QUALIDADE FÍSICA DO SOLO E LIMITES CRÍTICOS DE ATRIBUTOS FÍSICOS DE LATOSSOLO BRUNO DISTRÓFICO EM FUNÇÃO DA PRODUTIVIDADE DAS CULTURAS DE MILHO E AVEIA

Detalhes bibliográficos
Autor(a) principal: Bareta Junior, Eloi
Data de Publicação: 2018
Tipo de documento: Dissertação
Idioma: por
Título da fonte: Biblioteca Digital de Teses e Dissertações do UNICENTRO
Texto Completo: http://tede.unicentro.br:8080/jspui/handle/jspui/928
Resumo: With the upgrading of the agriculture and production of seeds and fodder, mostly under no tillage system, the use of agricultural machines and implements of great size has become more common, many times under not appropriated soil conditions, all on behalf of operating income. On that way, the excessive traffic, allied to a high soil humidity, have been upgrading the levels of soil compaction. The process of soil compaction, is related to the modification of the soil physical quality, presenting increases in soil density, decreases of macroporosity, decreases of water infiltration tax in the soil and increases the soil penetration resistance. The modification of the soil physical quality affects the root development and the crops productivities. To have technical subsidy at the decision-making to realise the mechanical intervention or the management practice change aiming decompress the soil, is necessary to know the critical levels of the soil physical attributes that are employed to determine the soil physical quality. Therefore, the objective of this work was to submit the soil to various intensities of tractor traffic to achieve different levels of soil compaction aiming to identify the critical limits of physical attributes to the maize and oat crop on a Xanthic Hapludox. The study was conducted at the experimental area of the agronomy department from Unicentro, at Guarapuava, PR. The trial design was a completely randomized blocks with six repetitions. The treatments were: The witness (without compaction), two, five and twenty passes with the agricultural tractor. The physical attributes were determined before the maize sowing and before the black oat sowing. Both crops were cultivated under no tillage system and measured their productivities. The critical limits for soil density, relative density, macroporosity and capacity of total aeration were determined for the maize and oat crops. The soil compaction caused by the tractor traffic caused change of the soil density, relative density, macroporosity, microporosity, field capacity, capacity of total aeration, water infiltration tax in the soil and soil resistance of penetration. Among the parameters associated to the crops, fodder and seed productivities of maize and dry matter of oat held higher effect of compaction, entailing on lower productivities on both crops. The depth sampled that best represented adjusted to determine the critical limits of the physical attributes from the soil was at 0,07 to 0,12 m. At this depth, for the maize crop, the ideal range of soil density was at the range from 0,93 to 1,07 Mg m-3 , for relative density the ideal range was from 76,9 to 90,4%, for macroporosity the ideal range was from 0,12 to 0,21 m3 m-3 and for the attribute capacity of total aeration the ideal values are on the range from 0,14 to 0,24 m3 m-3. The oat crop showed productivity limitation when the values of soil density were lower than 1,03 Mg m-3 , relative density lower than 85,7%, macroporosity lower than 0,13 m3 m-3 and capacity of total aeration lower than 0,15 m3 m-3 for the 0,07 to 0,12 m depth.
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spelling Genú, Aline Marqueshttp://lattes.cnpq.br/9286085119193660Pott, Cristiano Andréhttp://lattes.cnpq.br/7560267294347037076.401.039.-59http://lattes.cnpq.br/4894209415643683Bareta Junior, Eloi2019-02-21T12:39:08Z2018-07-31Bareta Junior, Eloi. QUALIDADE FÍSICA DO SOLO E LIMITES CRÍTICOS DE ATRIBUTOS FÍSICOS DE LATOSSOLO BRUNO DISTRÓFICO EM FUNÇÃO DA PRODUTIVIDADE DAS CULTURAS DE MILHO E AVEIA. 2018. 