Mineralização de resíduos orgânicos no solo em condição de campo
Autor(a) principal: | |
---|---|
Data de Publicação: | 2012 |
Tipo de documento: | Tese |
Idioma: | por |
Título da fonte: | LOCUS Repositório Institucional da UFV |
Texto Completo: | http://locus.ufv.br/handle/123456789/724 |
Resumo: | The decomposition and mineralization of organic carbon and nitrogen from manure of cattle, laying hens and pigs, and urban waste compost and sewage sludge, were monitored in field conditions, when these residues were incorporated or applied superficially in Red-Yellow Latosol (LVAd) in the city of St. John the Evangelist - MG. For this, the residues were incubated for 360 days, during which samples were taken for analysis of oxidizable organic carbon (COfo) and total nitrogen (NT), organic (NO), ammonium and nitrate. When incorporated into the soil mineralization rates of COfo estimated, using the first-order exponential equation set (TmCOfoEst) ranged from 24,0 to 120,5%. The constants of decomposition of COfo (kc) of varied residues incorporated 0,000354 d-1 (0,129 year-1) to 0,000708 d-1 (0,258 year-1). The constants of decomposition of COfo (kc) applied superficially to the waste receiver soil ranged from 0,000866 d-1 (0,316 year-1) to 0,002696 d-1 (0,984 year-1), however, to form surface application of the waste and under the conditions of this work, the calculation method TmCOfoEst was not suitable in view unrealistic values that were obtained. Mineralization rates calculated using the parameters of the exponential equations of first order (TmCOfo(L)), showed a variation from 20,3 to 60,1% and were more consistent considering the condition of the surface application of waste. Receptor incorporated in the soil, the rate of mineralization COfo waste, calculated by taking the initial oxidizable organic carbon (CO(i)) as reference (TmCOfo(i)), varied from 34,0 to 92,7% and when wastes were applied at the soil surface, the TmCOfo(i) ranged from 55,1 to 100,0%. When added to soil mineralization rates of NO estimated, using the exponential equations of first order set (TmNOEst) ranged from 13,2 to 60,2%. The constant average accumulation of nitrogen (kN) of the residues incorporated ranged from 0,000179 d-1 (0,065 year-1) 0,000975 d-1 (0,356 year-1). When applied superficially to the ground TmNOEst ranged from 18,6 to 64,6%. The constant average accumulation of nitrogen (kN) of waste disposed on the surface ranged from 0,000085 d-1 (0,031 year-1) to 0,002688 d-1 (0,981 year-1). When incorporated into the soil, mineralization rates of NO waste, calculated by taking the initial organic nitrogen (NO(i)) as a reference, TmNO(i) ranged from 40,7 to 72,5%, and when residues were applied on the surface of the soil, TmNO(i) ranged from 51,3 to 70,4%. Regardless of the forms of calculation and application of waste, only 13,2% TmNOEst, when the incorporation of sewage sludge, was below the 20% recommended in Resolution Nº 375/2006 of CONAMA. Other mineralization rates found were higher than the NO mineralization rate established minimum in CONAMA Resolution Nº 375/2006 to LE digested anaerobically. Variations in rates of mineralization and NO COfo, the constant of decomposition of COfo (kc) and the constant accumulation of nitrogen (kN) were associated with the application form of the residue in the soil (as incorporated or surface) and the form of sampling performed. |
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Paula, José Roberto dehttp://lattes.cnpq.br/1636858217220737Neves, Júlio César Limahttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4783076D4Costa, Claudionor Camilo dahttp://lattes.cnpq.br/8131095850505657Matos, Antonio Teixeira dehttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4783529H2Magalhães, Marcos Alves dehttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4770499E6Azevedo, Mônica de Abreuhttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4782410Z5Monaco, Paola Alfonsa Vieira Lohttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4705673E3Andrade, Cristiano Alberto dehttp://lattes.cnpq.br/22700009543271552015-03-26T12:31:23Z2013-09-162015-03-26T12:31:23Z2012-06-19PAULA, José Roberto de. Mineralization of organic residues in soil under field conditions. 