Nitrogênio hidrolisável em meio alcalino no perfil de solos cultivados com arroz irrigado e sua contribuição para a nutrição da cultura
Autor(a) principal: | |
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Data de Publicação: | 2019 |
Tipo de documento: | Tese |
Idioma: | por |
Título da fonte: | Manancial - Repositório Digital da UFSM |
dARK ID: | ark:/26339/001300000gggq |
Texto Completo: | http://repositorio.ufsm.br/handle/1/20234 |
Resumo: | Rice is an important food source for the world's population and is a substantial crop for Southern Brazil economic development. Nitrogen (N) is one of the most limiting nutrients for rice crop production, and the current N fertilizer recommendation for rice in Southern Brazil is based on soil organic matter (SOM) content at the 0-20 cm layer. However, the recommended N rates are very close for the different SOM classes and there is not always a yield increase by adding fertilizer. In flooded soils, the water input affects the dynamics of SOM decomposition and the N cycle, making it more difficult to predict the N rate based only on SOM content. More accurate N availability indexes, the N evaluation in soil profile and its recovery by rice plants, as well as the effect of N from greater soil depths on rice root morphology can help to improve our understanding on the nutrient dynamics in this production system, while contributing to improve the crop N fertilizer recommendation. This work aims to broaden our understanding of N dynamics in areas cultivated with rice and its relationship with soil properties, as well as identifying the capacity of plants to use N available at greater soil depths. A study was conducted to evaluate the total content and the amount of clay fixed ammonium (CF-NH4) extracted by the Nitrogen Soil Test for Rice (N-STaR) in soils from Arkansas, United States. In soils from southern Brazil, we evaluate the alkaline hydrolyzable N (AH-N) distribution in soil profile and its relationship with soil properties; we investigated the rice N recovery and absorption dynamics from different soil depths; and the effect of N from different soil depths on rice root growth and plant nutrition was also evaluated. The CF-NH4 represents 24.8 and 28.1% of the total N content at the 0-15 and 15-30 cm layers respectively, and the N-STaR estimates that a small proportion (<15%) of this N pool is plant available. These results indicate that CF-NH4 is an important soil N pool and might be a primary N source for rice crop. The AH-N distribution in soil profile is distinct between soils and can have increments in depth. Although granulometric fractions are strongly correlated with AH-N content for some soils, the total N is the major variable dictating AH-N distribution in soil profile. Rice effectively uses available N from depths of up to 45 cm and N recovery is affected by soil physical properties, especially hydraulic conductivity. Higher 15N recovery and N derived from fertilizer occurred when N was applied at the 10, 20 and 30 cm depths, which indicates that the N application in subsurface can increase the nutrient use efficiency by rice crop. The N availability in depth increased the root length, root surface area, and root volume while reducing the root average diameter. The N located at the soil superficial layers is absorbed by the plants in more responsive stages to fertilization, resulting in greater dry mass production. The N located at 30 and 45 cm contributed to plant nutrition at the reproductive stage, increasing the 15N content in the index leaves, the N content in tissue, the chlorophyll content, the photosynthesis rate and the carboxylation efficiency by Rubisco at rice heading. The N available in greater depths than 20 cm contributes to plant nutrition and should be considered in future studies involving the prediction and calibration of N availability indexes for flooded rice. |
