Wheat yield and physical properties of a brown latosol under no-tillage in south-central Paraná

Soil management influences the chemical and physical properties of soil. Chemical conditions have been thoroughly studied, while the role of soil physical conditions regarding crop yield has been neglected. This study aimed to analyze the wheat yield and its relationship with physical properties of...

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Veröffentlicht in:Revista Brasileira de Ciência do Solo 2013-10, Vol.37 (5), p.1216-1225
Hauptverfasser: Kramer, Luiz Fernando Machado, Müller, Marcelo Marques Lopes, Tormena, Cássio Antônio, Michalovicz, Leandro, Nascimento, Ronaldo do, Vicensi, Marcelo
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container_title Revista Brasileira de Ciência do Solo
container_volume 37
creator Kramer, Luiz Fernando Machado
Müller, Marcelo Marques Lopes
Tormena, Cássio Antônio
Michalovicz, Leandro
Nascimento, Ronaldo do
Vicensi, Marcelo
description Soil management influences the chemical and physical properties of soil. Chemical conditions have been thoroughly studied, while the role of soil physical conditions regarding crop yield has been neglected. This study aimed to analyze the wheat yield and its relationship with physical properties of an Oxisol under no-tillage (NT). The study was carried out between 2010 and 2011, in Reserva do Iguaçu, State of Paraná, Brazil, on the Campo Bonito farm, after 25 years of NT management. Based on harvest maps of barley (2006), wheat (2007) and maize (2009) of a plot (150 ha), zones with higher and lower yield potential (Z1 and Z2, respectively) were identified. Sampling grids with 16 units (50 x 50 m) and three sampling points per unit were established. The wheat grain yield (GY) and water infiltration capacity (WIC) were evaluated in 2010. Soil samples with disturbed and undisturbed structure were collected from the 0.00-0.10 and 0.10-0.20 m layers. The former were used to determine soil organic carbon (Corg) levels and the latter to determine soil bulk density (BD), total porosity (TP), macroporosity (Mac), and microporosity (Mic). Soil penetration resistance (PR) and water content (SWC) were also evaluated. The wheat GY of the whole plot was close to the regional average and the yield between the zones differed significantly, i.e. 22 % higher in Z1 than in Z2. No significant variation in Mic was observed between zones, but Z1 had higher Corg levels, SWC, TP and Mac and lower BD than Z2 in both soil layers, as well as a lower PR than Z2 in the 0.00-0.10 m layer. Therefore, soil physical conditions were more restrictive in Z2, in agreement with wheat yield and zone yield potential defined a priori, based on the harvest maps. Soil WIC in Z1 was significantly higher (30 %) than in Z2, in agreement with the results of TP and Mac which were also higher in Z1 in both soil layers. The correlation analysis of data of the two layers showed a positive relationship between wheat GY and the soil properties TP, SWC and WIC. O manejo influencia atributos químicos e físicos do solo; entretanto, os químicos têm sido mais estudados, negligenciando-se a relevância da física do solo para a produtividade das culturas. Os objetivos deste trabalho foram avaliar a produtividade do trigo e caracterizar a sua relação com os atributos físicos de um Latossolo Bruno, sob sistema plantio direto (NT). O estudo foi realizado entre 2010-2011 em Reserva do Iguaçu, Paraná, em um dos talhões d
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Chemical conditions have been thoroughly studied, while the role of soil physical conditions regarding crop yield has been neglected. This study aimed to analyze the wheat yield and its relationship with physical properties of an Oxisol under no-tillage (NT). The study was carried out between 2010 and 2011, in Reserva do Iguaçu, State of Paraná, Brazil, on the Campo Bonito farm, after 25 years of NT management. Based on harvest maps of barley (2006), wheat (2007) and maize (2009) of a plot (150 ha), zones with higher and lower yield potential (Z1 and Z2, respectively) were identified. Sampling grids with 16 units (50 x 50 m) and three