Soil acidity changes in bulk soil and maize rhizosphere in response to nitrogen fertilization

Autores
Rodriguez, M. B.; Godeas, Alicia Margarita; Lavado, Raul Silvio
Año de publicación
2008
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The capacity of nitrogen (N) fertilizers to acidify the soil is regulated principally by the rate and N source. Nitrogen fertilizers undergo hydrolysis and nitrification in soil, resulting in the release of free hydrogen (H+) ions. Simultaneously, ammonium (NH4 +) absorption by roots strongly acidifies the rhizosphere, whereas absorption of nitrate (NO3 -) slightly alkalinizes it. The rhizosphere effects on soil acidity and plant growth in conjunction with N rate are not clearly known. To assess the impact of these multiple factors, changes in the acidity of a Typic Argiudol soil, fertilized with two N sources (urea and UAN) at two rates (equivalent to 100 and 200 kg N ha-1), were studied in a greenhouse experiment using maize as the experimental plant. Soil pH (measured in a soil-water slurry), total acidity, exchangeable acidity, and exchangeable aluminum (Al) were measured in rhizospheric and bulk soil. Plant biomass and foliar area (FA) were also measured at the V6 stage. Nitrogen fertilization significantly reduce the pH in the bulk soil by 0.3 and 0.5 units for low and high rates respectively. Changes in the rhizosphere (the "rhizospheric effect") resulted in a significant increase in soil pH, from 5.9 to 6.2. The rhizospheric effect x N source interaction significantly increased exchangeable acidity in the rhizosphere relative to bulk soil, particularly when UAN was added at a low rate. Only total acidity was significantly increased by the fertilizer application rate. In spite of the bulk soil acidification, no significant differences in exchangeable aluminum were detected. Aerial biomass and FA were significantly increased by the higher N rate, but N source had no effect on them. Although changes in acidity were observed, root biomass was not significantly affected.
Fil: Rodriguez, M. B.. Universidad de Buenos Aires; Argentina
Fil: Godeas, Alicia Margarita. Universidad de Buenos Aires; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Lavado, Raul Silvio. Universidad de Buenos Aires; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Materia
MAIZE
NITROGEN FERTILIZATION
RHIZOSPHERE
SOIL ACIDITY
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/163834

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network_name_str CONICET Digital (CONICET)
spelling Soil acidity changes in bulk soil and maize rhizosphere in response to nitrogen fertilizationRodriguez, M. B.Godeas, Alicia MargaritaLavado, Raul SilvioMAIZENITROGEN FERTILIZATIONRHIZOSPHERESOIL ACIDITYhttps://purl.org/becyt/ford/1.6https://purl.org/becyt/ford/1The capacity of nitrogen (N) fertilizers to acidify the soil is regulated principally by the rate and N source. Nitrogen fertilizers undergo hydrolysis and nitrification in soil, resulting in the release of free hydrogen (H+) ions. Simultaneously, ammonium (NH4 +) absorption by roots strongly acidifies the rhizosphere, whereas absorption of nitrate (NO3 -) slightly alkalinizes it. The rhizosphere effects on soil acidity and plant growth in conjunction with N rate are not clearly known. To assess the impact of these multiple factors, changes in the acidity of a Typic Argiudol soil, fertilized with two N sources (urea and UAN) at two rates (equivalent to 100 and 200 kg N ha-1), were studied in a greenhouse experiment using maize as the experimental plant. Soil pH (measured in a soil-water slurry), total acidity, exchangeable acidity, and exchangeable aluminum (Al) were measured in rhizospheric and bulk soil. Plant biomass and foliar area (FA) were also measured at the V6 stage. Nitrogen fertilization significantly reduce the pH in the bulk soil by 0.3 and 0.5 units for low and high rates respectively. Changes in the rhizosphere (the "rhizospheric effect") resulted in a significant increase in soil pH, from 5.9 to 6.2. The rhizospheric effect x N source interaction significantly increased exchangeable acidity in the rhizosphere relative to bulk soil, particularly when UAN was added at a low rate. Only total acidity was significantly increased by the fertilizer application rate. In spite of the bulk soil acidification, no significant differences in exchangeable aluminum were detected. Aerial biomass and FA were significantly increased by the higher N rate, but N source had no effect on them. Although changes in acidity were observed, root biomass was not significantly affected.Fil: Rodriguez, M. B.. Universidad de Buenos Aires; ArgentinaFil: Godeas, Alicia Margarita. Universidad de Buenos Aires; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Lavado, Raul Silvio. Universidad de Buenos Aires; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaTaylor & Francis2008-10info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/163834Rodriguez, M. B.; Godeas, Alicia Margarita; Lavado, Raul Silvio; Soil acidity changes in bulk soil and maize rhizosphere in response to nitrogen fertilization; Taylor & Francis; Communications in Soil Science and Plant Analysis; 39; 17-18; 10-2008; 2597-26070010-3624CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.tandfonline.com/doi/abs/10.1080/00103620802358656info:eu-repo/semantics/altIdentifier/doi/10.1080/00103620802358656info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-10T13:13:00Zoai:ri.conicet.gov.ar:11336/163834instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-10 13:13:00.474CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Soil acidity changes in bulk soil and maize rhizosphere in response to nitrogen fertilization
title Soil acidity changes in bulk soil and maize rhizosphere in response to nitrogen fertilization
spellingShingle Soil acidity changes in bulk soil and maize rhizosphere in response to nitrogen fertilization
Rodriguez, M. B.