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Nitrogênio hidrolisável em meio alcalino no perfil de solos cultivados com arroz irrigado e sua contribuição para a nutrição da culturaAlkaline hydrolizable nitrogen in flooded rice fields soil profile and its contribution for rice crop nutritionAnálise do soloBalanço nutricionalFertilizante nitrogenadoMatéria orgânicaOryza sativa L.Recuperação de 15NSoil analysisNutritional balanceNitrogen fertilizerOrganic matter15N recoveryCNPQ::CIENCIAS AGRARIAS::AGRONOMIA::CIENCIA DO SOLORice is an important food source for the world's population and is a substantial crop for Southern Brazil economic development. Nitrogen (N) is one of the most limiting nutrients for rice crop production, and the current N fertilizer recommendation for rice in Southern Brazil is based on soil organic matter (SOM) content at the 0-20 cm layer. However, the recommended N rates are very close for the different SOM classes and there is not always a yield increase by adding fertilizer. In flooded soils, the water input affects the dynamics of SOM decomposition and the N cycle, making it more difficult to predict the N rate based only on SOM content. More accurate N availability indexes, the N evaluation in soil profile and its recovery by rice plants, as well as the effect of N from greater soil depths on rice root morphology can help to improve our understanding on the nutrient dynamics in this production system, while contributing to improve the crop N fertilizer recommendation. This work aims to broaden our understanding of N dynamics in areas cultivated with rice and its relationship with soil properties, as well as identifying the capacity of plants to use N available at greater soil depths. A study was conducted to evaluate the total content and the amount of clay fixed ammonium (CF-NH4) extracted by the Nitrogen Soil Test for Rice (N-STaR) in soils from Arkansas, United States. In soils from southern Brazil, we evaluate the alkaline hydrolyzable N (AH-N) distribution in soil profile and its relationship with soil properties; we investigated the rice N recovery and absorption dynamics from different soil depths; and the effect of N from different soil depths on rice root growth and plant nutrition was also evaluated. The CF-NH4 represents 24.8 and 28.1% of the total N content at the 0-15 and 15-30 cm layers respectively, and the N-STaR estimates that a small proportion (<15%) of this N pool is plant available. These results indicate that CF-NH4 is an important soil N pool and might be a primary N source for rice crop. The AH-N distribution in soil profile is distinct between soils and can have increments in depth. Although granulometric fractions are strongly correlated with AH-N content for some soils, the total N is the major variable dictating AH-N distribution in soil profile. Rice effectively uses available N from depths of up to 45 cm and N recovery is affected by soil physical properties, especially hydraulic conductivity. Higher 15N recovery and N derived from fertilizer occurred when N was applied at the 10, 20 and 30 cm depths, which indicates that the N application in subsurface can increase the nutrient use efficiency by rice crop. The N availability in depth increased the root length, root surface area, and root volume while reducing the root average diameter. The N located at the soil superficial layers is absorbed by the plants in more responsive stages to fertilization, resulting in greater dry mass production. The N located at 30 and 45 cm contributed to plant nutrition at the reproductive stage, increasing the 15N content in the index leaves, the N content in tissue, the chlorophyll content, the photosynthesis rate and the carboxylation efficiency by Rubisco at rice heading. The N available in greater depths than 20 cm contributes to plant nutrition and should be considered in future studies involving the prediction and calibration of N availability indexes for flooded rice.Conselho Nacional de Pesquisa e Desenvolvimento Científico e Tecnológico - CNPqO arroz é uma importante fonte de alimento para a população mundial e uma cultura substancial para o desenvolvimento econômico do Sul do Brasil. O nitrogênio (N) é um dos nutrientes mais limitantes para a produção da cultura do arroz, sendo a atual recomendação da adubação nitrogenada para o arroz no Sul do Brasil baseada no