation of soil colors; mainly to identify the pigments that generate the greenish colors in hydromorphic conditions (gley colors) in vertisols of the coastal plain of the Rio de la Plata estuary. These colors are of cold hues, generally greenish (olive-gray), and occur in poorly drained soils with prolonged water accumulation. For this purpose, samples of Bssg horizons of hydromorphic vertisols from the coastal plain of the Rio de la Plata estuary were analyzed using routine and chemical analyses, Mossbauer spectroscopy, determination of rocks magnetic parameters, X-ray diffraction, thermogravimetric and differential thermal analysis and petrographic-electronic microscopy. The pigments associated with the gley colors of these soils are mainly due to ferric iron content, corresponding to minerals such as ferric iron-rich smectites (nontronite/Fe-rich beidellite) and oxy-hydroxides like goethite, which colors range from green to yellow. These minerals, combined with gray or black components, e.g., manganese compounds and/or organic matter, contribute to the generation of the usual gley colors in the analyzed soils of the Pampean plain. The obtained data allows us to state that it is a mistake to assing the olive color in hydromorphic soils to the presence of ferrous iron compounds, as it is traditionally done. The oxidizing condition of iron is dominant in all the analyzed samples, integrating the composition of ferric iron-rich clay minerals and oxy-hydroxides (goethite).
Instituto de Física La Plata
Laboratorio de Entrenamiento Multidisciplinario para la Investigación Tecnológica
Materia
Ciencias Exactas
Química
Vertisol
Gleysol
Stagnosol
Goethite
Nontronite
Beidellite
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/133965

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repository_id_str 1329
network_name_str SEDICI (UNLP)
spelling The origin of gley colors in hydromorphic vertisols : The study case of the coastal plain of the Río de la Plata estuaryGómez Samus, Mauro LeandroComerio, Marcos AlejandroMontes, María LucianaBoff, Laura DanielaLöffler, JuliaMercader, Roberto CarlosBidegain, Juan CarlosCiencias ExactasQuímicaVertisolGleysolStagnosolGoethiteNontroniteBeidelliteThis work aims to contribute to the interpretation of soil colors; mainly to identify the pigments that generate the greenish colors in hydromorphic conditions (gley colors) in vertisols of the coastal plain of the Rio de la Plata estuary. These colors are of cold hues, generally greenish (olive-gray), and occur in poorly drained soils with prolonged water accumulation. For this purpose, samples of Bssg horizons of hydromorphic vertisols from the coastal plain of the Rio de la Plata estuary were analyzed using routine and chemical analyses, Mossbauer spectroscopy, determination of rocks magnetic parameters, X-ray diffraction, thermogravimetric and differential thermal analysis and petrographic-electronic microscopy. The pigments associated with the gley colors of these soils are mainly due to ferric iron content, corresponding to minerals such as ferric iron-rich smectites (nontronite/Fe-rich beidellite) and oxy-hydroxides like goethite, which colors range from green to yellow. These minerals, combined with gray or black components, e.g., manganese compounds and/or organic matter, contribute to the generation of the usual gley colors in the analyzed soils of the Pampean plain. The obtained data allows us to state that it is a mistake to assing the olive color in hydromorphic soils to the presence of ferrous iron compounds, as it is traditionally done. The oxidizing condition of iron is dominant in all the analyzed samples, integrating the composition of ferric iron-rich clay minerals and oxy-hydroxides (goethite).Instituto de Física La PlataLaboratorio de Entrenamiento Multidisciplinario para la Investigación Tecnológica2021-01-29info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdf1-15http://sedici.unlp.edu.ar/handle/10915/133965enginfo:eu-repo/semantics/altIdentifier/issn/1866-6280info:eu-repo/semantics/altIdentifier/issn/1866-6299info:eu-repo/semantics/altIdentifier/doi/10.1007/s12665-021-09391-2info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/4.0/Creative Commons Attribution 4.0 International (CC BY 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-09-03T11:03:54Zoai:sedici.unlp.edu.ar:10915/133965Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-03 11:03:54.306SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv The origin of gley colors in hydromorphic vertisols : The study case of the coastal plain of the Río de la Plata estuary
title The origin of gley colors in hydromorphic vertisols : The study case of the coastal plain of the Río de la Plata estuary
spellingShingle The origin of gley colors in hydromorphic vertisols : The study case of the coastal plain of the Río de la Plata estuary
Gómez Samus, Mauro Leandro
Ciencias Exactas
Química
Vertisol
Gleysol
Stagnosol
Goethite
Nontronite
Beidellite
title_short The origin of gley colors in hydromorphic vertisols : The study case of the coastal plain of the Río de la Plata estuary
title_full The origin of gley colors in hydromorphic vertisols : The study case of the coastal plain of the Río de la Plata estuary
