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Registro Completo |
Biblioteca(s): |
Embrapa Solos. |
Data corrente: |
31/10/2024 |
Data da última atualização: |
22/01/2025 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
NOVOTNY, E. H.; AZEVEDO, E. R. de; WANG, J.; MCCARNEY, E.; GALVOSAS, P. |
Afiliação: |
ETELVINO HENRIQUE NOVOTNY, CNPS; EDUARDO RIBEIRO DE AZEVEDO, UNIVERSIDADE DE SÃO PAULO; JIE WANG, VICTORIA UNIVERSITY WELLINGTON; EVAN MCCARNEY, KORIMAKO CHEMICAL; PETRIK GALVOSAS, VICTORIA UNIVERSITY WELLINGTON. |
Título: |
Solid-state nuclear magnetic resonance at low-field as an approach for fertiliser dissolution monitoring. |
Ano de publicação: |
2025 |
Fonte/Imprenta: |
Biology and Fertility of Soils, v. 61, n. 1, p. 177-185, Jan. 2025. |
DOI: |
https://doi.org/10.1007/s00374-024-01876-z |
Idioma: |
Inglês |
Conteúdo: |
The dissolution of fertilisers is the initial process that takes place in soils following fertiliser application and influences the fate and effectiveness of fertilisers. Currently, there are only a few methods for studying fertiliser dissolution in soil. These approaches typically do not accurately represent real soil-fertiliser systems and are susceptible to errors, since they are influenced by processes associated with the loss or retention of the trace ions of the fertiliser. Low field NMR or time-domain NMR (1H-TDNMR) is typically employed for studying 1H in fluids (or mobile 1H), however, special pulse sequences enable the selective detection of 1H in solids. Furthermore, it is possible to filter out undesired signals like 1H from minerals and from soil organic matter. This allows for the detection and monitoring of 1H only from protonated fertilisers (e.g., ammonia, (di)-hydrogen phosphates, etc.). The aim of this study is to present an efficient procedure which monitors the dissolution of fertilisers in soils using 1H-TDNMR. For this, six contrasting New Zealand soils and four protonated fertilisers - NH4Cl, NH4NO3, NaH2PO4.H2O, and (NH4)2HPO4 - were utilised. The proposed method efficiently, accurately, and precisely, monitored the dissolution of the studied fertilisers in all the tested soils under different rain regimes, from violent rain (60 mm h− 1) to light rain (2 mm h− 1) with a time interval (temporal resolution) as short as 5 s. |
Palavras-Chave: |
Dissolution kinetic; Fertiliser; Low-field NMR; Time domain NMR. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
Marc: |
LEADER 02200naa a2200229 a 4500 001 2168674 005 2025-01-22 008 2025 bl uuuu u00u1 u #d 024 7 $ahttps://doi.org/10.1007/s00374-024-01876-z$2DOI 100 1 $aNOVOTNY, E. H. 245 $aSolid-state nuclear magnetic resonance at low-field as an approach for fertiliser dissolution monitoring.$h[electronic resource] 260 $c2025 520 $aThe dissolution of fertilisers is the initial process that takes place in soils following fertiliser application and influences the fate and effectiveness of fertilisers. Currently, there are only a few methods for studying fertiliser dissolution in soil. These approaches typically do not accurately represent real soil-fertiliser systems and are susceptible to errors, since they are influenced by processes associated with the loss or retention of the trace ions of the fertiliser. Low field NMR or time-domain NMR (1H-TDNMR) is typically employed for studying 1H in fluids (or mobile 1H), however, special pulse sequences enable the selective detection of 1H in solids. Furthermore, it is possible to filter out undesired signals like 1H from minerals and from soil organic matter. This allows for the detection and monitoring of 1H only from protonated fertilisers (e.g., ammonia, (di)-hydrogen phosphates, etc.). The aim of this study is to present an efficient procedure which monitors the dissolution of fertilisers in soils using 1H-TDNMR. For this, six contrasting New Zealand soils and four protonated fertilisers - NH4Cl, NH4NO3, NaH2PO4.H2O, and (NH4)2HPO4 - were utilised. The proposed method efficiently, accurately, and precisely, monitored the dissolution of the studied fertilisers in all the tested soils under different rain regimes, from violent rain (60 mm h− 1) to light rain (2 mm h− 1) with a time interval (temporal resolution) as short as 5 s. 653 $aDissolution kinetic 653 $aFertiliser 653 $aLow-field NMR 653 $aTime domain NMR 700 1 $aAZEVEDO, E. R. de 700 1 $aWANG, J. 700 1 $aMCCARNEY, E. 700 1 $aGALVOSAS, P. 773 $tBiology and Fertility of Soils$gv. 61, n. 1, p. 177-185, Jan. 2025.
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1. |  | RYBKA, A. C. P.; SOUZA, F. de F.; DEON, M. D. I.; ALMEIDA, L. C. P.; LIMA, M. A. C. de; CASTRO, J. M. da C. e. Análise sensorial do suco de aceroleiras do Banco Ativo de Germoplasma da Embrapa Semiárido. In: CONGRESSO BRASILEIRO DE FRUTICULTURA, 22., 2012, Bento Gonçalves. Anais... Bento Gonçalves: SBF, 2012. 1 CD-ROM.Tipo: Artigo em Anais de Congresso |
Biblioteca(s): Embrapa Semiárido. |
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2. |  | SILVA, W. T. L. DA; HANEDA, R. N.; NOVAES, A. P. DE; MILORI, D. M. P.; MARTIN-NETO, L. SIMÕES, M. L.; FIALHO, L. L.; CAMPOS, J. B. DE; ANDERAÓS NETO, N.; NAJM FILHO, M.; ALMEIDA, L. C. P. DE; SILVEIRA, D. Humidification degree of fermentated urban residues determined by chemical and spectroscopic methods. In: INTERNATIONAL MEETING OF INTERNATIONAL HUMIC SUBSTANCES SOCIETY. -- IHSS, 12, São Pedro, SP, 2004. Humic substances and soil and water environment. Abstracts...[São Carlos], SP: Embrapa Instrumentação Agropecuária, 2004. p. 107. O nome correto de um dos autores é MILORI, D. M. B. P.Biblioteca(s): Embrapa Instrumentação. |
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3. |  | SILVA, W. T. L. da; HANEDA, R. N.; NOVAES, A. P. de; SIMOES, M. L.; FIALHO, L. L.; MILORI, D. M. B. P.; MARTIN-NETO, L.; CAMPOS, J. B. de ANDERÁOS NETO, N.; NAJM FILHO, M.; ALMEIDA, L. C. P. de; SILVEIRA, D. Humification degree of fermentated urban residues determined by chemical and spectroscopic methods. In: MARTIN-NETO, L.; MILORI, D.M.B.P.; SILVA, W.T.L. (Ed.). Humic substances and soil and water environment: International Meeting of IHSS, 12. São Carlos : Embrapa Instrumentação Agropecuária, 2004. p. 550-553. CLASSIFICAÇÃO CDD: 630Biblioteca(s): Embrapa Instrumentação. |
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