teor de matéria orgânica do solo (MOS) da camada de 0-20 cm. Contudo, as doses de N recomendadas são muito próximas para as diferentes classes de MOS e, nem sempre, ocorre incremento em produtividade pela adição do fertilizante. Em solos sujeitos ao alagamento, a entrada da água afeta a dinâmica de decomposição da MOS e o ciclo do N, dificultando a predição da dose de N apenas pelo teor de MOS. Índices de disponibilidade de N mais precisos, a avaliação do N no perfil do solo e sua recuperação pelo arroz, bem como o efeito do N de maiores profundidades do solo sobre a morfologia radicular das plantas podem auxiliar para uma melhor compreensão da dinâmica do nutriente neste sistema de produção, contribuindo para aprimorar a recomendação do fertilizante nitrogenado para a cultura. Este trabalho objetiva ampliar a compreensão sobre a dinâmica do N em áreas cultivadas com arroz irrigado e sua relação com as propriedades do solo, bem como identificar a capacidade das plantas utilizarem o N disponível em maiores profundidades no solo. Foi conduzido um estudo avaliando o teor total e a quantidade de amônio fixo pela argila (CF-NH4) extraída pelo Nitrogen Soil Test for Rice (N-STaR) em solos do Arkansas, Estados Unidos. Em solos do Sul do Brasil, foi avaliada a distribuição do N hidrolisável em meio alcalino (AH-N) no perfil do solo e sua relação com as propriedades do solo; foi estudada a recuperação e a dinâmica de absorção do N de diferentes profundidades pelo arroz; e, foi avaliado o efeito do N de diferentes profundidades do solo sobre o crescimento radicular e a nutrição das plantas. O CF-NH4 representa 24.8 e 28.1% do teor de N total nas camadas de 0-15 e 15-30 cm, respectivamente, sendo que o N-STaR estima que uma pequena proporção (<15%) deste compartimento de N seja disponível as plantas. Estes resultados indicam que CF-NH4 é um importante compartimento de N do solo, podendo ser uma fonte primária de N para o arroz. A distribuição do AH-N no perfil do solo é distinta entre solos e pode apresentar incrementos em profundidade. Embora as frações granulométricas estejam fortemente correlacionas com o teor de AH-N para alguns solos, o N total é a principal variável que determina a distribuição do AH-N no perfil do solo. O arroz utiliza efetivamente o N disponível em profundidades de até 45 cm e a recuperação do N é afetada pelas propriedades físicas do solo, especialmente a condutividade hidráulica. Maior recuperação de 15N e N derivado do fertilizante ocorreu quando o N foi aplicado aos 10, 20 e 30 cm de profundidade, o que indica que a aplicação do N em subsuperfície pode aumentar a eficiência de utilização do nutriente pela cultura do arroz. A disponibilidade de N em profundidade aumentou o comprimento, área superficial e volume radicular e reduziu o diâmetro médio das raízes. O N localizado nas camadas superficiais do solo é absorvido pelas plantas em estágios mais responsivos à adubação, resultando em maior produção de massa seca. O N localizado aos 30 e 45 cm contribuiu para a nutrição das plantas no estágio reprodutivo, aumentando o teor de 15N na folha índice, o teor de N no tecido, o teor clorofila, a taxa fotossintética e eficiência de carboxilação pela Rubisco no florescimento do arroz. O N disponível em profundidades superiores à 20 cm contribui para a nutrição das plantas e deve ser considerado em estudos futuros envolvendo a predição e calibração de índices de disponibilidade de N para o arroz irrigado por alagamento.Universidade Federal de Santa MariaBrasilAgronomiaUFSMPrograma de Pós-Graduação em Ciência do SoloCentro de Ciências RuraisSilva, Leandro Souza dahttp://lattes.cnpq.br/2152888530643357Carlos, Filipe Selauhttp://lattes.cnpq.br/1071521284494576Brunetto, Gustavohttp://lattes.cnpq.br/1185169003700830Ferreira, Paulo Ademar Avelarhttp://lattes.cnpq.br/1871733582967061Scivittaro, Walkyria Buenohttp://lattes.cnpq.br/7090419604571199Drescher, Gerson Laerson2020-12-29T10:21:38Z2020-12-29T10:21:38Z2019-01-25info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/doctoralThesisapplication/pdfhttp://repositorio.ufsm.br/handle/1/20234ark:/26339/001300000gggqporAttribution-NonCommercial-NoDerivatives 4.0 Internationalhttp://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccessreponame:Manancial - Repositório Digital da UFSMinstname:Universidade Federal de Santa Maria (UFSM)instacron:UFSM2020-12-30T06:02:27Zoai:repositorio.ufsm.br:1/20234Biblioteca Digital de Teses e Dissertaçõeshttps://repositorio.ufsm.br/ONGhttps://repositorio.ufsm.br/oai/requestatendimento.sib@ufsm.br||tedebc@gmail.comopendoar:2020-12-30T06:02:27Manancial - Repositório Digital da UFSM - Universidade Federal de Santa Maria (UFSM)false |