63 f. Dissertação (Programa de Pós-Graduação em Agronomia - Mestrado) - Universidade Estadual do Centro-Oeste, Guarapuava - PR.http://tede.unicentro.br:8080/jspui/handle/jspui/928With the upgrading of the agriculture and production of seeds and fodder, mostly under no tillage system, the use of agricultural machines and implements of great size has become more common, many times under not appropriated soil conditions, all on behalf of operating income. On that way, the excessive traffic, allied to a high soil humidity, have been upgrading the levels of soil compaction. The process of soil compaction, is related to the modification of the soil physical quality, presenting increases in soil density, decreases of macroporosity, decreases of water infiltration tax in the soil and increases the soil penetration resistance. The modification of the soil physical quality affects the root development and the crops productivities. To have technical subsidy at the decision-making to realise the mechanical intervention or the management practice change aiming decompress the soil, is necessary to know the critical levels of the soil physical attributes that are employed to determine the soil physical quality. Therefore, the objective of this work was to submit the soil to various intensities of tractor traffic to achieve different levels of soil compaction aiming to identify the critical limits of physical attributes to the maize and oat crop on a Xanthic Hapludox. The study was conducted at the experimental area of the agronomy department from Unicentro, at Guarapuava, PR. The trial design was a completely randomized blocks with six repetitions. The treatments were: The witness (without compaction), two, five and twenty passes with the agricultural tractor. The physical attributes were determined before the maize sowing and before the black oat sowing. Both crops were cultivated under no tillage system and measured their productivities. The critical limits for soil density, relative density, macroporosity and capacity of total aeration were determined for the maize and oat crops. The soil compaction caused by the tractor traffic caused change of the soil density, relative density, macroporosity, microporosity, field capacity, capacity of total aeration, water infiltration tax in the soil and soil resistance of penetration. Among the parameters associated to the crops, fodder and seed productivities of maize and dry matter of oat held higher effect of compaction, entailing on lower productivities on both crops. The depth sampled that best represented adjusted to determine the critical limits of the physical attributes from the soil was at 0,07 to 0,12 m. At this depth, for the maize crop, the ideal range of soil density was at the range from 0,93 to 1,07 Mg m-3 , for relative density the ideal range was from 76,9 to 90,4%, for macroporosity the ideal range was from 0,12 to 0,21 m3 m-3 and for the attribute capacity of total aeration the ideal values are on the range from 0,14 to 0,24 m3 m-3. The oat crop showed productivity limitation when the values of soil density were lower than 1,03 Mg m-3 , relative density lower than 85,7%, macroporosity lower than 0,13 m3 m-3 and capacity of total aeration lower than 0,15 m3 m-3 for the 0,07 to 0,12 m depth.Com a modernização da agricultura na produção de grãos e forragens, majoritariamente sob sistema de plantio direto, a utilização de máquinas e implementos agrícolas de grande porte vem se tornando mais frequente, muitas vezes sob condições de solo inapropriadas, tudo em prol do rendimento operacional. Desta maneira, o tráfego excessivo, aliado a uma alta umidade do solo, vem elevando os níveis de compactação do solo. O processo de compactação do solo, esta relacionado à alteração da qualidade física do solo, apresentando aumento da densidade do solo, diminuição da macroporosidade, diminuição da taxa de infiltração de água no solo e aumento da resistência do solo à penetração. A modificação da qualidade física do solo influencia o desenvolvimento radicular e a produtividade das culturas. Para se ter subsidio técnico na tomada de decisão para realizar uma intervenção mecânica ou alteração de prática de manejo visando descompactar o solo, necessita-se conhecer os níveis críticos dos atributos físicos que são empregados para se determinar a qualidade física do solo. Assim, o objetivo do trabalho foi submeter o solo à várias intensidades de tráfego de trator para atingir diferentes níveis de compactação do solo visando identificar os limites críticos de atributos físicos para as culturas do milho e aveia em um Latossolo Bruno. O estudo foi realizado na área experimental do departamento de agronomia da UNICENTRO, em Guarapuava, PR. O delineamento experimental foi de blocos casualizados com seis repetições. Os tratamentos foram: Testemunha (sem compactação), duas, cinco e vinte passadas de trator agrícola. Foram