2012. 111 f. Tese (Doutorado em Construções rurais e ambiência; Energia na agricultura; Mecanização agrícola; Processamento de produ) - Universidade Federal de Viçosa, Viçosa, 2012.http://locus.ufv.br/handle/123456789/724The decomposition and mineralization of organic carbon and nitrogen from manure of cattle, laying hens and pigs, and urban waste compost and sewage sludge, were monitored in field conditions, when these residues were incorporated or applied superficially in Red-Yellow Latosol (LVAd) in the city of St. John the Evangelist - MG. For this, the residues were incubated for 360 days, during which samples were taken for analysis of oxidizable organic carbon (COfo) and total nitrogen (NT), organic (NO), ammonium and nitrate. When incorporated into the soil mineralization rates of COfo estimated, using the first-order exponential equation set (TmCOfoEst) ranged from 24,0 to 120,5%. The constants of decomposition of COfo (kc) of varied residues incorporated 0,000354 d-1 (0,129 year-1) to 0,000708 d-1 (0,258 year-1). The constants of decomposition of COfo (kc) applied superficially to the waste receiver soil ranged from 0,000866 d-1 (0,316 year-1) to 0,002696 d-1 (0,984 year-1), however, to form surface application of the waste and under the conditions of this work, the calculation method TmCOfoEst was not suitable in view unrealistic values that were obtained. Mineralization rates calculated using the parameters of the exponential equations of first order (TmCOfo(L)), showed a variation from 20,3 to 60,1% and were more consistent considering the condition of the surface application of waste. Receptor incorporated in the soil, the rate of mineralization COfo waste, calculated by taking the initial oxidizable organic carbon (CO(i)) as reference (TmCOfo(i)), varied from 34,0 to 92,7% and when wastes were applied at the soil surface, the TmCOfo(i) ranged from 55,1 to 100,0%. When added to soil mineralization rates of NO estimated, using the exponential equations of first order set (TmNOEst) ranged from 13,2 to 60,2%. The constant average accumulation of nitrogen (kN) of the residues incorporated ranged from 0,000179 d-1 (0,065 year-1) 0,000975 d-1 (0,356 year-1). When applied superficially to the ground TmNOEst ranged from 18,6 to 64,6%. The constant average accumulation of nitrogen (kN) of waste disposed on the surface ranged from 0,000085 d-1 (0,031 year-1) to 0,002688 d-1 (0,981 year-1). When incorporated into the soil, mineralization rates of NO waste, calculated by taking the initial organic nitrogen (NO(i)) as a reference, TmNO(i) ranged from 40,7 to 72,5%, and when residues were applied on the surface of the soil, TmNO(i) ranged from 51,3 to 70,4%. Regardless of the forms of calculation and application of waste, only 13,2% TmNOEst, when the incorporation of sewage sludge, was below the 20% recommended in Resolution Nº 375/2006 of CONAMA. Other mineralization rates found were higher than the NO mineralization rate established minimum in CONAMA Resolution Nº 375/2006 to LE digested anaerobically. Variations in rates of mineralization and NO COfo, the constant of decomposition of COfo (kc) and the constant accumulation of nitrogen (kN) were associated with the application form of the residue in the soil (as incorporated or surface) and the form of sampling performed.A decomposição e mineralização de formas orgânicas de carbono e de nitrogênio de estercos de bovinos, de galinhas poedeiras e de suínos, além de composto de lixo urbano e lodo de esgoto, foram monitoradas, em condição de campo, quando esses resíduos foram incorporados ou aplicados superficialmente em Latossolo Vermelho-Amarelo distrófico (LVAd) do município de São João Evangelista, MG. Para isso, os referidos resíduos foram incubados durante 360 dias, período em que foram retiradas amostras para análise de carbono orgânico