sampling points per unit were established. The wheat grain yield (GY) and water infiltration capacity (WIC) were evaluated in 2010. Soil samples with disturbed and undisturbed structure were collected from the 0.00-0.10 and 0.10-0.20 m layers. The former were used to determine soil organic carbon (Corg) levels and the latter to determine soil bulk density (BD), total porosity (TP), macroporosity (Mac), and microporosity (Mic). Soil penetration resistance (PR) and water content (SWC) were also evaluated. The wheat GY of the whole plot was close to the regional average and the yield between the zones differed significantly, i.e. 22 % higher in Z1 than in Z2. No significant variation in Mic was observed between zones, but Z1 had higher Corg levels, SWC, TP and Mac and lower BD than Z2 in both soil layers, as well as a lower PR than Z2 in the 0.00-0.10 m layer. Therefore, soil physical conditions were more restrictive in Z2, in agreement with wheat yield and zone yield potential defined a priori, based on the harvest maps. Soil WIC in Z1 was significantly higher (30 %) than in Z2, in agreement with the results of TP and Mac which were also higher in Z1 in both soil layers. The correlation analysis of data of the two layers showed a positive relationship between wheat GY and the soil properties TP, SWC and WIC. O manejo influencia atributos químicos e físicos do solo; entretanto, os químicos têm sido mais estudados, negligenciando-se a relevância da física do solo para a produtividade das culturas. Os objetivos deste trabalho foram avaliar a produtividade do trigo e caracterizar a sua relação com os atributos físicos de um Latossolo Bruno, sob sistema plantio direto (NT). O estudo foi realizado entre 2010-2011 em Reserva do Iguaçu, Paraná, em um dos talhões da fazenda Campo Bonito, com 25 anos de NT. Os mapas de colheita de cevada (2006), trigo (2007) e milho (2009) permitiram identificar as zonas Z1 (potencial produtivo maior) e Z2 (potencial produtivo menor), em que se estabeleceram malhas amostrais com 16 unidades de 50 x 50 m e três pontos de amostragem por unidade. Em 2010, avaliaram-se a produtividade de grãos (GY) do trigo e a capacidade de infiltração de água no solo (WIC). Amostras de solo com estrutura deformada e indeformada foram coletadas nas camadas de 0,00-0,10 e 0,10-0,20 m. As primeiras serviram para determinar o teor de carbono orgânico (Corg) e as últimas para determinar: densidade do solo (BD), porosidade total do solo (TP), macroporosidade (Mac) e microporosidade (Mic). Avaliaram-se, também, a resistência do solo à penetração (PR) e o conteúdo de água do solo (SWC). A GY do trigo no talhão foi próxima da média regional e houve diferença significativa de rendimento entre zonas, sendo 22 % superior em Z1 em relação a Z2. Não houve variação significativa da Mic entre as zonas do talhão; Z1 apresentou teores de Corg, SWC, TP e Mac maiores e BD menor que Z2, nas duas camadas de solo avaliadas, além de PR menor que Z2, na camada de 0,00-0,10 m, havendo, portanto, condição física de solo mais restritiva em Z2, condizente com os resultados de produtividade do trigo e potencial produtivo delimitado a priori, a partir dos mapas de colheita. A WIC foi significativamente maior (30 %) em Z1 que em Z2, em acordo com os resultados de TP e Mac, também maiores em Z1, nas duas camadas de solo. Considerando-se essas duas camadas, a análise de correlação permitiu destacar relações positivas entre a GY do trigo e TP, SWC e WIC.</description><identifier>ISSN: 0100-0683</identifier><identifier>ISSN: 1806-9657</identifier><identifier>EISSN: 0100-0683</identifier><identifier>DOI: 10.1590/S0100-06832013000500011</identifier><language>eng</language><publisher>Sociedade Brasileira de Ciência do Solo</publisher><subject>correlação ; qualidade física do solo ; rendimento do trigo ; SOIL SCIENCE</subject><ispartof>Revista Brasileira de Ciência do Solo, 2013-10, Vol.37 (5), p.1216-1225</ispartof><rights>This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c341t-e3b4b462244d4c67abb66fc678f1b3cd446a6d4a643e554f6bafec48d51552193</citedby><cites>FETCH-LOGICAL-c341t-e3b4b462244d4c67abb66fc678f1b3cd446a6d4a643e554f6bafec48d51552193</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>230,315,781,785,865,886,27929,27930</link.rule.ids></links><search><creatorcontrib>Kramer, Luiz