Effect of mineral nitrogen on transfer of 13C-Carbon from Eucalyptus harvest residue components to soil organic matter fractions
Autor(a) principal: | |
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Data de Publicação: | 2017 |
Outros Autores: | , , , , |
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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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 |
format |
article |
status_str |
publishedVersion |
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 |
url |
http://dx.doi.org/10.1590/18069657rbcs20160203 http://www.locus.ufv.br/handle/123456789/14453 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.ispartofseries.pt-BR.fl_str_mv |
41, e0160203, July 2017 |
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info:eu-repo/semantics/openAccess |
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openAccess |
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Revista Brasileira de Ciência do Solo |
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Revista Brasileira de Ciência do Solo |
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