Effect of mineral nitrogen on transfer of 13C-Carbon from Eucalyptus harvest residue components to soil organic matter fractions

Detalhes bibliográficos
Autor(a) principal: Demolinari, Michelle de Sales Moreira
Data de Publicação: 2017
Outros Autores: Sousa, Rodrigo Nogueira de, Silva, Ivo Ribeiro da, Teixeira, Rafael da Silva, Neves, Júlio César Lima, Mendes, Gilberto de Oliveira
Tipo de documento: Artigo
Idioma: eng
Título da fonte: LOCUS Repositório Institucional da UFV
Texto Completo: http://dx.doi.org/10.1590/18069657rbcs20160203
http://www.locus.ufv.br/handle/123456789/14453
Resumo: The amount of harvest residues retained in Eucalyptus plantations strongly influences soil organic matter (SOM), but the efficiency of conversion to SOM may vary according to the type of residue. This study evaluated the recovery of C from Eucalyptus residue components - leaves, bark, branches, roots, and a mix of all residues - in different SOM fractions with or without mineral-N supplementation (200 mg kg-1 of N). Variation in natural 13C abundance was used to trace the destination of residue-derived C in the soil. The C content of the light fraction (LF) and heavy fraction (HF) of SOM increased over a 240-days decomposition period in response to incorporation of Eucalyptus residues in the soil. Bark and leaf residues showed the best results. Bark residues increased the C content of the HF by 45 % over the initial condition. Leaf residues made the largest contribution to LF-C, increasing it by 8.6 times. Leaf residues also led to the highest N contents in the LF and HF, whereas branches, roots, and the mixture of residues caused significant net transfers of N from the HF. Mineral-N supplementation had no effect on stabilization of organic C in the HF of SOM, in which the C could be maintained for longer periods due to physical/colloidal protection against microbial decomposition. These results highlight the importance of keeping Eucalyptus harvest residues in the planted area, especially the bark, which is the most abundant harvest residue component under field conditions, for maintenance of SOM.
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spelling Demolinari, Michelle de Sales MoreiraSousa, Rodrigo Nogueira deSilva, Ivo Ribeiro daTeixeira, Rafael da SilvaNeves, Júlio César LimaMendes, Gilberto de Oliveira2017-12-06T13:22:47Z2017-12-06T13:22:47Z2017-07-311806-9657http://dx.doi.org/10.1590/18069657rbcs20160203http://www.locus.ufv.br/handle/123456789/14453The amount of harvest residues retained in Eucalyptus plantations strongly influences soil organic matter (SOM), but the efficiency of conversion to SOM may vary according to the type of residue. This study evaluated the recovery of C from Eucalyptus residue components - leaves, bark, branches, roots, and a mix of all residues - in different SOM fractions with or without mineral-N supplementation (200 mg kg-1 of N). Variation in natural 13C abundance was used to trace the destination of residue-derived C in the soil. The C content of the light fraction (LF) and heavy fraction (HF) of SOM increased over a 240-days decomposition period in response to incorporation of Eucalyptus residues in the soil. Bark and leaf residues showed the best results. Bark residues increased the C content of the HF by 45 % over the initial condition. Leaf residues made the largest contribution to LF-C, increasing it by 8.6 times. Leaf residues also led to the highest N contents in the LF and HF, whereas branches, roots, and the mixture of residues caused significant net transfers of N from the HF. Mineral-N supplementation had no effect on stabilization of organic C in the HF of SOM, in which the C could be maintained for longer periods due to physical/colloidal protection against microbial decomposition. These results highlight the importance of keeping Eucalyptus harvest residues in the planted area, especially the bark, which is the most abundant harvest residue component under field conditions, for maintenance of SOM.engRevista Brasileira de Ciência do Solo41, e0160203, July 2017C cyclingN cyclingSOMStable isotopesEffect of mineral nitrogen on transfer of 13C-Carbon from Eucalyptus harvest residue components to soil organic matter fractionsinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfinfo:eu-repo/semantics/openAccessreponame:LOCUS Repositório Institucional da UFVinstname:Universidade Federal de Viçosa (UFV)instacron:UFVORIGINAL0100-0683-rbcs-18069657rbcs20160203.pdf0100-0683-rbcs-18069657rbcs20160203.pdftexto completoapplication/pdf469131https://locus.ufv.br//bitstream/123456789/14453/1/0100-0683-rbcs-18069657rbcs20160203.pdf80f9bb876526cea268ffe9f84fdc36ffMD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81748https://locus.ufv.br//bitstream/123456789/14453/2/license.txt8a4605be74aa9ea9d79846c1fba20a33MD52THUMBNAIL0100-0683-rbcs-18069657rbcs20160203.pdf.jpg0100-0683-rbcs-18069657rbcs20160203.pdf.jpgIM Thumbnailimage/jpeg4641https://locus.ufv.br//bitstream/123456789/14453/3/0100-0683-rbcs-18069657rbcs20160203.pdf.jpg7db2dc730b221b4a3aced0b1fd1ec5ddMD53123456789/144532017-12-06 22:00:48.495oai:locus.ufv.br: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Repositório InstitucionalPUBhttps://www.locus.ufv.br/oai/requestfabiojreis@ufv.bropendoar:21452017-12-07T01:00:48LOCUS Repositório Institucional da UFV - Universidade Federal de Viçosa (UFV)false