dc.title.none.fl_str_mv |
Nitrogênio hidrolisável em meio alcalino no perfil de solos cultivados com arroz irrigado e sua contribuição para a nutrição da cultura Alkaline hydrolizable nitrogen in flooded rice fields soil profile and its contribution for rice crop nutrition |
title |
Nitrogênio hidrolisável em meio alcalino no perfil de solos cultivados com arroz irrigado e sua contribuição para a nutrição da cultura |
spellingShingle |
Nitrogênio hidrolisável em meio alcalino no perfil de solos cultivados com arroz irrigado e sua contribuição para a nutrição da cultura Drescher, Gerson Laerson Análise do solo Balanço nutricional Fertilizante nitrogenado Matéria orgânica Oryza sativa L. Recuperação de 15N Soil analysis Nutritional balance Nitrogen fertilizer Organic matter 15N recovery CNPQ::CIENCIAS AGRARIAS::AGRONOMIA::CIENCIA DO SOLO |
title_short |
Nitrogênio hidrolisável em meio alcalino no perfil de solos cultivados com arroz irrigado e sua contribuição para a nutrição da cultura |
title_full |
Nitrogênio hidrolisável em meio alcalino no perfil de solos cultivados com arroz irrigado e sua contribuição para a nutrição da cultura |
title_fullStr |
Nitrogênio hidrolisável em meio alcalino no perfil de solos cultivados com arroz irrigado e sua contribuição para a nutrição da cultura |
title_full_unstemmed |
Nitrogênio hidrolisável em meio alcalino no perfil de solos cultivados com arroz irrigado e sua contribuição para a nutrição da cultura |
title_sort |
Nitrogênio hidrolisável em meio alcalino no perfil de solos cultivados com arroz irrigado e sua contribuição para a nutrição da cultura |
author |
Drescher, Gerson Laerson |
author_facet |
Drescher, Gerson Laerson |
author_role |
author |
dc.contributor.none.fl_str_mv |
Silva, Leandro Souza da http://lattes.cnpq.br/2152888530643357 Carlos, Filipe Selau http://lattes.cnpq.br/1071521284494576 Brunetto, Gustavo http://lattes.cnpq.br/1185169003700830 Ferreira, Paulo Ademar Avelar http://lattes.cnpq.br/1871733582967061 Scivittaro, Walkyria Bueno http://lattes.cnpq.br/7090419604571199 |
dc.contributor.author.fl_str_mv |
Drescher, Gerson Laerson |
dc.subject.por.fl_str_mv |
Análise do solo Balanço nutricional Fertilizante nitrogenado Matéria orgânica Oryza sativa L. Recuperação de 15N Soil analysis Nutritional balance Nitrogen fertilizer Organic matter 15N recovery CNPQ::CIENCIAS AGRARIAS::AGRONOMIA::CIENCIA DO SOLO |
topic |
Análise do solo Balanço nutricional Fertilizante nitrogenado Matéria orgânica Oryza sativa L. Recuperação de 15N Soil analysis Nutritional balance Nitrogen fertilizer Organic matter 15N recovery CNPQ::CIENCIAS AGRARIAS::AGRONOMIA::CIENCIA DO SOLO |
description |
Rice is an important food source for the world's population and is a substantial crop for Southern Brazil economic development. Nitrogen (N) is one of the most limiting nutrients for rice crop production, and the current N fertilizer recommendation for rice in Southern Brazil is based on soil organic matter (SOM) content at the 0-20 cm layer. However, the recommended N rates are very close for the different SOM classes and there is not always a yield increase by adding fertilizer. In flooded soils, the water input affects the dynamics of SOM decomposition and the N cycle, making it more difficult to predict the N rate based only on SOM content. More accurate N availability indexes, the N evaluation in soil profile and its recovery by rice plants, as well as the effect of N from greater soil depths on rice root morphology can help to improve our understanding on the nutrient dynamics in this production system, while