Caracterização analítica de rochas silicatadas e avaliação de seu potencial agrícola como fonte de potássio

Detalhes bibliográficos
Autor(a) principal: Penha, Maria da Natividade Chagas
Data de Publicação: 2016
Tipo de documento: Dissertação
Idioma: por
Título da fonte: Repositório Institucional da UFSCAR
Texto Completo: https://repositorio.ufscar.br/handle/ufscar/8471
Resumo: This study evaluated the agronomic efficiency of application of powder of silicate rocks as potassium sources in consecutive crops of millet and alfalfa in a greenhouse experiment. The rocks Biotite Schist (BX), Syenite Ceraima (TA15), Mafurito Acreuna (TA21), Syenite SANW (TA20), Biotite Gneiss (EL02), and Phonolite Curimbaba (FN) were applied as slowreleased potassium sources in three doses 1.25; 2.50; and 5.0 g kg-1 of ground rock. Potassium chloride was used as standard fertilizer in doses of 0.10; 0,20; and 0.40 g of KCl kg-1 of soil. The soil used in the experiments was a Latosol, with 1.2 mmol dm-3 of potassium content. The TA21 rock was tested with and without soil acidity correction (TA21WL). In order to evaluate the rocks K reliase, five consecutive crops were performed: (1) millet (62 days of planting); (2), (3) and (4) Alfalfa (80, 115 and 155 days of planting, respectively), and (5) with 80 days of planting. The dry matter yield in the alfalfa was significantly lower than that millet cultivation. The forage samples were HNO3 + H2O2 microwave assisted digested for K determining content. The samples of rocks were characterized by X-ray fluorescence, X-ray diffraction, scanning electron microscopy and particle size distribution. Afterward, extraction experiments with Mehlich 1, and different extraction times of acetic acid and fumaric acid 0.05mol L-1 were performed. Aluminium, Ca, K, Mg, Mn, Na, P, and Zn were quantified by inductively coupled plasma optical emission spectrometry (ICP OES) in all the obtained extracts. The method of ion exchange resin was also applied to evaluated the rocks, and K, Ca, Mg, and P were quantified. Potassium soluble was determined by flame photometry after extraction with hot water, according to with the Brazilian Ministry of Agriculture, Livestock and Supply (MAPA) official method. For drastic extraction, two microwave assisted decomposition methods were evaluated: aqua regia and reversed aqua regia with H2O2. Aluminiun, Ca, K, Mg, Mn, Na, and Zn were quantified by ICP OES and the results, compared by using the paired t-test, presented no significant difference between the decomposition methods in the 95% range of confidence. The correlation between the extractors, the nutrients plants amount, and agronomic efficiency was evaluated from the extraction obtained concentrations and the amount of extracted potassium in crops. The use of lime in soils that received the addition of TA21 rock significantly influenced the absorption of potassium and was no effect on the release of K only when this rock was added to the soil without prior liming.treatment. The decreasing order of potassium extraction efficiency, considering the total applied in treatments and K extracted by plants was EL02> TA21-SC> KCl> FN> BX> TA20> TA15> TA21. The two developed decomposition methods showed a better correlation with potassium extracted from the EL02 rocks. The greenhouse study corroborated the extraction tests performed in the laboratory, which indicated that the EL02 rock is the one with the highest percentage of K release compared with the other evaluated rocks.
