Produção de biomassa, composição química e decomposição de resíduos culturais da parte aérea e raízes no solo

Detalhes bibliográficos
Ano de defesa: 2014
Autor(a) principal: Redin, Marciel lattes
Orientador(a): Giacomini, Sandro José lattes
Banca de defesa: Aita, Celso lattes, Brunetto, Gustavo lattes, Schenato, Ricardo Bergamo lattes, Jantalia, Cláudia Pozzi lattes
Tipo de documento: Tese
Tipo de acesso: Acesso aberto
Idioma: por
Instituição de defesa: Universidade Federal de Santa Maria
Centro de Ciências Rurais
Programa de Pós-Graduação: Programa de Pós-Graduação em Ciência do Solo
Departamento: Agronomia
País: Brasil
Palavras-chave em Português:
Palavras-chave em Inglês:
Área do conhecimento CNPq:
Link de acesso: http://repositorio.ufsm.br/handle/1/15629
Resumo: Crop residues (CR) from shoots (S) and roots (R) of plants are the main source of carbon C (C) and nitrogen (N) for the agricultural soils. Compared to the S of plants there are few studies on the production of dry matter (DM), C and N accumulation and decomposition of R. The decomposition of CR in soil is affected in part by its chemical composition, which can be affected by family and mixture of CR. The objectives of this study were as follows: a) evaluate the dry matter production (DM), chemical composition and accumulation of C and N in DM of S and R from 27 species of annual crops five families; b) relate the chemical composition of R from 20 species of annual crops with C mineralization in soil and c) study the interactions of additivity or non-additivity of the mineralization of C and N of CR of different chemical compositions (leaves and stems) on the surface of the soil. Three studies were realized: In the first study was quantified DM, accumulation of C and N in DM, chemical composition of S (leaves and stems) and R and the other two study was evaluated under laboratory conditions for 120 days, the mineralization of C and/or N of the CR in soil. The data measured of C mineralization were adjusted with a simple exponential model. Principal components analyses (PCAs) were performed to explore the qualitative address in CR and of decomposition. The DM of R, concentrated in the 0-10 cm layer, ranged from 0.54 to 1.44 Mg ha-1 in the legumes (Fabaceae) species and from 0.53 to 2.32 Mg ha-1 in the non-legumes (mainly Poaceae), corresponding the values between 63 to 97% of the total amount of roots in the 0-20 cm layer. The R/S ratio average was below legumes compared to non-legumes (0.14 times 0.20). The legumes acumulated in R 392 kg C ha-1 and 15 kg N ha-1 and the non-legumes 642 kg C ha-1 and 16 kg N ha-1. PCAs showed that the chemical composition of the S and R differentiated plant families. Mineralization of C of R ranged widely in terms of kinetics and the total amount of C mineralized (36% to 59%). The mineralization constant (k) was negatively correlated with hemicellulose and positively with the N content in R. R of Poaceae with high content of hemicellulose, cellulose and low total N showed a low value of k and cumulative mineralization C. The S of the legumes showed high total nitrogen, soluble compounds and greater differences between the chemical composition of leaves and stems. The Poaceae were characterized by high content of hemicellulose and cellulose, little difference between leaves and stems and slow decomposition. The mixture of leaves and stems showed mainly additives effects (no effect) in the mineralization of C and N in the soil. Antagonistic effect on N mineralization was observed in most Fabaceae mixtures with high content of N and heterogeneity between leaves and stems. Species of non-legumes produce more DM and C accumulation (1.8 times), high accumulation of N in R (1.3 times) and ratio R/S (1.6 times) than legumes. The decomposition of R species of annual crops is controlled by the content of cellulose and hemicellulose. The interactions of non-additivity related to decomposition of mixed of residues of leaves and stems are controlled by the degree of heterogeneity and N availability in the mixtures.