dc.title.en.fl_str_mv Effect of mineral nitrogen on transfer of 13C-Carbon from Eucalyptus harvest residue components to soil organic matter fractions
title Effect of mineral nitrogen on transfer of 13C-Carbon from Eucalyptus harvest residue components to soil organic matter fractions
spellingShingle Effect of mineral nitrogen on transfer of 13C-Carbon from Eucalyptus harvest residue components to soil organic matter fractions
Demolinari, Michelle de Sales Moreira
C cycling
N cycling
SOM
Stable isotopes
title_short Effect of mineral nitrogen on transfer of 13C-Carbon from Eucalyptus harvest residue components to soil organic matter fractions
title_full Effect of mineral nitrogen on transfer of 13C-Carbon from Eucalyptus harvest residue components to soil organic matter fractions
title_fullStr Effect of mineral nitrogen on transfer of 13C-Carbon from Eucalyptus harvest residue components to soil organic matter fractions
title_full_unstemmed Effect of mineral nitrogen on transfer of 13C-Carbon from Eucalyptus harvest residue components to soil organic matter fractions
title_sort Effect of mineral nitrogen on transfer of 13C-Carbon from Eucalyptus harvest residue components to soil organic matter fractions
author Demolinari, Michelle de Sales Moreira
author_facet Demolinari, Michelle de Sales Moreira
Sousa, Rodrigo Nogueira de
Silva, Ivo Ribeiro da
Teixeira, Rafael da Silva
Neves, Júlio César Lima
Mendes, Gilberto de Oliveira
author_role author
author2 Sousa, Rodrigo Nogueira de
Silva, Ivo Ribeiro da
Teixeira, Rafael da Silva
Neves, Júlio César Lima
Mendes, Gilberto de Oliveira
author2_role author
author
author
author
author
dc.contributor.author.fl_str_mv Demolinari, Michelle de Sales Moreira
Sousa, Rodrigo Nogueira de
Silva, Ivo Ribeiro da
Teixeira, Rafael da Silva
Neves, Júlio César Lima
Mendes, Gilberto de Oliveira
dc.subject.pt-BR.fl_str_mv C cycling
N cycling
SOM
Stable isotopes
topic C cycling
N cycling
SOM
Stable isotopes
description The amount of harvest residues retained in Eucalyptus plantations strongly influences soil organic matter (SOM), but the efficiency of conversion to SOM may vary according to the type of residue. This study evaluated the recovery of C from Eucalyptus residue components - leaves, bark, branches, roots, and a mix of all residues - in different SOM fractions with or without mineral-N supplementation (200 mg kg-1 of N). Variation in natural 13C abundance was used to trace the destination of residue-derived C in the soil. The C content of the light fraction (LF) and heavy fraction (HF) of SOM increased over a 240-days decomposition period in response to incorporation of Eucalyptus residues in the soil. Bark and leaf residues showed the best results. Bark residues increased the C content of the HF by 45 % over the initial condition. Leaf residues made the largest contribution to LF-C, increasing it by 8.6 times. Leaf residues also led to the highest N contents in the LF and HF, whereas branches, roots, and the mixture of residues caused significant net transfers of N from the HF. Mineral-N supplementation had no effect on stabilization of organic C in the HF of SOM, in which the C could be maintained for longer periods due to physical/colloidal protection against microbial decomposition. These results highlight the importance of keeping Eucalyptus harvest residues in the planted area, especially the bark, which is the most abundant harvest residue component under field conditions, for maintenance of SOM.
publishDate 2017
dc.date.accessioned.fl_str_mv 2017-12-06T13:22:47Z
dc.date.available.fl_str_mv 2017-12-06T13:22:47Z
dc.date.issued.fl_str_mv 2017-07-31
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
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dc.identifier.uri.fl_str_mv http://dx.doi.org/10.1590/18069657rbcs20160203
http://www.locus.ufv.br/handle/123456789/14453
dc.identifier.issn.none.fl_str_mv 1806-9657
identifier_str_mv 1806-9657
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dc.language.iso.fl_str_mv eng
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dc.relation.ispartofseries.pt-BR.fl_str_mv 41, e0160203, July 2017
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