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spelling Penha, Maria da Natividade ChagasNogueira, Ana Rita de Araújohttp://lattes.cnpq.br/7034773971317045http://lattes.cnpq.br/3058538599121106997f29cb-ef72-464e-80f1-6e476997cd452017-02-06T18:47:25Z2017-02-06T18:47:25Z2016-04-19PENHA, Maria da Natividade Chagas. Caracterização analítica de rochas silicatadas e avaliação de seu potencial agrícola como fonte de potássio. 2016. Dissertação (Mestrado em Química) – Universidade Federal de São Carlos, São Carlos, 2016. Disponível em: https://repositorio.ufscar.br/handle/ufscar/8471.https://repositorio.ufscar.br/handle/ufscar/8471This study evaluated the agronomic efficiency of application of powder of silicate rocks as potassium sources in consecutive crops of millet and alfalfa in a greenhouse experiment. The rocks Biotite Schist (BX), Syenite Ceraima (TA15), Mafurito Acreuna (TA21), Syenite SANW (TA20), Biotite Gneiss (EL02), and Phonolite Curimbaba (FN) were applied as slowreleased potassium sources in three doses 1.25; 2.50; and 5.0 g kg-1 of ground rock. Potassium chloride was used as standard fertilizer in doses of 0.10; 0,20; and 0.40 g of KCl kg-1 of soil. The soil used in the experiments was a Latosol, with 1.2 mmol dm-3 of potassium content. The TA21 rock was tested with and without soil acidity correction (TA21WL). In order to evaluate the rocks K reliase, five consecutive crops were performed: (1) millet (62 days of planting); (2), (3) and (4) Alfalfa (80, 115 and 155 days of planting, respectively), and (5) with 80 days of planting. The dry matter yield in the alfalfa was significantly lower than that millet cultivation. The forage samples were HNO3 + H2O2 microwave assisted digested for K determining content. The samples of rocks were characterized by X-ray fluorescence, X-ray diffraction, scanning electron microscopy and particle size distribution. Afterward, extraction experiments with Mehlich 1, and different extraction times of acetic acid and fumaric acid 0.05mol L-1 were performed. Aluminium, Ca, K, Mg, Mn, Na, P, and Zn were quantified by inductively coupled plasma optical emission spectrometry (ICP OES) in all the obtained extracts. The method of ion exchange resin was also applied to evaluated the rocks, and K, Ca, Mg, and P were quantified. Potassium soluble was determined by flame photometry after extraction with hot water, according to with the Brazilian Ministry of Agriculture, Livestock and Supply (MAPA) official method. For drastic extraction, two microwave assisted decomposition methods were evaluated: aqua regia and reversed aqua regia with H2O2. Aluminiun, Ca, K, Mg, Mn, Na, and Zn were quantified by ICP OES and the results, compared by using the paired t-test, presented no significant difference between the decomposition methods in the 95% range of confidence. The correlation between the extractors, the nutrients plants amount, and agronomic efficiency was evaluated from the extraction obtained concentrations and the amount of extracted potassium in crops. The use of lime in soils that received the addition of TA21 rock significantly influenced the absorption of potassium and was no effect on the release of K only when this rock was added to the soil without prior liming.treatment. The decreasing order of potassium extraction efficiency, considering the total applied in treatments and K extracted by plants was EL02> TA21-SC> KCl> FN> BX> TA20> TA15> TA21. The two developed decomposition methods showed a better correlation with potassium extracted from the EL02 rocks. The greenhouse study corroborated the extraction tests performed in the laboratory, which indicated that the EL02 rock is the one with the highest percentage of K release compared with the other evaluated rocks.O presente estudo avaliou a eficiência agronômica da aplicação de pó de rochas silicatadas como fonte de potássio em cultivos consecutivos de milheto e alfafa em casa de vegetação. As rochas Biotita Xisto (BX), Sienito Ceraíma (TA15), Mafurito Acreúna (TA21), Sienito SANW (TA20), Biotita Gnaísse (EL02) e Fonolito Curimbaba (FN) foram