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spelling 2019-02-13T14:42:18Z2019-02-13T14:42:18Z2014-02-27http://repositorio.ufsm.br/handle/1/15629Crop residues (CR) from shoots (S) and roots (R) of plants are the main source of carbon C (C) and nitrogen (N) for the agricultural soils. Compared to the S of plants there are few studies on the production of dry matter (DM), C and N accumulation and decomposition of R. The decomposition of CR in soil is affected in part by its chemical composition, which can be affected by family and mixture of CR. The objectives of this study were as follows: a) evaluate the dry matter production (DM), chemical composition and accumulation of C and N in DM of S and R from 27 species of annual crops five families; b) relate the chemical composition of R from 20 species of annual crops with C mineralization in soil and c) study the interactions of additivity or non-additivity of the mineralization of C and N of CR of different chemical compositions (leaves and stems) on the surface of the soil. Three studies were realized: In the first study was quantified DM, accumulation of C and N in DM, chemical composition of S (leaves and stems) and R and the other two study was evaluated under laboratory conditions for 120 days, the mineralization of C and/or N of the CR in soil. The data measured of C mineralization were adjusted with a simple exponential model. Principal components analyses (PCAs) were performed to explore the qualitative address in CR and of decomposition. The DM of R, concentrated in the 0-10 cm layer, ranged from 0.54 to 1.44 Mg ha-1 in the legumes (Fabaceae) species and from 0.53 to 2.32 Mg ha-1 in the non-legumes (mainly Poaceae), corresponding the values between 63 to 97% of the total amount of roots in the 0-20 cm layer. The R/S ratio average was below legumes compared to non-legumes (0.14 times 0.20). The legumes acumulated in R 392 kg C ha-1 and 15 kg N ha-1 and the non-legumes 642 kg C ha-1 and 16 kg N ha-1. PCAs showed that the chemical composition of the S and R differentiated plant families. Mineralization of C of R ranged widely in terms of kinetics and the total amount of C mineralized (36% to 59%). The mineralization constant (k) was negatively correlated with hemicellulose and positively with the N content in R. R of Poaceae with high content of hemicellulose, cellulose and low total N showed a low value of k and cumulative mineralization C. The S of the legumes showed high total nitrogen, soluble compounds and greater differences between the chemical composition of leaves and stems. The Poaceae were characterized by high content of hemicellulose and cellulose, little difference between leaves and stems and slow decomposition. The mixture of leaves and stems showed mainly additives effects (no effect) in the mineralization of C and N in the soil. Antagonistic effect on N mineralization was observed in most Fabaceae mixtures with high content of N and heterogeneity between leaves and stems. Species of non-legumes produce more DM and C accumulation (1.8 times), high accumulation of N in R (1.3 times) and ratio R/S (1.6 times) than legumes. The decomposition of R species of annual crops is controlled by the content of cellulose and hemicellulose. The interactions of non-additivity related to decomposition of mixed of residues of leaves and stems are controlled by the degree of heterogeneity and N availability in the mixtures.Os resíduos culturais (RC) da parte aérea (PA) e raízes (R) constituem a principal fonte de carbono (C) e nitrogênio (N) para os solos agrícolas. Comparado à PA das plantas poucos são os estudos sobre a produção de matéria seca (MS), acúmulo de C e N e decomposição das R. A decomposição de RC no solo é afetada em parte pela sua composição química, a qual pode ser afetada pela família e mistura de RC. Os objetivos do presente trabalho foram os seguintes: a) avaliar a produção de MS, composição química e acúmulo de C e N na MS da PA e de R de 27 espécies de culturas anuais de cinco famílias; b) relacionar a composição química das R de 20 espécies de culturas anuais com a mineralização do C no solo e; c) estudar as interações de aditividade ou não aditividade sobre a mineralização do C e do N de RC de diferentes composições químicas (folhas e talos) na superfície do solo. Foram realizados três estudos. No primeiro estudo foi quantificada a MS, acúmulo de C e N na MS, composição química da PA (folhas e talos) e R e nos outros dois, avaliou-se em condições de laboratório por 120 dias, a mineralização do C e/ou N dos RC no solo. Os dados medidos de mineralização do C foram ajustados com um modelo exponencial simples. Análises de componentes principais (ACPs) foram realizadas para explorar padrões qualitativos nos RC e de decomposição. A MS das R, concentradas na camada de 0-10 cm variou de 0,54 a 1,44 Mg ha-1 nas espécies de leguminosas (Fabaceae) e de 0,53 a 2,32 Mg ha-1 em não