MAIZE
NITROGEN FERTILIZATION
RHIZOSPHERE
SOIL ACIDITY
title_short Soil acidity changes in bulk soil and maize rhizosphere in response to nitrogen fertilization
title_full Soil acidity changes in bulk soil and maize rhizosphere in response to nitrogen fertilization
title_fullStr Soil acidity changes in bulk soil and maize rhizosphere in response to nitrogen fertilization
title_full_unstemmed Soil acidity changes in bulk soil and maize rhizosphere in response to nitrogen fertilization
title_sort Soil acidity changes in bulk soil and maize rhizosphere in response to nitrogen fertilization
dc.creator.none.fl_str_mv Rodriguez, M. B.
Godeas, Alicia Margarita
Lavado, Raul Silvio
author Rodriguez, M. B.
author_facet Rodriguez, M. B.
Godeas, Alicia Margarita
Lavado, Raul Silvio
author_role author
author2 Godeas, Alicia Margarita
Lavado, Raul Silvio
author2_role author
author
dc.subject.none.fl_str_mv MAIZE
NITROGEN FERTILIZATION
RHIZOSPHERE
SOIL ACIDITY
topic MAIZE
NITROGEN FERTILIZATION
RHIZOSPHERE
SOIL ACIDITY
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.6
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv The capacity of nitrogen (N) fertilizers to acidify the soil is regulated principally by the rate and N source. Nitrogen fertilizers undergo hydrolysis and nitrification in soil, resulting in the release of free hydrogen (H+) ions. Simultaneously, ammonium (NH4 +) absorption by roots strongly acidifies the rhizosphere, whereas absorption of nitrate (NO3 -) slightly alkalinizes it. The rhizosphere effects on soil acidity and plant growth in conjunction with N rate are not clearly known. To assess the impact of these multiple factors, changes in the acidity of a Typic Argiudol soil, fertilized with two N sources (urea and UAN) at two rates (equivalent to 100 and 200 kg N ha-1), were studied in a greenhouse experiment using maize as the experimental plant. Soil pH (measured in a soil-water slurry), total acidity, exchangeable acidity, and exchangeable aluminum (Al) were measured in rhizospheric and bulk soil. Plant biomass and foliar area (FA) were also measured at the V6 stage. Nitrogen fertilization significantly reduce the pH in the bulk soil by 0.3 and 0.5 units for low and high rates respectively. Changes in the rhizosphere (the "rhizospheric effect") resulted in a significant increase in soil pH, from 5.9 to 6.2. The rhizospheric effect x N source interaction significantly increased exchangeable acidity in the rhizosphere relative to bulk soil, particularly when UAN was added at a low rate. Only total acidity was significantly increased by the fertilizer application rate. In spite of the bulk soil acidification, no significant differences in exchangeable aluminum were detected. Aerial biomass and FA were significantly increased by the higher N rate, but N source had no effect on them. Although changes in acidity were observed, root biomass was not significantly affected.
Fil: Rodriguez, M. B.. Universidad de Buenos Aires; Argentina
Fil: Godeas, Alicia Margarita. Universidad de Buenos Aires; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Lavado, Raul Silvio. Universidad de Buenos Aires; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
description The capacity of nitrogen (N) fertilizers to acidify the soil is regulated principally by the rate and N source. Nitrogen fertilizers undergo hydrolysis and nitrification in soil, resulting in the release of free hydrogen (H+) ions. Simultaneously, ammonium (NH4 +) absorption by roots strongly acidifies the rhizosphere, whereas absorption of nitrate (NO3 -) slightly alkalinizes it. The rhizosphere effects on soil acidity and plant growth in conjunction with N rate are not clearly known. To assess the impact of these multiple factors, changes in the acidity of a Typic Argiudol soil, fertilized with two N sources (urea and UAN) at two rates (equivalent to 100 and 200 kg N ha-1), were studied in a greenhouse experiment using maize as the experimental plant. Soil pH (measured in a soil-water slurry), total acidity, exchangeable acidity, and exchangeable aluminum (Al) were measured in rhizospheric and bulk soil. Plant biomass and foliar area (FA) were also measured at the V6 stage. Nitrogen fertilization significantly reduce the pH in the bulk soil by 0.3 and 0.5 units for low and high rates respectively. Changes in the rhizosphere (the "rhizospheric effect") resulted in a significant increase in soil pH, from 5.9 to 6.2. The rhizospheric effect x N source interaction significantly increased exchangeable acidity in the rhizosphere relative to bulk soil, particularly when UAN was added at a low rate. Only total acidity was significantly increased by the fertilizer application rate. In spite of the bulk soil acidification, no significant differences in exchangeable aluminum were detected. Aerial biomass and FA were significantly increased by the higher N rate, but N source had no effect on them. Although changes in acidity were observed, root biomass was not significantly affected.
publishDate 2008
dc.date.none.fl_str_mv 2008-10
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
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://hdl.handle.net/11336/163834
Rodriguez, M. B.; Godeas, Alicia Margarita; Lavado, Raul Silvio; Soil acidity changes in bulk soil and maize rhizosphere in response to nitrogen fertilization; Taylor & Francis; Communications in Soil Science and Plant Analysis; 39; 17-18; 10-2008; 2597-2607
0010-3624
CONICET Digital
CONICET
url http://hdl.handle.net/11336/163834
identifier_str_mv Rodriguez, M. B.; Godeas, Alicia Margarita; Lavado, Raul Silvio; Soil acidity changes in bulk soil and maize rhizosphere in response to nitrogen fertilization; Taylor & Francis; Communications in Soil Science and Plant Analysis; 39; 17-18; 10-2008; 2597-2607
0010-3624
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://www.tandfonline.com/doi/abs/10.1080/00103620802358656
info:eu-repo/semantics/altIdentifier/doi/10.1080/00103620802358656
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
application/pdf
application/pdf
dc.publisher.none.fl_str_mv Taylor & Francis
publisher.none.fl_str_mv Taylor & Francis
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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