determinados os atributos físicos antes da semeadura do milho e antes da semeadura da aveia preta. Ambas as culturas foram cultivadas em sistema plantio direto e mensurado a produtividade das culturas. Os limites críticos para densidade do solo, densidade relativa, macroporosidade e capacidade de aeração total foram determinados para as culturas do milho e da aveia preta. A compactação do solo ocasionada pelo trafego de trator ocasionou alteração da densidade do solo, da densidade relativa, da macroporosidade, da microporosidade, da capacidade de campo, da capacidade de aeração total, da taxa de infiltração de água no solo e da resistência do solo à penetração. Dentre os parâmetros associados às culturas, produtividade de forragem e grãos do milho e matéria seca da aveia tiveram maior efeito da compactação, acarretando em menores produtividades de ambas as culturas. A profundidade amostrada que melhor representou se ajustou para determinação dos limites críticos dos atributos físicos do solo foi a de 0,07-0,12m. Nessa profundidade, para a cultura do milho, a faixa ideal de densidade do solo foi a 0,93 a 1,07 Mg m-3, para densidade relativa a faixa ideal foi de 76,9 a 90,4%, para macroporosidade a faixa ideal foi de 0,12 a 0,21 m3 m-3 e para o atributo capacidade de aeração total os valores ideais enquadraram-se na faixa de 0,14 a 0,24 m3 m-3. A cultura da aveia preta apresentou limitação de produtividade quando os valores de densidade do solo foram menor que 1,03 Mg m-3, densidade relativa menor que 85,7%, macroporosidade menor que 0,13 m3 m-3 e capacidade de aeração total menor que 0,15 m3 m-3 para a camada de 0,07-0,12 m.Submitted by Fabiano Jucá (fjuca@unicentro.br) on 2019-02-21T12:39:08Z No. of bitstreams: 1 dissertacao_final_eloi_bareta.pdf: 3984476 bytes, checksum: 708776b318fcaefb4a3c812ec51cecfb (MD5)Made available in DSpace on 2019-02-21T12:39:08Z (GMT). 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dc.title.por.fl_str_mv QUALIDADE FÍSICA DO SOLO E LIMITES CRÍTICOS DE ATRIBUTOS FÍSICOS DE LATOSSOLO BRUNO DISTRÓFICO EM FUNÇÃO DA PRODUTIVIDADE DAS CULTURAS DE MILHO E AVEIA
dc.title.alternative.eng.fl_str_mv Soil physical quality and critical limits of physical attributes of a Xanthic Hapludox according to the productivity of maize and oat crop
title QUALIDADE FÍSICA DO SOLO E LIMITES CRÍTICOS DE ATRIBUTOS FÍSICOS DE LATOSSOLO BRUNO DISTRÓFICO EM FUNÇÃO DA PRODUTIVIDADE DAS CULTURAS DE MILHO E AVEIA
spellingShingle QUALIDADE FÍSICA DO SOLO E LIMITES CRÍTICOS DE ATRIBUTOS FÍSICOS DE LATOSSOLO BRUNO DISTRÓFICO EM FUNÇÃO DA PRODUTIVIDADE DAS CULTURAS DE MILHO E AVEIA
Bareta Junior, Eloi
compactação do solo
porosidade
densidade do solo
tráfego de máquina
indicadores de qualidade física
soil compaction
porosity
soil density
machine traffic
physical quality indicators
CIENCIAS AGRARIAS::AGRONOMIA
title_short QUALIDADE FÍSICA DO SOLO E LIMITES CRÍTICOS DE ATRIBUTOS FÍSICOS DE LATOSSOLO BRUNO DISTRÓFICO EM FUNÇÃO DA PRODUTIVIDADE DAS CULTURAS DE MILHO E AVEIA
title_full QUALIDADE FÍSICA DO SOLO E LIMITES CRÍTICOS DE ATRIBUTOS FÍSICOS DE LATOSSOLO BRUNO DISTRÓFICO EM FUNÇÃO DA PRODUTIVIDADE DAS CULTURAS DE MILHO E AVEIA
title_fullStr QUALIDADE FÍSICA DO SOLO E LIMITES CRÍTICOS DE ATRIBUTOS FÍSICOS DE LATOSSOLO BRUNO DISTRÓFICO EM FUNÇÃO DA PRODUTIVIDADE DAS CULTURAS DE MILHO E AVEIA
title_full_unstemmed QUALIDADE FÍSICA DO SOLO E LIMITES CRÍTICOS DE ATRIBUTOS FÍSICOS DE LATOSSOLO BRUNO DISTRÓFICO EM FUNÇÃO DA PRODUTIVIDADE DAS CULTURAS DE MILHO E AVEIA
title_sort QUALIDADE FÍSICA DO SOLO E LIMITES CRÍTICOS DE ATRIBUTOS FÍSICOS DE LATOSSOLO BRUNO DISTRÓFICO EM FUNÇÃO DA PRODUTIVIDADE DAS CULTURAS DE MILHO E AVEIA
author Bareta Junior, Eloi
author_facet Bareta Junior, Eloi
author_role author
dc.contributor.advisor1.fl_str_mv Genú, Aline Marques
dc.contributor.advisor1Lattes.fl_str_mv http://lattes.cnpq.br/9286085119193660
dc.contributor.advisor-co1.fl_str_mv Pott, Cristiano André
dc.contributor.advisor-co1Lattes.fl_str_mv http://lattes.cnpq.br/7560267294347037
dc.contributor.authorID.fl_str_mv 076.401.039.-59
dc.contributor.authorLattes.fl_str_mv http://lattes.cnpq.br/4894209415643683
dc.contributor.author.fl_str_mv Bareta Junior, Eloi
contributor_str_mv Genú, Aline Marques
Pott, Cristiano André
dc.subject.por.fl_str_mv compactação do solo
porosidade
densidade do solo
tráfego de máquina
indicadores de qualidade física
topic compactação do solo
porosidade
densidade do solo