leguminosas (principalmente Poaceae), correspondendo a valores entre 63 a 97% da quantidade total de raízes da camada 0-20 cm. A relação R/PA média das leguminosas foi inferior àquela das espécies não leguminosas (0,14 vezes 0,20). As leguminosas acumularam nas R 392 kg C ha-1 e 15 kg N ha-1 e nas não leguminosas 642 kg C ha-1 e 16 kg N ha-1. ACPs mostraram que a composição química da PA e R diferenciaram as famílias de plantas. A mineralização do C das R variou muito em termos de cinética e na quantidade total de C mineralizado (36% a 59%). A constante de mineralização (k) foi negativamente correlacionada com hemicelulose e positivamente com o teor de N nas R. R de Poaceae com alto conteúdo de hemicelulose, celulose e baixo N total apresentaram baixo valor de k e mineralização cumulativa de C. A PA das leguminosas apresentaram elevado N total, compostos solúveis e grandes diferenças entre a composição química de folhas e talos. As Poaceae foram caracterizadas por elevado conteúdo de hemicelulose e celulose, pequena diferença entre folhas e talos e lenta decomposição. A mistura de folhas e talos mostrou, principalmente, efeitos aditivos (efeito nulo) na mineralização do C e N no solo. Efeito antagonista na mineralização do N foi observado na maioria das misturas de leguminosas com elevado teor de N e grande heterogeneidade entre folhas e talos. Espécies de não leguminosas produzem maior quantidade de MS e acúmulo de C (1,8 vezes), maior acúmulo de N nas R (1,3 vezes) e relação R/PA (1,6 vezes) que leguminosas. A decomposição de R das espécies de culturas anuais é controlada pelo conteúdo de celulose e hemicelulose. As interações de não aditividade relacionadas à decomposição de misturas de resíduos de folhas e talos são controladas pelo grau de heterogeneidade e disponibilidade de N nas misturas.porUniversidade Federal de Santa MariaCentro de Ciências RuraisPrograma de Pós-Graduação em Ciência do SoloUFSMBrasilAgronomiaAttribution-NonCommercial-NoDerivatives 4.0 Internationalhttp://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccessQualidade do resíduoMineralizaçãoCarbonoNitrogênioRaízesQuality residueMineralizationCarbonNitrogenRootsCNPQ::CIENCIAS AGRARIAS::AGRONOMIAProdução de biomassa, composição química e decomposição de resíduos culturais da parte aérea e raízes no soloBiomass production, chemical composition and decomposition of crop residues from shoot and roots in soilinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/doctoralThesisGiacomini, Sandro Joséhttp://lattes.cnpq.br/1112466940331009Aita, Celsohttp://lattes.cnpq.br/7391004032643110Brunetto, Gustavohttp://lattes.cnpq.br/1185169003700830Schenato, Ricardo Bergamohttp://lattes.cnpq.br/4043277579467500Jantalia, Cláudia Pozzihttp://lattes.cnpq.br/3465919209024196http://lattes.cnpq.br/7912908707815307Redin, Marciel500100000009600300419b5a2f-20df-408a-a156-d652293f4a739a55164d-4f4c-4885-8a10-39cebca294e8b46e65b9-e307-4c06-a922-2942f17e7dc547c53d70-f89e-4d53-83be-c30ab75c841ddac0aa7d-baf2-43a2-a7f9-b3405e70ff2a7998753d-f6b8-4b60-81af-6de80ae38d3freponame:Biblioteca Digital de Teses e Dissertações do UFSMinstname:Universidade Federal de Santa Maria (UFSM)instacron:UFSMCC-LICENSElicense_rdflicense_rdfapplication/rdf+xml; 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dc.title.por.fl_str_mv Produção de biomassa, composição química e decomposição de resíduos culturais da parte aérea e raízes no solo
dc.title.alternative.eng.fl_str_mv Biomass production, chemical composition and decomposition of crop residues from shoot and roots in soil
title Produção de biomassa, composição química e decomposição de resíduos culturais da parte aérea e raízes no solo
spellingShingle Produção de biomassa, composição química e decomposição de resíduos culturais da parte aérea e raízes no solo
Redin, Marciel
Qualidade do resíduo
Mineralização
Carbono
Nitrogênio
Raízes
Quality residue
Mineralization
Carbon
Nitrogen
Roots
CNPQ::CIENCIAS AGRARIAS::AGRONOMIA
title_short Produção de biomassa, composição química e decomposição de resíduos culturais da parte aérea e raízes no solo
title_full Produção de biomassa, composição química e decomposição de resíduos culturais da parte aérea e raízes no solo
title_fullStr Produção de biomassa, composição química e decomposição de resíduos culturais da parte aérea e raízes no solo
title_full_unstemmed Produção de biomassa, composição química e decomposição de resíduos culturais da parte aérea e raízes no solo
title_sort Produção de biomassa, composição química e decomposição de resíduos culturais da parte aérea e raízes no solo
author Redin, Marciel
author_facet Redin, Marciel
author_role author
dc.contributor.advisor1.fl_str_mv Giacomini, Sandro José
dc.contributor.advisor1Lattes.fl_str_mv http://lattes.cnpq.br/1112466940331009
dc.contributor.referee1.fl_str_mv Aita, Celso
dc.contributor.referee1Lattes.fl_str_mv http://lattes.cnpq.br/7391004032643110