aplicadas como fontes de potássio de liberação lenta em três doses de 1,25; 2,50 e 5,0 g de rocha moída por kg de solo. Cloreto de potássio foi utilizado como fertilizante convencional em doses de 0,10; 0,20 e 0,40 g de KCl kg-1 de solo. O solo utilizado nos experimentos foi um latossolo amarelo distrófico de textura média, com teor de potássio de 1,2 mmolc dm-3 solo. A rocha TA21 foi testada sem e com correção da acidez do solo. Com a finalidade de observar a dissolução das rochas em um ambiente com plantas foram realizados cinco cultivos consecutivos: (1) milheto (62 dias de cultivo); (2), (3) e (4) alfafa (80, 115 e 155 dias de cultivo, respectivamente) e (5) milheto, com 80 dias de cultivo. A produção de matéria seca no cultivo da alfafa foi significativamente menor do que o cultivo do milheto. As amostras de forrageira foram digeridas e quantificadas empregando o método de decomposição assistida por radiação micro-ondas com HNO3 + H2O2 para a determinação do teor de potássio extraído pelas plantas. As amostras de rochas foram caracterizadas por fluorescência de raios X, difração de raios X, microscopia eletrônica de varredura e distribuição de tamanho das partículas e submetidas a ensaios com solução extratora Mehlich-1, ácido acético e ácido fumárico 0,05mol L-1, em diferentes tempos de extração. Todos os extratos foram quantificados por espectrometria de emissão óptica com plasma acoplado indutivamente (ICP OES), sendo determinados os teores de Al, Ca, K, Mg, Mn, Na, P e Zn. O método da resina trocadora de íons foi aplicado para todas as amostras de rochas avaliadas, sendo quantificados K, Ca, Mg e P. Potássio solúvel foi determinado por fotometria de chama após extração com água quente, método oficial do Ministério da Agricultura, Pecuária e Abastecimento (MAPA). Para extração drástica foram avaliados dois métodos de decomposição assistida por radiação microondas: com uso de água régia e água régia invertida com adição de H2O2 e 2 etapas de pré-decomposição. Os elementos Al, Ca, K, Mg, Mn, Na e Zn foram quantificados por ICP OES e os resultados obtidos foram comparados por meio do teste t pareado, que indicou não haver diferença significativa entre os métodos de decomposição no intervalo de 95% de confiança. A partir das concentrações obtidas nas extrações e da quantidade de potássio extraída nos cultivos foi realizado o cálculo de correlação entre os extratores e as plantas, considerando a eficiência agronômica. O uso da calagem nos solos que receberam adição da rocha TA21 influenciou significativamente a absorção de potássio, sendo que foi observado efeito relativo à liberação de K apenas quando essa rocha foi adicionada ao solo sem tratamento prévio com a calagem. A ordem decrescente de eficiência de extração de potássio, considerando o total aplicado nos tratamentos e o K extraído pelas plantas foi EL02 > TA21-SC > KCl > FN> BX> TA20 > TA15 > TA21. Os dois métodos de decomposição desenvolvidos apresentaram melhor correlação com o potássio extraído das rochas EL02. O estudo de casa de vegetação corroborou com os ensaios de extração realizados em laboratório, que indicaram que a rocha EL02 é a que possui o maior percentual de liberação de K em relação às demais rochas avaliadas.Não recebi financiamentoporUniversidade Federal de São CarlosCâmpus São CarlosPrograma de Pós-Graduação em Química - PPGQUFSCarMétodos de extraçãoPotássioRochagemEficiência agronômicaMethods of extractionPotassiumStonemealAgronomic efficiencyCIENCIAS EXATAS E DA TERRA::QUIMICA::QUIMICA ANALITICA::ANALISE DE TRACOS E QUIMICA AMBIENTALCaracterização analítica de rochas silicatadas e avaliação de seu potencial agrícola como fonte de potássioinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesisOnline600600e83fd9a0-c0d6-4518-b677-9aa885aeffbcinfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da UFSCARinstname:Universidade Federal de São Carlos (UFSCAR)instacron:UFSCARORIGINALDissMNCP.pdfDissMNCP.pdfapplication/pdf2950899https://repositorio.ufscar.br/bitstream/ufscar/8471/1/DissMNCP.pdf29259d512afa24d2a17d6f5c8569f612MD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81957https://repositorio.ufscar.br/bitstream/ufscar/8471/2/license.txtae0398b6f8b235e40ad82cba6c50031dMD52TEXTDissMNCP.pdf.txtDissMNCP.pdf.txtExtracted