Fernando Machado</creatorcontrib><creatorcontrib>Müller, Marcelo Marques Lopes</creatorcontrib><creatorcontrib>Tormena, Cássio Antônio</creatorcontrib><creatorcontrib>Michalovicz, Leandro</creatorcontrib><creatorcontrib>Nascimento, Ronaldo do</creatorcontrib><creatorcontrib>Vicensi, Marcelo</creatorcontrib><title>Wheat yield and physical properties of a brown latosol under no-tillage in south-central Paraná</title><title>Revista Brasileira de Ciência do Solo</title><addtitle>Rev. Bras. Ciênc. Solo</addtitle><description>Soil management influences the chemical and physical properties of soil. Chemical conditions have been thoroughly studied, while the role of soil physical conditions regarding crop yield has been neglected. This study aimed to analyze the wheat yield and its relationship with physical properties of an Oxisol under no-tillage (NT). The study was carried out between 2010 and 2011, in Reserva do Iguaçu, State of Paraná, Brazil, on the Campo Bonito farm, after 25 years of NT management. Based on harvest maps of barley (2006), wheat (2007) and maize (2009) of a plot (150 ha), zones with higher and lower yield potential (Z1 and Z2, respectively) were identified. Sampling grids with 16 units (50 x 50 m) and three sampling points per unit were established. The wheat grain yield (GY) and water infiltration capacity (WIC) were evaluated in 2010. Soil samples with disturbed and undisturbed structure were collected from the 0.00-0.10 and 0.10-0.20 m layers. The former were used to determine soil organic carbon (Corg) levels and the latter to determine soil bulk density (BD), total porosity (TP), macroporosity (Mac), and microporosity (Mic). Soil penetration resistance (PR) and water content (SWC) were also evaluated. The wheat GY of the whole plot was close to the regional average and the yield between the zones differed significantly, i.e. 22 % higher in Z1 than in Z2. No significant variation in Mic was observed between zones, but Z1 had higher Corg levels, SWC, TP and Mac and lower BD than Z2 in both soil layers, as well as a lower PR than Z2 in the 0.00-0.10 m layer. Therefore, soil physical conditions were more restrictive in Z2, in agreement with wheat yield and zone yield potential defined a priori, based on the harvest maps. Soil WIC in Z1 was significantly higher (30 %) than in Z2, in agreement with the results of TP and Mac which were also higher in Z1 in both soil layers. The correlation analysis of data of the two layers showed a positive relationship between wheat GY and the soil properties TP, SWC and WIC. O manejo influencia atributos químicos e físicos do solo; entretanto, os químicos têm sido mais estudados, negligenciando-se a relevância da física do solo para a produtividade das culturas. Os objetivos deste trabalho foram avaliar a produtividade do trigo e caracterizar a sua relação com os atributos físicos de um Latossolo Bruno, sob sistema plantio direto (NT). O estudo foi realizado entre 2010-2011 em Reserva do Iguaçu, Paraná, em um dos talhões da fazenda Campo Bonito, com 25 anos de NT. Os mapas de colheita de cevada (2006), trigo (2007) e milho (2009) permitiram identificar as zonas Z1 (potencial produtivo maior) e Z2 (potencial produtivo menor), em que se estabeleceram malhas amostrais com 16 unidades de 50 x 50 m e três pontos de amostragem por unidade. Em 2010, avaliaram-se a produtividade de grãos (GY) do trigo e a capacidade de infiltração de água no solo (WIC). Amostras de solo com estrutura deformada e indeformada foram coletadas nas camadas de 0,00-0,10 e 0,10-0,20 m. As primeiras serviram para determinar o teor de carbono orgânico (Corg) e as últimas para determinar: densidade do solo (BD), porosidade total do solo (TP), macroporosidade (Mac) e microporosidade (Mic). Avaliaram-se, também, a resistência do solo à penetração (PR) e o conteúdo de água do solo (SWC). A GY do trigo no talhão foi próxima da média regional e houve diferença significativa de rendimento entre zonas, sendo 22 % superior em Z1 em relação a Z2. Não houve variação significativa