dc.contributor.referee2.fl_str_mv Brunetto, Gustavo
dc.contributor.referee2Lattes.fl_str_mv http://lattes.cnpq.br/1185169003700830
dc.contributor.referee3.fl_str_mv Schenato, Ricardo Bergamo
dc.contributor.referee3Lattes.fl_str_mv http://lattes.cnpq.br/4043277579467500
dc.contributor.referee4.fl_str_mv Jantalia, Cláudia Pozzi
dc.contributor.referee4Lattes.fl_str_mv http://lattes.cnpq.br/3465919209024196
dc.contributor.authorLattes.fl_str_mv http://lattes.cnpq.br/7912908707815307
dc.contributor.author.fl_str_mv Redin, Marciel
contributor_str_mv Giacomini, Sandro José
Aita, Celso
Brunetto, Gustavo
Schenato, Ricardo Bergamo
Jantalia, Cláudia Pozzi
dc.subject.por.fl_str_mv Qualidade do resíduo
Mineralização
Carbono
Nitrogênio
Raízes
topic Qualidade do resíduo
Mineralização
Carbono
Nitrogênio
Raízes
Quality residue
Mineralization
Carbon
Nitrogen
Roots
CNPQ::CIENCIAS AGRARIAS::AGRONOMIA
dc.subject.eng.fl_str_mv Quality residue
Mineralization
Carbon
Nitrogen
Roots
dc.subject.cnpq.fl_str_mv CNPQ::CIENCIAS AGRARIAS::AGRONOMIA
description Crop residues (CR) from shoots (S) and roots (R) of plants are the main source of carbon C (C) and nitrogen (N) for the agricultural soils. Compared to the S of plants there are few studies on the production of dry matter (DM), C and N accumulation and decomposition of R. The decomposition of CR in soil is affected in part by its chemical composition, which can be affected by family and mixture of CR. The objectives of this study were as follows: a) evaluate the dry matter production (DM), chemical composition and accumulation of C and N in DM of S and R from 27 species of annual crops five families; b) relate the chemical composition of R from 20 species of annual crops with C mineralization in soil and c) study the interactions of additivity or non-additivity of the mineralization of C and N of CR of different chemical compositions (leaves and stems) on the surface of the soil. Three studies were realized: In the first study was quantified DM, accumulation of C and N in DM, chemical composition of S (leaves and stems) and R and the other two study was evaluated under laboratory conditions for 120 days, the mineralization of C and/or N of the CR in soil. The data measured of C mineralization were adjusted with a simple exponential model. Principal components analyses (PCAs) were performed to explore the qualitative address in CR and of decomposition. The DM of R, concentrated in the 0-10 cm layer, ranged from 0.54 to 1.44 Mg ha-1 in the legumes (Fabaceae) species and from 0.53 to 2.32 Mg ha-1 in the non-legumes (mainly Poaceae), corresponding the values between 63 to 97% of the total amount of roots in the 0-20 cm layer. The R/S ratio average was below legumes compared to non-legumes (0.14 times 0.20). The legumes acumulated in R 392 kg C ha-1 and 15 kg N ha-1 and the non-legumes 642 kg C ha-1 and 16 kg N ha-1. PCAs showed that the chemical composition of the S and R differentiated plant families. Mineralization of C of R ranged widely in terms of kinetics and the total amount of C mineralized (36% to 59%). The mineralization constant (k) was negatively correlated with hemicellulose and positively with the N content in R. R of Poaceae with high content of hemicellulose, cellulose and low total N showed a low value of k and cumulative mineralization C. The S of the legumes showed high total nitrogen, soluble compounds and greater differences between the chemical composition of leaves and stems. The Poaceae were characterized by high content of hemicellulose and cellulose, little difference between leaves and stems and slow decomposition. The mixture of leaves and stems showed mainly additives effects (no effect) in the mineralization of C and N in the soil. Antagonistic effect on N mineralization was observed in most Fabaceae mixtures with high content of N and heterogeneity between leaves and stems. Species of non-legumes produce more DM and C accumulation (1.8 times), high accumulation of N in R (1.3 times) and ratio R/S (1.6 times) than legumes. The decomposition of R species of annual crops is controlled by the content of cellulose and hemicellulose. The interactions of non-additivity related to decomposition of mixed of residues of leaves and stems are controlled by the degree of heterogeneity and N availability in the mixtures.
publishDate 2014
dc.date.issued.fl_str_mv 2014-02-27
dc.date.accessioned.fl_str_mv 2019-02-13T14:42:18Z
dc.date.available.fl_str_mv 2019-02-13T14:42:18Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/doctoralThesis
format doctoralThesis
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://repositorio.ufsm.br/handle/1/15629
url http://repositorio.ufsm.br/handle/1/15629
dc.language.iso.fl_str_mv por
language por
dc.relation.cnpq.fl_str_mv 500100000009
dc.relation.confidence.fl_str_mv 600
300
dc.relation.authority.fl_str_mv 419b5a2f-20df-408a-a156-d652293f4a73
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