facilmente oxidável (COfo) e nitrogênio total (NT), orgânico (NO), amoniacal e nítrico. Quando incorporados ao solo, as taxas de mineralização de COfo estimadas, utilizando-se as equações exponenciais de primeira ordem ajustadas (TmCOfoEst), variaram de 24,0 a 120,5%. As constantes de decomposição do COfo (kc) dos resíduos incorporados variaram de 0,000354 d-1 (0,129 ano-1) a 0,000708 d-1 (0,258 ano-1). As constantes de decomposição do COfo (kc) dos resíduos aplicados superficialmente ao solo receptor variaram de 0,000866 d-1 (0,316 ano-1) a 0,002696 d-1 (0,984 ano-1). No entanto, para a forma de aplicação superficial dos resíduos e nas condições deste trabalho, o método de cálculo de TmCOfoEst não se mostrou adequado, tendo em vista que foram obtidos valores irreais. As taxas de mineralização calculadas utilizando-se parâmetros das equações exponenciais de primeira ordem (TmCOfo(L)) apresentaram variação de 20,3 a 60,1% e foram mais coerentes considerando a condição de aplicação superficial dos resíduos. Incorporados ao solo receptor, as taxas de mineralização do COfo dos resíduos, calculadas tomando-se o carbono orgânico facilmente oxidável inicial (COfo(i)) como referencial (TmCOfo(i)), variaram de 34,0 a 92,7% e, quando os resíduos foram aplicados na superfície dos solos, as TmCOfo(i) variaram de 55,1 a 100,0%. Quando incorporados ao solo, as taxas de mineralização de NO estimadas, utilizando-se as equações exponenciais de primeira ordem ajustadas (TmNOEst), variaram de 13,2 a 60,2%. As constantes médias de acúmulo de nitrogênio (kN) dos resíduos incorporados variaram de 0,000179 d-1 (0,065 ano-1) a 0,000975 d-1 (0,356 ano-1). Quando dispostos superficialmente ao solo, as TmNOEst variaram de 18,6 a 64,6%. As constantes médias de acúmulo de nitrogênio (kN) dos resíduos dispostos superficialmente variaram de 0,000085 d-1 (0,031 ano-1) a 0,002688 d-1 (0,981 ano-1). Quando incorporados ao solo, as taxas de mineralização do NO dos resíduos, calculadas tomando-se o nitrogênio orgânico inicial (NO(i)) como referencial, ou seja, TmNO(i), variaram de 40,7 a 72,5% e, quando os resíduos foram aplicados na superfície dos solos, as TmNO(i) variaram de 51,3 a 70,4%. Independentemente das formas de cálculo e de aplicação dos resíduos, somente a TmNOEst de 13,2%, quando da incorporação do LE, foi inferior aos 20%, preconizados na Resolução Nº 375/2006 do CONAMA. As demais taxas de mineralização de NO encontradas foram superiores à fração de mineralização mínima estabelecida na Resolução CONAMA Nº 375/2006, para LE digerido anaerobicamente. Alterações nas taxas de mineralização de COfo e NO, nas constantes de decomposição do COfo (kc) e nas constantes de acúmulo de nitrogênio (kN) estiveram associadas à forma de aplicação do resíduo no solo (forma incorporada ou superficial) e à forma de amostragem efetuada.Coordenação de Aperfeiçoamento de Pessoal de Nível Superiorapplication/pdfporUniversidade Federal de ViçosaDoutorado em Engenharia AgrícolaUFVBRConstruções rurais e ambiência; Energia na agricultura; Mecanização agrícola; Processamento de produRecursos hídricosResíduos orgânicosWater resourcesOrganic WasteCNPQ::CIENCIAS AGRARIAS::ENGENHARIA AGRICOLAMineralização de resíduos orgânicos no solo em condição de campoMineralização de resíduos orgânicos no solo em condição de campoMineralization of organic residues in soil under field conditionsMineralization of organic residues in soil under field conditionsinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/doctoralThesisinfo:eu-repo/semantics/openAccessreponame:LOCUS Repositório Institucional da UFVinstname:Universidade Federal de Viçosa (UFV)instacron:UFVORIGINALtexto completo.pdfapplication/pdf1921321https://locus.ufv.br//bitstream/123456789/724/1/texto%20completo.pdf3801107c545ad32523ca313fdbbf6b9fMD51TEXTtexto completo.pdf.txttexto completo.pdf.txtExtracted texttext/plain174198https://locus.ufv.br//bitstream/123456789/724/2/texto%20completo.pdf.txtc7a9b0e52dc8c3fc2f812f8cf2c16fd5MD52THUMBNAILtexto completo.pdf.jpgtexto completo.pdf.jpgIM Thumbnailimage/jpeg3534https://locus.ufv.br//bitstream/123456789/724/3/texto%20completo.pdf.jpg227291445171001c82e536ac35acf4b4MD53123456789/7242016-04-06 23:13:32.149oai:locus.ufv.br:123456789/724Repositório InstitucionalPUBhttps://www.locus.ufv.br/oai/requestfabiojreis@ufv.bropendoar:21452016-04-07T02:13:32LOCUS Repositório Institucional da UFV - Universidade Federal de Viçosa (UFV)false |