texttext/plain155764https://repositorio.ufscar.br/bitstream/ufscar/8471/3/DissMNCP.pdf.txt86534c62f0b4d71b05eda14f11d815b2MD53THUMBNAILDissMNCP.pdf.jpgDissMNCP.pdf.jpgIM Thumbnailimage/jpeg9428https://repositorio.ufscar.br/bitstream/ufscar/8471/4/DissMNCP.pdf.jpg7408389f374aceb4c2dba057fa7bb8b0MD54ufscar/84712023-09-18 18:31:07.838oai:repositorio.ufscar.br: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Repositório InstitucionalPUBhttps://repositorio.ufscar.br/oai/requestopendoar:43222023-09-18T18:31:07Repositório Institucional da UFSCAR - Universidade Federal de São Carlos (UFSCAR)false
dc.title.por.fl_str_mv Caracterização analítica de rochas silicatadas e avaliação de seu potencial agrícola como fonte de potássio
title Caracterização analítica de rochas silicatadas e avaliação de seu potencial agrícola como fonte de potássio
spellingShingle Caracterização analítica de rochas silicatadas e avaliação de seu potencial agrícola como fonte de potássio
Penha, Maria da Natividade Chagas
Métodos de extração
Potássio
Rochagem
Eficiência agronômica
Methods of extraction
Potassium
Stonemeal
Agronomic efficiency
CIENCIAS EXATAS E DA TERRA::QUIMICA::QUIMICA ANALITICA::ANALISE DE TRACOS E QUIMICA AMBIENTAL
title_short Caracterização analítica de rochas silicatadas e avaliação de seu potencial agrícola como fonte de potássio
title_full Caracterização analítica de rochas silicatadas e avaliação de seu potencial agrícola como fonte de potássio
title_fullStr Caracterização analítica de rochas silicatadas e avaliação de seu potencial agrícola como fonte de potássio
title_full_unstemmed Caracterização analítica de rochas silicatadas e avaliação de seu potencial agrícola como fonte de potássio
title_sort Caracterização analítica de rochas silicatadas e avaliação de seu potencial agrícola como fonte de potássio
author Penha, Maria da Natividade Chagas
author_facet Penha, Maria da Natividade Chagas
author_role author
dc.contributor.authorlattes.por.fl_str_mv http://lattes.cnpq.br/3058538599121106
dc.contributor.author.fl_str_mv Penha, Maria da Natividade Chagas
dc.contributor.advisor1.fl_str_mv Nogueira, Ana Rita de Araújo
dc.contributor.advisor1Lattes.fl_str_mv http://lattes.cnpq.br/7034773971317045
dc.contributor.authorID.fl_str_mv 997f29cb-ef72-464e-80f1-6e476997cd45
contributor_str_mv Nogueira, Ana Rita de Araújo
dc.subject.por.fl_str_mv Métodos de extração
Potássio
Rochagem
Eficiência agronômica
topic Métodos de extração
Potássio
Rochagem
Eficiência agronômica
Methods of extraction
Potassium
Stonemeal
Agronomic efficiency
CIENCIAS EXATAS E DA TERRA::QUIMICA::QUIMICA ANALITICA::ANALISE DE TRACOS E QUIMICA AMBIENTAL
dc.subject.eng.fl_str_mv Methods of extraction
Potassium
Stonemeal
Agronomic efficiency
dc.subject.cnpq.fl_str_mv CIENCIAS EXATAS E DA TERRA::QUIMICA::QUIMICA ANALITICA::ANALISE DE TRACOS E QUIMICA AMBIENTAL
description This study evaluated the agronomic efficiency of application of powder of silicate rocks as potassium sources in consecutive crops of millet and alfalfa in a greenhouse experiment. The rocks Biotite Schist (BX), Syenite Ceraima (TA15), Mafurito Acreuna (TA21), Syenite SANW (TA20), Biotite Gneiss (EL02), and Phonolite Curimbaba (FN) were applied as slowreleased potassium sources in three doses 1.25; 2.50; and 5.0 g kg-1 of ground rock. Potassium chloride was used as standard fertilizer in doses of 0.10; 0,20; and 0.40 g of KCl kg-1 of soil. The soil used in the experiments was a Latosol, with 1.2 mmol dm-3 of potassium content. The TA21 rock was tested with and without soil acidity correction (TA21WL). In order to evaluate the rocks K reliase, five consecutive crops were performed: (1) millet (62 days of planting); (2), (3) and (4) Alfalfa (80, 115 and 155 days of planting, respectively), and (5) with 80 days of planting. The dry matter yield in the alfalfa was significantly lower than that millet cultivation. The forage samples were HNO3 + H2O2 microwave assisted