title_fullStr The origin of gley colors in hydromorphic vertisols : The study case of the coastal plain of the Río de la Plata estuary
title_full_unstemmed The origin of gley colors in hydromorphic vertisols : The study case of the coastal plain of the Río de la Plata estuary
title_sort The origin of gley colors in hydromorphic vertisols : The study case of the coastal plain of the Río de la Plata estuary
dc.creator.none.fl_str_mv Gómez Samus, Mauro Leandro
Comerio, Marcos Alejandro
Montes, María Luciana
Boff, Laura Daniela
Löffler, Julia
Mercader, Roberto Carlos
Bidegain, Juan Carlos
author Gómez Samus, Mauro Leandro
author_facet Gómez Samus, Mauro Leandro
Comerio, Marcos Alejandro
Montes, María Luciana
Boff, Laura Daniela
Löffler, Julia
Mercader, Roberto Carlos
Bidegain, Juan Carlos
author_role author
author2 Comerio, Marcos Alejandro
Montes, María Luciana
Boff, Laura Daniela
Löffler, Julia
Mercader, Roberto Carlos
Bidegain, Juan Carlos
author2_role author
author
author
author
author
author
dc.subject.none.fl_str_mv Ciencias Exactas
Química
Vertisol
Gleysol
Stagnosol
Goethite
Nontronite
Beidellite
topic Ciencias Exactas
Química
Vertisol
Gleysol
Stagnosol
Goethite
Nontronite
Beidellite
dc.description.none.fl_txt_mv This work aims to contribute to the interpretation of soil colors; mainly to identify the pigments that generate the greenish colors in hydromorphic conditions (gley colors) in vertisols of the coastal plain of the Rio de la Plata estuary. These colors are of cold hues, generally greenish (olive-gray), and occur in poorly drained soils with prolonged water accumulation. For this purpose, samples of Bssg horizons of hydromorphic vertisols from the coastal plain of the Rio de la Plata estuary were analyzed using routine and chemical analyses, Mossbauer spectroscopy, determination of rocks magnetic parameters, X-ray diffraction, thermogravimetric and differential thermal analysis and petrographic-electronic microscopy. The pigments associated with the gley colors of these soils are mainly due to ferric iron content, corresponding to minerals such as ferric iron-rich smectites (nontronite/Fe-rich beidellite) and oxy-hydroxides like goethite, which colors range from green to yellow. These minerals, combined with gray or black components, e.g., manganese compounds and/or organic matter, contribute to the generation of the usual gley colors in the analyzed soils of the Pampean plain. The obtained data allows us to state that it is a mistake to assing the olive color in hydromorphic soils to the presence of ferrous iron compounds, as it is traditionally done. The oxidizing condition of iron is dominant in all the analyzed samples, integrating the composition of ferric iron-rich clay minerals and oxy-hydroxides (goethite).
Instituto de Física La Plata
Laboratorio de Entrenamiento Multidisciplinario para la Investigación Tecnológica
description This work aims to contribute to the interpretation of soil colors; mainly to identify the pigments that generate the greenish colors in hydromorphic conditions (gley colors) in vertisols of the coastal plain of the Rio de la Plata estuary. These colors are of cold hues, generally greenish (olive-gray), and occur in poorly drained soils with prolonged water accumulation. For this purpose, samples of Bssg horizons of hydromorphic vertisols from the coastal plain of the Rio de la Plata estuary were analyzed using routine and chemical analyses, Mossbauer spectroscopy, determination of rocks magnetic parameters, X-ray diffraction, thermogravimetric and differential thermal analysis and petrographic-electronic microscopy. The pigments associated with the gley colors of these soils are mainly due to ferric iron content, corresponding to minerals such as ferric iron-rich smectites (nontronite/Fe-rich beidellite) and oxy-hydroxides like goethite, which colors range from green to yellow. These minerals, combined with gray or black components, e.g., manganese compounds and/or organic matter, contribute to the generation of the usual gley colors in the analyzed soils of the Pampean plain. The obtained data allows us to state that it is a mistake to assing the olive color in hydromorphic soils to the presence of ferrous iron compounds, as it is traditionally done. The oxidizing condition of iron is dominant in all the analyzed samples, integrating the composition of ferric iron-rich clay minerals and oxy-hydroxides (goethite).
publishDate 2021
dc.date.none.fl_str_mv 2021-01-29
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
Articulo
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://sedici.unlp.edu.ar/handle/10915/133965
url http://sedici.unlp.edu.ar/handle/10915/133965
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/issn/1866-6280
info:eu-repo/semantics/altIdentifier/issn/1866-6299
info:eu-repo/semantics/altIdentifier/doi/10.1007/s12665-021-09391-2
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International (CC BY 4.0)
eu_rights_str_mv openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International (CC BY 4.0)
dc.format.none.fl_str_mv application/pdf
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repository.name.fl_str_mv SEDICI (UNLP) - Universidad Nacional de La Plata
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