dc.title.por.fl_str_mv |
Mineralização de resíduos orgânicos no solo em condição de campo Mineralização de resíduos orgânicos no solo em condição de campo |
dc.title.alternative.eng.fl_str_mv |
Mineralization of organic residues in soil under field conditions Mineralization of organic residues in soil under field conditions |
title |
Mineralização de resíduos orgânicos no solo em condição de campo |
spellingShingle |
Mineralização de resíduos orgânicos no solo em condição de campo Paula, José Roberto de Recursos hídricos Resíduos orgânicos Water resources Organic Waste CNPQ::CIENCIAS AGRARIAS::ENGENHARIA AGRICOLA |
title_short |
Mineralização de resíduos orgânicos no solo em condição de campo |
title_full |
Mineralização de resíduos orgânicos no solo em condição de campo |
title_fullStr |
Mineralização de resíduos orgânicos no solo em condição de campo |
title_full_unstemmed |
Mineralização de resíduos orgânicos no solo em condição de campo |
title_sort |
Mineralização de resíduos orgânicos no solo em condição de campo |
author |
Paula, José Roberto de |
author_facet |
Paula, José Roberto de |
author_role |
author |
dc.contributor.authorLattes.por.fl_str_mv |
http://lattes.cnpq.br/1636858217220737 |
dc.contributor.author.fl_str_mv |
Paula, José Roberto de |
dc.contributor.advisor-co1.fl_str_mv |
Neves, Júlio César Lima |
dc.contributor.advisor-co1Lattes.fl_str_mv |
http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4783076D4 |
dc.contributor.advisor-co2.fl_str_mv |
Costa, Claudionor Camilo da |
dc.contributor.advisor-co2Lattes.fl_str_mv |
http://lattes.cnpq.br/8131095850505657 |
dc.contributor.advisor1.fl_str_mv |
Matos, Antonio Teixeira de |
dc.contributor.advisor1Lattes.fl_str_mv |
http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4783529H2 |
dc.contributor.referee1.fl_str_mv |
Magalhães, Marcos Alves de |
dc.contributor.referee1Lattes.fl_str_mv |
http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4770499E6 |
dc.contributor.referee2.fl_str_mv |
Azevedo, Mônica de Abreu |
dc.contributor.referee2Lattes.fl_str_mv |
http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4782410Z5 |
dc.contributor.referee3.fl_str_mv |
Monaco, Paola Alfonsa Vieira Lo |
dc.contributor.referee3Lattes.fl_str_mv |
http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4705673E3 |
dc.contributor.referee4.fl_str_mv |
Andrade, Cristiano Alberto de |
dc.contributor.referee4Lattes.fl_str_mv |
http://lattes.cnpq.br/2270000954327155 |
contributor_str_mv |
Neves, Júlio César Lima Costa, Claudionor Camilo da Matos, Antonio Teixeira de Magalhães, Marcos Alves de Azevedo, Mônica de Abreu Monaco, Paola Alfonsa Vieira Lo Andrade, Cristiano Alberto de |
dc.subject.por.fl_str_mv |
Recursos hídricos Resíduos orgânicos |
topic |
Recursos hídricos Resíduos orgânicos Water resources Organic Waste CNPQ::CIENCIAS AGRARIAS::ENGENHARIA AGRICOLA |
dc.subject.eng.fl_str_mv |
Water resources Organic Waste |
dc.subject.cnpq.fl_str_mv |
CNPQ::CIENCIAS AGRARIAS::ENGENHARIA AGRICOLA |
description |
The decomposition and mineralization of organic carbon and nitrogen from manure of cattle, laying hens and pigs, and urban waste compost and sewage sludge, were monitored in field conditions, when these residues were incorporated or applied superficially in Red-Yellow Latosol (LVAd) in the city of St. John the Evangelist - MG. For this, the residues were incubated for 360 days, during which samples were taken for analysis of oxidizable organic carbon (COfo) and total nitrogen (NT), organic (NO), ammonium and nitrate. When incorporated into the soil mineralization rates of COfo estimated, using the first-order exponential equation set (TmCOfoEst) ranged