contributing to improve the crop N fertilizer recommendation. This work aims to broaden our understanding of N dynamics in areas cultivated with rice and its relationship with soil properties, as well as identifying the capacity of plants to use N available at greater soil depths. A study was conducted to evaluate the total content and the amount of clay fixed ammonium (CF-NH4) extracted by the Nitrogen Soil Test for Rice (N-STaR) in soils from Arkansas, United States. In soils from southern Brazil, we evaluate the alkaline hydrolyzable N (AH-N) distribution in soil profile and its relationship with soil properties; we investigated the rice N recovery and absorption dynamics from different soil depths; and the effect of N from different soil depths on rice root growth and plant nutrition was also evaluated. The CF-NH4 represents 24.8 and 28.1% of the total N content at the 0-15 and 15-30 cm layers respectively, and the N-STaR estimates that a small proportion (<15%) of this N pool is plant available. These results indicate that CF-NH4 is an important soil N pool and might be a primary N source for rice crop. The AH-N distribution in soil profile is distinct between soils and can have increments in depth. Although granulometric fractions are strongly correlated with AH-N content for some soils, the total N is the major variable dictating AH-N distribution in soil profile. Rice effectively uses available N from depths of up to 45 cm and N recovery is affected by soil physical properties, especially hydraulic conductivity. Higher 15N recovery and N derived from fertilizer occurred when N was applied at the 10, 20 and 30 cm depths, which indicates that the N application in subsurface can increase the nutrient use efficiency by rice crop. The N availability in depth increased the root length, root surface area, and root volume while reducing the root average diameter. The N located at the soil superficial layers is absorbed by the plants in more responsive stages to fertilization, resulting in greater dry mass production. The N located at 30 and 45 cm contributed to plant nutrition at the reproductive stage, increasing the 15N content in the index leaves, the N content in tissue, the chlorophyll content, the photosynthesis rate and the carboxylation efficiency by Rubisco at rice heading. The N available in greater depths than 20 cm contributes to plant nutrition and should be considered in future studies involving the prediction and calibration of N availability indexes for flooded rice. |
publishDate |
2019 |
dc.date.none.fl_str_mv |
2019-01-25 2020-12-29T10:21:38Z 2020-12-29T10:21:38Z |
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/1/20234 |
dc.identifier.dark.fl_str_mv |
ark:/26339/001300000gggq |
url |
http://repositorio.ufsm.br/handle/1/20234 |
identifier_str_mv |
ark:/26339/001300000gggq |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.rights.driver.fl_str_mv |
Attribution-NonCommercial-NoDerivatives 4.0 International http://creativecommons.org/licenses/by-nc-nd/4.0/ info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Attribution-NonCommercial-NoDerivatives 4.0 International http://creativecommons.org/licenses/by-nc-nd/4.0/ |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidade Federal de Santa Maria Brasil Agronomia UFSM Programa de Pós-Graduação em Ciência do Solo Centro de Ciências Rurais |
publisher.none.fl_str_mv |
Universidade Federal de Santa Maria Brasil Agronomia UFSM Programa de Pós-Graduação em Ciência do Solo Centro de Ciências Rurais |
dc.source.none.fl_str_mv |
reponame:Manancial - Repositório Digital da UFSM instname:Universidade Federal de Santa Maria (UFSM) instacron:UFSM |
instname_str |
Universidade Federal de Santa Maria (UFSM) |
instacron_str |
UFSM |
institution |
UFSM |
reponame_str |
Manancial - Repositório Digital da UFSM |
collection |
Manancial - Repositório Digital da UFSM |
repository.name.fl_str_mv |
Manancial - Repositório Digital da UFSM - Universidade Federal de Santa Maria (UFSM) |
repository.mail.fl_str_mv |
atendimento.sib@ufsm.br||tedebc@gmail.com |
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1815172339118112768 |