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
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/133965
Ver los metadatos del registro completo
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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 |
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info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International (CC BY 4.0) |
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openAccess |
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http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International (CC BY 4.0) |
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application/pdf 1-15 |
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SEDICI (UNLP) - Universidad Nacional de La Plata |
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