from 24,0 to 120,5%. The constants of decomposition of COfo (kc) of varied residues incorporated 0,000354 d-1 (0,129 year-1) to 0,000708 d-1 (0,258 year-1). The constants of decomposition of COfo (kc) applied superficially to the waste receiver soil ranged from 0,000866 d-1 (0,316 year-1) to 0,002696 d-1 (0,984 year-1), however, to form surface application of the waste and under the conditions of this work, the calculation method TmCOfoEst was not suitable in view unrealistic values that were obtained. Mineralization rates calculated using the parameters of the exponential equations of first order (TmCOfo(L)), showed a variation from 20,3 to 60,1% and were more consistent considering the condition of the surface application of waste. Receptor incorporated in the soil, the rate of mineralization COfo waste, calculated by taking the initial oxidizable organic carbon (CO(i)) as reference (TmCOfo(i)), varied from 34,0 to 92,7% and when wastes were applied at the soil surface, the TmCOfo(i) ranged from 55,1 to 100,0%. When added to soil mineralization rates of NO estimated, using the exponential equations of first order set (TmNOEst) ranged from 13,2 to 60,2%. The constant average accumulation of nitrogen (kN) of the residues incorporated ranged from 0,000179 d-1 (0,065 year-1) 0,000975 d-1 (0,356 year-1). When applied superficially to the ground TmNOEst ranged from 18,6 to 64,6%. The constant average accumulation of nitrogen (kN) of waste disposed on the surface ranged from 0,000085 d-1 (0,031 year-1) to 0,002688 d-1 (0,981 year-1). When incorporated into the soil, mineralization rates of NO waste, calculated by taking the initial organic nitrogen (NO(i)) as a reference, TmNO(i) ranged from 40,7 to 72,5%, and when residues were applied on the surface of the soil, TmNO(i) ranged from 51,3 to 70,4%. Regardless of the forms of calculation and application of waste, only 13,2% TmNOEst, when the incorporation of sewage sludge, was below the 20% recommended in Resolution Nº 375/2006 of CONAMA. Other mineralization rates found were higher than the NO mineralization rate established minimum in CONAMA Resolution Nº 375/2006 to LE digested anaerobically. Variations in rates of mineralization and NO COfo, the constant of decomposition of COfo (kc) and the constant accumulation of nitrogen (kN) were associated with the application form of the residue in the soil (as incorporated or surface) and the form of sampling performed. |
publishDate |
2012 |
dc.date.issued.fl_str_mv |
2012-06-19 |
dc.date.available.fl_str_mv |
2013-09-16 2015-03-26T12:31:23Z |
dc.date.accessioned.fl_str_mv |
2015-03-26T12:31:23Z |
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.citation.fl_str_mv |
PAULA, José Roberto de. Mineralization of organic residues in soil under field conditions. 2012. 111 f. Tese (Doutorado em Construções rurais e ambiência; Energia na agricultura; Mecanização agrícola; Processamento de produ) - Universidade Federal de Viçosa, Viçosa, 2012. |
dc.identifier.uri.fl_str_mv |
http://locus.ufv.br/handle/123456789/724 |
identifier_str_mv |
PAULA, José Roberto de. Mineralization of organic residues in soil under field conditions. 2012. 111 f. Tese (Doutorado em Construções rurais e ambiência; Energia na agricultura; Mecanização agrícola; Processamento de produ) - Universidade Federal de Viçosa, Viçosa, 2012. |
url |
http://locus.ufv.br/handle/123456789/724 |
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por |
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por |
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Universidade Federal de Viçosa |
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Doutorado em Engenharia Agrícola |
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UFV |
dc.publisher.country.fl_str_mv |
BR |
dc.publisher.department.fl_str_mv |
Construções rurais e ambiência; Energia na agricultura; Mecanização agrícola; Processamento de produ |
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Universidade Federal de Viçosa |
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