digested for K determining content. The samples of rocks were characterized by X-ray fluorescence, X-ray diffraction, scanning electron microscopy and particle size distribution. Afterward, extraction experiments with Mehlich 1, and different extraction times of acetic acid and fumaric acid 0.05mol L-1 were performed. Aluminium, Ca, K, Mg, Mn, Na, P, and Zn were quantified by inductively coupled plasma optical emission spectrometry (ICP OES) in all the obtained extracts. The method of ion exchange resin was also applied to evaluated the rocks, and K, Ca, Mg, and P were quantified. Potassium soluble was determined by flame photometry after extraction with hot water, according to with the Brazilian Ministry of Agriculture, Livestock and Supply (MAPA) official method. For drastic extraction, two microwave assisted decomposition methods were evaluated: aqua regia and reversed aqua regia with H2O2. Aluminiun, Ca, K, Mg, Mn, Na, and Zn were quantified by ICP OES and the results, compared by using the paired t-test, presented no significant difference between the decomposition methods in the 95% range of confidence. The correlation between the extractors, the nutrients plants amount, and agronomic efficiency was evaluated from the extraction obtained concentrations and the amount of extracted potassium in crops. The use of lime in soils that received the addition of TA21 rock significantly influenced the absorption of potassium and was no effect on the release of K only when this rock was added to the soil without prior liming.treatment. The decreasing order of potassium extraction efficiency, considering the total applied in treatments and K extracted by plants was EL02> TA21-SC> KCl> FN> BX> TA20> TA15> TA21. The two developed decomposition methods showed a better correlation with potassium extracted from the EL02 rocks. The greenhouse study corroborated the extraction tests performed in the laboratory, which indicated that the EL02 rock is the one with the highest percentage of K release compared with the other evaluated rocks.
publishDate 2016
dc.date.issued.fl_str_mv 2016-04-19
dc.date.accessioned.fl_str_mv 2017-02-06T18:47:25Z
dc.date.available.fl_str_mv 2017-02-06T18:47:25Z
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 PENHA, Maria da Natividade Chagas. Caracterização analítica de rochas silicatadas e avaliação de seu potencial agrícola como fonte de potássio. 2016. Dissertação (Mestrado em Química) – Universidade Federal de São Carlos, São Carlos, 2016. Disponível em: https://repositorio.ufscar.br/handle/ufscar/8471.
dc.identifier.uri.fl_str_mv https://repositorio.ufscar.br/handle/ufscar/8471
identifier_str_mv PENHA, Maria da Natividade Chagas. Caracterização analítica de rochas silicatadas e avaliação de seu potencial agrícola como fonte de potássio. 2016. Dissertação (Mestrado em Química) – Universidade Federal de São Carlos, São Carlos, 2016. Disponível em: https://repositorio.ufscar.br/handle/ufscar/8471.
url https://repositorio.ufscar.br/handle/ufscar/8471
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dc.relation.confidence.fl_str_mv 600
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dc.relation.authority.fl_str_mv e83fd9a0-c0d6-4518-b677-9aa885aeffbc
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Universidade Federal de São Carlos
Câmpus São Carlos
dc.publisher.program.fl_str_mv Programa de Pós-Graduação em Química - PPGQ
dc.publisher.initials.fl_str_mv UFSCar
publisher.none.fl_str_mv Universidade Federal de São Carlos
Câmpus São Carlos
dc.source.none.fl_str_mv reponame:Repositório Institucional da UFSCAR
instname:Universidade Federal de São Carlos (UFSCAR)
instacron:UFSCAR
instname_str Universidade Federal de São Carlos (UFSCAR)
instacron_str UFSCAR
institution UFSCAR
reponame_str Repositório Institucional da UFSCAR
collection Repositório Institucional da UFSCAR
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MD5
MD5
repository.name.fl_str_mv Repositório Institucional da UFSCAR - Universidade Federal de São Carlos (UFSCAR)
repository.mail.fl_str_mv
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