da Mic entre as zonas do talhão; Z1 apresentou teores de Corg, SWC, TP e Mac maiores e BD menor que Z2, nas duas camadas de solo avaliadas, além de PR menor que Z2, na camada de 0,00-0,10 m, havendo, portanto, condição física de solo mais restritiva em Z2, condizente com os resultados de produtividade do trigo e potencial produtivo delimitado a priori, a partir dos mapas de colheita. A WIC foi significativamente maior (30 %) em Z1 que em Z2, em acordo com os resultados de TP e Mac, também maiores em Z1, nas duas camadas de solo. Considerando-se essas duas camadas, a análise de correlação permitiu destacar relações positivas entre a GY do trigo e TP, SWC e WIC.</description><subject>correlação</subject><subject>qualidade física do solo</subject><subject>rendimento do trigo</subject><subject>SOIL SCIENCE</subject><issn>0100-0683</issn><issn>1806-9657</issn><issn>0100-0683</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><sourceid>DOA</sourceid><recordid>eNp1UdtKAzEQDaJgrX6D-YHVyW6S7j5K8VIoKKj4GCeXbbesmyXZIv0cv8UfM7ZSBPFhmGGGc87MGULOGVwwUcHlIzCADGRZ5MAKABApGDsgo_3g8Fd9TE5iXAHkFVR8RF5flg4Humlcayl2lvbLTWwMtrQPvndhaFykvqZIdfDvHW1x8NG3dN1ZF2jns6FpW1w42nQ0-vWwzIzrhpDwDxiw-_w4JUc1ttGd_eQxeb65fpreZfP729n0ap6ZgrMhc4Xmmss859xyIyeotZR1Ksqa6cJYziVKy1HywgnBa6mxdoaXVjAhclYVYzLb8VqPK9WH5g3DRnls1Lbhw0Jhusa0TkESsMzqQlcsqUFZcWG4AZaXXFQTk7gudlzRJF-8Wvl16NLyauu1-uN1Akx2ABN8jMHV-wUYqO8v_Yv8Auatgso</recordid><startdate>20131001</startdate><enddate>20131001</enddate><creator>Kramer, Luiz Fernando Machado</creator><creator>Müller, Marcelo Marques Lopes</creator><creator>Tormena, Cássio Antônio</creator><creator>Michalovicz, Leandro</creator><creator>Nascimento, Ronaldo do</creator><creator>Vicensi, Marcelo</creator><general>Sociedade Brasileira de Ciência do Solo</general><scope>AAYXX</scope><scope>CITATION</scope><scope>GPN</scope><scope>DOA</scope></search><sort><creationdate>20131001</creationdate><title>Wheat yield and physical properties of a brown latosol under no-tillage in south-central Paraná</title><author>Kramer, Luiz Fernando Machado ; Müller, Marcelo Marques Lopes ; Tormena, Cássio Antônio ; Michalovicz, Leandro ; Nascimento, Ronaldo do ; Vicensi, Marcelo</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c341t-e3b4b462244d4c67abb66fc678f1b3cd446a6d4a643e554f6bafec48d51552193</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>correlação</topic><topic>qualidade física do solo</topic><topic>rendimento do trigo</topic><topic>SOIL SCIENCE</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kramer, Luiz Fernando Machado</creatorcontrib><creatorcontrib>Müller, Marcelo Marques Lopes</creatorcontrib><creatorcontrib>Tormena, Cássio Antônio</creatorcontrib><creatorcontrib>Michalovicz, Leandro</creatorcontrib><creatorcontrib>Nascimento, Ronaldo do</creatorcontrib><creatorcontrib>Vicensi, Marcelo</creatorcontrib><collection>CrossRef</collection><collection>SciELO</collection><collection>DOAJ Directory of Open Access Journals</collection><jtitle>Revista Brasileira de Ciência do Solo</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kramer, Luiz Fernando Machado</au><au>Müller, Marcelo Marques Lopes</au><au>Tormena, Cássio Antônio</au><au>Michalovicz, Leandro</au><au>Nascimento, Ronaldo do</au><au>Vicensi, Marcelo</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Wheat yield and physical properties of a brown latosol under no-tillage in south-central Paraná</atitle><jtitle>Revista Brasileira de Ciência do Solo</jtitle><addtitle>Rev. Bras. Ciênc. Solo</addtitle><date>2013-10-01</date><risdate>2013</risdate><volume>37</volume><issue>5</issue><spage>1216</spage><epage>1225</epage><pages>1216-1225</pages><issn>0100-0683</issn><issn>1806-9657</issn><eissn>0100-0683</eissn><abstract>Soil management influences the chemical and physical properties of soil. Chemical conditions have been thoroughly studied, while the role of soil physical conditions regarding crop yield has been neglected. This study aimed to analyze the wheat yield and its relationship with physical properties of an Oxisol under no-tillage (NT). The study was carried out between 2010 and 2011, in Reserva do Iguaçu, State of Paraná, Brazil, on the Campo Bonito