Mössbauer study of the Fe mineralogy in two different Argentine soils

Two Argentine soils featuring different characteristics and compositions (mollisols and ultisols) have been studied by Mössbauer spectroscopy and X-ray diffraction. The first type has a weakly developed profile with a solum thickness of 40 cm; the Fe oxyhydroxides are present in low concentrations i...

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Detalles Bibliográficos
Autores principales:	Mijovilovich, Ana Esther, Causevic, Hernán, Saragovi, Celia
Publicado:	1999
Materias:	Fe-mineralogy Lithological characteristics and pedological evolution Mössbauer spectroscopy Mollisols Ultisols X-ray diffraction
Acceso en línea:	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03043843_v122_n1-2_p83_Mijovilovich http://hdl.handle.net/20.500.12110/paper_03043843_v122_n1-2_p83_Mijovilovich
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

id	paper:paper_03043843_v122_n1-2_p83_Mijovilovich
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spelling	paper:paper_03043843_v122_n1-2_p83_Mijovilovich2023-06-08T15:29:20Z Mössbauer study of the Fe mineralogy in two different Argentine soils Mijovilovich, Ana Esther Causevic, Hernán Saragovi, Celia Fe-mineralogy Lithological characteristics and pedological evolution Mössbauer spectroscopy Mollisols Ultisols X-ray diffraction Two Argentine soils featuring different characteristics and compositions (mollisols and ultisols) have been studied by Mössbauer spectroscopy and X-ray diffraction. The first type has a weakly developed profile with a solum thickness of 40 cm; the Fe oxyhydroxides are present in low concentrations in mixtures with other slightly weathered minerals (e.g., quartz, feldspars, 2 : 1 phyllosilicates, etc.). The second one is a typic kandihumult, which is a highly weathered red coloured, deep soil. The Fe oxyhydroxides are abundant, mixed mainly with kaolinite clay minerals. Analyses of iron mineralogy show hematite and goethite in both soils. Their ratio is low in the first case and high in the last case. Magnetite-maghemite are also present in both situations, but in the mollisol their content is much lower than in the ultisol. The mineralogy found is related to the different lithological characteristics and processes of pedological evolution on both soils. Fil:Mijovilovich, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Causevic, H. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Saragovi, C. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 1999 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03043843_v122_n1-2_p83_Mijovilovich http://hdl.handle.net/20.500.12110/paper_03043843_v122_n1-2_p83_Mijovilovich
institution	Universidad de Buenos Aires
institution_str	I-28
repository_str	R-134
collection	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic	Fe-mineralogy Lithological characteristics and pedological evolution Mössbauer spectroscopy Mollisols Ultisols X-ray diffraction
spellingShingle	Fe-mineralogy Lithological characteristics and pedological evolution Mössbauer spectroscopy Mollisols Ultisols X-ray diffraction Mijovilovich, Ana Esther Causevic, Hernán Saragovi, Celia Mössbauer study of the Fe mineralogy in two different Argentine soils
topic_facet	Fe-mineralogy Lithological characteristics and pedological evolution Mössbauer spectroscopy Mollisols Ultisols X-ray diffraction
description	Two Argentine soils featuring different characteristics and compositions (mollisols and ultisols) have been studied by Mössbauer spectroscopy and X-ray diffraction. The first type has a weakly developed profile with a solum thickness of 40 cm; the Fe oxyhydroxides are present in low concentrations in mixtures with other slightly weathered minerals (e.g., quartz, feldspars, 2 : 1 phyllosilicates, etc.). The second one is a typic kandihumult, which is a highly weathered red coloured, deep soil. The Fe oxyhydroxides are abundant, mixed mainly with kaolinite clay minerals. Analyses of iron mineralogy show hematite and goethite in both soils. Their ratio is low in the first case and high in the last case. Magnetite-maghemite are also present in both situations, but in the mollisol their content is much lower than in the ultisol. The mineralogy found is related to the different lithological characteristics and processes of pedological evolution on both soils.
author	Mijovilovich, Ana Esther Causevic, Hernán Saragovi, Celia
author_facet	Mijovilovich, Ana Esther Causevic, Hernán Saragovi, Celia
author_sort	Mijovilovich, Ana Esther
title	Mössbauer study of the Fe mineralogy in two different Argentine soils
title_short	Mössbauer study of the Fe mineralogy in two different Argentine soils
title_full	Mössbauer study of the Fe mineralogy in two different Argentine soils
title_fullStr	Mössbauer study of the Fe mineralogy in two different Argentine soils
title_full_unstemmed	Mössbauer study of the Fe mineralogy in two different Argentine soils
title_sort	mössbauer study of the fe mineralogy in two different argentine soils
publishDate	1999
url	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03043843_v122_n1-2_p83_Mijovilovich http://hdl.handle.net/20.500.12110/paper_03043843_v122_n1-2_p83_Mijovilovich
work_keys_str_mv	AT mijovilovichanaesther mossbauerstudyofthefemineralogyintwodifferentargentinesoils AT causevichernan mossbauerstudyofthefemineralogyintwodifferentargentinesoils AT saragovicelia mossbauerstudyofthefemineralogyintwodifferentargentinesoils
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Mössbauer study of the Fe mineralogy in two different Argentine soils

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