tráfego de máquina
indicadores de qualidade física
soil compaction
porosity
soil density
machine traffic
physical quality indicators
CIENCIAS AGRARIAS::AGRONOMIA
dc.subject.eng.fl_str_mv soil compaction
porosity
soil density
machine traffic
physical quality indicators
dc.subject.cnpq.fl_str_mv CIENCIAS AGRARIAS::AGRONOMIA
description With the upgrading of the agriculture and production of seeds and fodder, mostly under no tillage system, the use of agricultural machines and implements of great size has become more common, many times under not appropriated soil conditions, all on behalf of operating income. On that way, the excessive traffic, allied to a high soil humidity, have been upgrading the levels of soil compaction. The process of soil compaction, is related to the modification of the soil physical quality, presenting increases in soil density, decreases of macroporosity, decreases of water infiltration tax in the soil and increases the soil penetration resistance. The modification of the soil physical quality affects the root development and the crops productivities. To have technical subsidy at the decision-making to realise the mechanical intervention or the management practice change aiming decompress the soil, is necessary to know the critical levels of the soil physical attributes that are employed to determine the soil physical quality. Therefore, the objective of this work was to submit the soil to various intensities of tractor traffic to achieve different levels of soil compaction aiming to identify the critical limits of physical attributes to the maize and oat crop on a Xanthic Hapludox. The study was conducted at the experimental area of the agronomy department from Unicentro, at Guarapuava, PR. The trial design was a completely randomized blocks with six repetitions. The treatments were: The witness (without compaction), two, five and twenty passes with the agricultural tractor. The physical attributes were determined before the maize sowing and before the black oat sowing. Both crops were cultivated under no tillage system and measured their productivities. The critical limits for soil density, relative density, macroporosity and capacity of total aeration were determined for the maize and oat crops. The soil compaction caused by the tractor traffic caused change of the soil density, relative density, macroporosity, microporosity, field capacity, capacity of total aeration, water infiltration tax in the soil and soil resistance of penetration. Among the parameters associated to the crops, fodder and seed productivities of maize and dry matter of oat held higher effect of compaction, entailing on lower productivities on both crops. The depth sampled that best represented adjusted to determine the critical limits of the physical attributes from the soil was at 0,07 to 0,12 m. At this depth, for the maize crop, the ideal range of soil density was at the range from 0,93 to 1,07 Mg m-3 , for relative density the ideal range was from 76,9 to 90,4%, for macroporosity the ideal range was from 0,12 to 0,21 m3 m-3 and for the attribute capacity of total aeration the ideal values are on the range from 0,14 to 0,24 m3 m-3. The oat crop showed productivity limitation when the values of soil density were lower than 1,03 Mg m-3 , relative density lower than 85,7%, macroporosity lower than 0,13 m3 m-3 and capacity of total aeration lower than 0,15 m3 m-3 for the 0,07 to 0,12 m depth.
publishDate 2018
dc.date.issued.fl_str_mv 2018-07-31
dc.date.accessioned.fl_str_mv 2019-02-21T12:39:08Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/masterThesis
format masterThesis
status_str publishedVersion
dc.identifier.citation.fl_str_mv Bareta Junior, Eloi. QUALIDADE FÍSICA DO SOLO E LIMITES CRÍTICOS DE ATRIBUTOS FÍSICOS DE LATOSSOLO BRUNO DISTRÓFICO EM FUNÇÃO DA PRODUTIVIDADE DAS CULTURAS DE MILHO E AVEIA. 2018. 63 f. Dissertação (Programa de Pós-Graduação em Agronomia - Mestrado) - Universidade Estadual do Centro-Oeste, Guarapuava - PR.
dc.identifier.uri.fl_str_mv http://tede.unicentro.br:8080/jspui/handle/jspui/928
identifier_str_mv Bareta Junior, Eloi. QUALIDADE FÍSICA DO SOLO E LIMITES CRÍTICOS DE ATRIBUTOS FÍSICOS DE LATOSSOLO BRUNO DISTRÓFICO EM FUNÇÃO DA PRODUTIVIDADE DAS CULTURAS DE MILHO E AVEIA. 2018. 63 f. Dissertação (Programa de Pós-Graduação em Agronomia - Mestrado) - Universidade Estadual do Centro-Oeste, Guarapuava - PR.
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