farm, after 25 years of NT management. Based on harvest maps of barley (2006), wheat (2007) and maize (2009) of a plot (150 ha), zones with higher and lower yield potential (Z1 and Z2, respectively) were identified. Sampling grids with 16 units (50 x 50 m) and three sampling points per unit were established. The wheat grain yield (GY) and water infiltration capacity (WIC) were evaluated in 2010. Soil samples with disturbed and undisturbed structure were collected from the 0.00-0.10 and 0.10-0.20 m layers. The former were used to determine soil organic carbon (Corg) levels and the latter to determine soil bulk density (BD), total porosity (TP), macroporosity (Mac), and microporosity (Mic). Soil penetration resistance (PR) and water content (SWC) were also evaluated. The wheat GY of the whole plot was close to the regional average and the yield between the zones differed significantly, i.e. 22 % higher in Z1 than in Z2. No significant variation in Mic was observed between zones, but Z1 had higher Corg levels, SWC, TP and Mac and lower BD than Z2 in both soil layers, as well as a lower PR than Z2 in the 0.00-0.10 m layer. Therefore, soil physical conditions were more restrictive in Z2, in agreement with wheat yield and zone yield potential defined a priori, based on the harvest maps. Soil WIC in Z1 was significantly higher (30 %) than in Z2, in agreement with the results of TP and Mac which were also higher in Z1 in both soil layers. The correlation analysis of data of the two layers showed a positive relationship between wheat GY and the soil properties TP, SWC and WIC. O manejo influencia atributos químicos e físicos do solo; entretanto, os químicos têm sido mais estudados, negligenciando-se a relevância da física do solo para a produtividade das culturas. Os objetivos deste trabalho foram avaliar a produtividade do trigo e caracterizar a sua relação com os atributos físicos de um Latossolo Bruno, sob sistema plantio direto (NT). O estudo foi realizado entre 2010-2011 em Reserva do Iguaçu, Paraná, em um dos talhões da fazenda Campo Bonito, com 25 anos de NT. Os mapas de colheita de cevada (2006), trigo (2007) e milho (2009) permitiram identificar as zonas Z1 (potencial produtivo maior) e Z2 (potencial produtivo menor), em que se estabeleceram malhas amostrais com 16 unidades de 50 x 50 m e três pontos de amostragem por unidade. Em 2010, avaliaram-se a produtividade de grãos (GY) do trigo e a capacidade de infiltração de água no solo (WIC). Amostras de solo com estrutura deformada e indeformada foram coletadas nas camadas de 0,00-0,10 e 0,10-0,20 m. As primeiras serviram para determinar o teor de carbono orgânico (Corg) e as últimas para determinar: densidade do solo (BD), porosidade total do solo (TP), macroporosidade (Mac) e microporosidade (Mic). Avaliaram-se, também, a resistência do solo à penetração (PR) e o conteúdo de água do solo (SWC). A GY do trigo no talhão foi próxima da média regional e houve diferença significativa de rendimento entre zonas, sendo 22 % superior em Z1 em relação a Z2. Não houve variação significativa da Mic entre as zonas do talhão; Z1 apresentou teores de Corg, SWC, TP e Mac maiores e BD menor que Z2, nas duas camadas de solo avaliadas, além de PR menor que Z2, na camada de 0,00-0,10 m, havendo, portanto, condição física de solo mais restritiva em Z2, condizente com os resultados de produtividade do trigo e potencial produtivo delimitado a priori, a partir dos mapas de colheita. A WIC foi significativamente maior (30 %) em Z1 que em Z2, em acordo com os resultados de TP e Mac, também maiores em Z1, nas duas camadas de solo. Considerando-se essas duas camadas, a análise de correlação permitiu destacar relações positivas entre a GY do trigo e TP, SWC e WIC.</abstract><pub>Sociedade Brasileira de Ciência do Solo</pub><doi>10.1590/S0100-06832013000500011</doi><tpages>10</tpages><oa>free_for_read</oa></addata></record>
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subjects correlação
qualidade física do solo
rendimento do trigo
SOIL SCIENCE
title Wheat yield and physical properties of a brown latosol under no-tillage in south-central Paraná
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