Distribution and vertical stratification of carbon and nitrogen in soil under different managements in the pampean region of Argentina

One of the expected benefits of no-tillage systems is a higher rate of soil C sequestration. However, higher C retention in soil is not always apparent when no-tillage is applied, due e.g., to substantial differences in soil type and initial C content. The main purpose of this study was to evaluate the potential of no-tillage management to increase the stock of total organic C in soils of the Pampas region in Argentina. Forty crop fields under no-tillage and conventional tillage systems and seven undisturbed soils were sampled. Total organic C, total N, their fractions and stratification ratios and the C storage capacity of the soils under different managements were assessed in samples to a depth of 30 cm, in three layers (0-5, 5-15 and 15-30 cm). The differences between the C pools of the undisturbed and cultivated soils were significant (p < 0.05) and most pronounced in the top (0-5 cm) soil layer, with more active C near the soil surface (undisturbed &gt; no-tillage &gt; conventional tillage). Based on the stratification ratio of the labile C pool (0-5/5-15 cm), the untilled were separated from conventionally tilled areas. Much of the variation in potentially mineralizable C was explained by this active C fraction (R² = 0.61) and by total organic C (R² = 0.67). No-till soils did not accumulate more organic C than conventionally tilled soils in the 0-30 cm layer, but there was substantial stratification of total and active C pools at no till sites. If the C stratification ratio is really an indicator of soil quality, then the C storage potential of no-tillage would be greater than in conventional tillage, at least in the surface layers. Particulate organic C and potentially mineralizable C may be useful to evaluate variations in topsoil organic matter.

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Main Authors: Álvarez,Carina Rosa, Costantini,Alejandro Oscar, Bono,Alfredo, Taboada,Miguel Ángel, Boem,Flavio Hernán Gutiérrez, Fernández,Patricia Lilia, Prystupa,Pablo
Format: Digital revista
Language:English
Published: Sociedade Brasileira de Ciência do Solo 2011
Online Access:http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832011000600015
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spelling oai:scielo:S0100-068320110006000152012-02-10Distribution and vertical stratification of carbon and nitrogen in soil under different managements in the pampean region of ArgentinaÁlvarez,Carina RosaCostantini,Alejandro OscarBono,AlfredoTaboada,Miguel ÁngelBoem,Flavio Hernán GutiérrezFernández,Patricia LiliaPrystupa,Pablo no-tillage soil organic matter fractions tillage systems carbon stratification C and N stocks One of the expected benefits of no-tillage systems is a higher rate of soil C sequestration. However, higher C retention in soil is not always apparent when no-tillage is applied, due e.g., to substantial differences in soil type and initial C content. The main purpose of this study was to evaluate the potential of no-tillage management to increase the stock of total organic C in soils of the Pampas region in Argentina. Forty crop fields under no-tillage and conventional tillage systems and seven undisturbed soils were sampled. Total organic C, total N, their fractions and stratification ratios and the C storage capacity of the soils under different managements were assessed in samples to a depth of 30 cm, in three layers (0-5, 5-15 and 15-30 cm). The differences between the C pools of the undisturbed and cultivated soils were significant (p < 0.05) and most pronounced in the top (0-5 cm) soil layer, with more active C near the soil surface (undisturbed &gt; no-tillage &gt; conventional tillage). Based on the stratification ratio of the labile C pool (0-5/5-15 cm), the untilled were separated from conventionally tilled areas. Much of the variation in potentially mineralizable C was explained by this active C fraction (R² = 0.61) and by total organic C (R² = 0.67). No-till soils did not accumulate more organic C than conventionally tilled soils in the 0-30 cm layer, but there was substantial stratification of total and active C pools at no till sites. If the C stratification ratio is really an indicator of soil quality, then the C storage potential of no-tillage would be greater than in conventional tillage, at least in the surface layers. Particulate organic C and potentially mineralizable C may be useful to evaluate variations in topsoil organic matter.info:eu-repo/semantics/openAccessSociedade Brasileira de Ciência do SoloRevista Brasileira de Ciência do Solo v.35 n.6 20112011-12-01info:eu-repo/semantics/articletext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832011000600015en10.1590/S0100-06832011000600015
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countrycode BR
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databasecode rev-scielo-br
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region America del Sur
libraryname SciELO
language English
format Digital
author Álvarez,Carina Rosa
Costantini,Alejandro Oscar
Bono,Alfredo
Taboada,Miguel Ángel
Boem,Flavio Hernán Gutiérrez
Fernández,Patricia Lilia
Prystupa,Pablo
spellingShingle Álvarez,Carina Rosa
Costantini,Alejandro Oscar
Bono,Alfredo
Taboada,Miguel Ángel
Boem,Flavio Hernán Gutiérrez
Fernández,Patricia Lilia
Prystupa,Pablo
Distribution and vertical stratification of carbon and nitrogen in soil under different managements in the pampean region of Argentina
author_facet Álvarez,Carina Rosa
Costantini,Alejandro Oscar
Bono,Alfredo
Taboada,Miguel Ángel
Boem,Flavio Hernán Gutiérrez
Fernández,Patricia Lilia
Prystupa,Pablo
author_sort Álvarez,Carina Rosa
title Distribution and vertical stratification of carbon and nitrogen in soil under different managements in the pampean region of Argentina
title_short Distribution and vertical stratification of carbon and nitrogen in soil under different managements in the pampean region of Argentina
title_full Distribution and vertical stratification of carbon and nitrogen in soil under different managements in the pampean region of Argentina
title_fullStr Distribution and vertical stratification of carbon and nitrogen in soil under different managements in the pampean region of Argentina
title_full_unstemmed Distribution and vertical stratification of carbon and nitrogen in soil under different managements in the pampean region of Argentina
title_sort distribution and vertical stratification of carbon and nitrogen in soil under different managements in the pampean region of argentina
description One of the expected benefits of no-tillage systems is a higher rate of soil C sequestration. However, higher C retention in soil is not always apparent when no-tillage is applied, due e.g., to substantial differences in soil type and initial C content. The main purpose of this study was to evaluate the potential of no-tillage management to increase the stock of total organic C in soils of the Pampas region in Argentina. Forty crop fields under no-tillage and conventional tillage systems and seven undisturbed soils were sampled. Total organic C, total N, their fractions and stratification ratios and the C storage capacity of the soils under different managements were assessed in samples to a depth of 30 cm, in three layers (0-5, 5-15 and 15-30 cm). The differences between the C pools of the undisturbed and cultivated soils were significant (p < 0.05) and most pronounced in the top (0-5 cm) soil layer, with more active C near the soil surface (undisturbed &gt; no-tillage &gt; conventional tillage). Based on the stratification ratio of the labile C pool (0-5/5-15 cm), the untilled were separated from conventionally tilled areas. Much of the variation in potentially mineralizable C was explained by this active C fraction (R² = 0.61) and by total organic C (R² = 0.67). No-till soils did not accumulate more organic C than conventionally tilled soils in the 0-30 cm layer, but there was substantial stratification of total and active C pools at no till sites. If the C stratification ratio is really an indicator of soil quality, then the C storage potential of no-tillage would be greater than in conventional tillage, at least in the surface layers. Particulate organic C and potentially mineralizable C may be useful to evaluate variations in topsoil organic matter.
publisher Sociedade Brasileira de Ciência do Solo
publishDate 2011
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832011000600015
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