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Biblioteca(s): |
Embrapa Agrobiologia; Embrapa Arroz e Feijão; Embrapa Solos. |
Data corrente: |
30/01/2006 |
Data da última atualização: |
14/05/2022 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
MADARI, B. E.; REEVES, J. B.; COELHO, M. R.; MACHADO, P. L. O. A.; DE-POLLI, H.; COELHO, R. M.; BENITES, V. M.; SOUZA, L. F.; McCARTY, G. W. |
Afiliação: |
BEATA EMOKE MADARI, CNPAF; JAMES B. REEVES, USDA; MAURICIO RIZZATO COELHO, CNPS; PEDRO LUIZ OLIVEIRA DE A MACHADO, CNPAF; HELVECIO DE POLLI, CNPAB; RICARDO M. COELHO, IAC; VINICIUS DE MELO BENITES, CNPS; LUCAS F. SOUZA; GREGORY W. MCCARTY, USDA. |
Título: |
Mid- and near-infrared spectroscopic determination of carbon in a diverse set of soils from the Brazilian national soil collection. |
Ano de publicação: |
2005 |
Fonte/Imprenta: |
Spectroscopy Letters, v. 38, n. 6, p. 721-740, 2005. |
DOI: |
https://doi.org/10.1080/00387010500315876 |
Idioma: |
Inglês |
Conteúdo: |
Calibrations for soil carbon content measured by combustion (total carbon, TC) and chromate oxidation by a modified Walkley-Black method (Walkley-Black carbon, WBC) from the Brazilian National Soil Collection were made using Fourier-transform near (1100 to 2500 nm; NIRS) and mid-infrared diffuse reflectance (2,500 to 25,000 nm; DRIFTS) spectroscopy combined with partial least squares (PLS). Calibration sets of sample populations of different carbon ranges, soil taxonomic classes, and soil textural groups were established. These are for TC ranges between 0.4 to 555.0, 0.4 to 99.1, and 0.4 to 39.9 g kg21: for WBC 0.2 to 401.0, 0.2 to 66.0, and 0.2 to 66.0, and 0.2 to 30.0 g kg21: for soil taxonomic classes Ferralsols and Acrisols; and for soil textural groups very clayey, clayey, and medium textures were examined. Calibrations obtained for the largest TC and WBC ranges were better compared to the lower ones, but lower root mean squared deviation (RMSD) and relative difference (RD ¼ RMSD/mean value) were found for the lower carbon ranges. Taxonomic soil class was not an adequate criterium for calibration set formation. Soil texture had effect on calibrations, especially using NIR, because of the particle size effect to which NIR was more sensitive than mid-IR. In general, DRIFTS showed better performance than NIRS. NIRS only outperformed DRIFTS when used with calibration set fairly homogeneous in its particle size distribution. Results demonstrated that while calibrations can be developed using either DRIFTS or NIRS for even a very diverse set of soil samples, which will determine C over a wide range of concentrations inherent in such a diverse set, it is desirable to seperate sample populations by soil textural properties and choose the adequate spectral range (NIR or mid-IR) based on the textural group, for calibration development to achieve more accurate results. MenosCalibrations for soil carbon content measured by combustion (total carbon, TC) and chromate oxidation by a modified Walkley-Black method (Walkley-Black carbon, WBC) from the Brazilian National Soil Collection were made using Fourier-transform near (1100 to 2500 nm; NIRS) and mid-infrared diffuse reflectance (2,500 to 25,000 nm; DRIFTS) spectroscopy combined with partial least squares (PLS). Calibration sets of sample populations of different carbon ranges, soil taxonomic classes, and soil textural groups were established. These are for TC ranges between 0.4 to 555.0, 0.4 to 99.1, and 0.4 to 39.9 g kg21: for WBC 0.2 to 401.0, 0.2 to 66.0, and 0.2 to 66.0, and 0.2 to 30.0 g kg21: for soil taxonomic classes Ferralsols and Acrisols; and for soil textural groups very clayey, clayey, and medium textures were examined. Calibrations obtained for the largest TC and WBC ranges were better compared to the lower ones, but lower root mean squared deviation (RMSD) and relative difference (RD ¼ RMSD/mean value) were found for the lower carbon ranges. Taxonomic soil class was not an adequate criterium for calibration set formation. Soil texture had effect on calibrations, especially using NIR, because of the particle size effect to which NIR was more sensitive than mid-IR. In general, DRIFTS showed better performance than NIRS. NIRS only outperformed DRIFTS when used with calibration set fairly homogeneous in its particle size distribution. Results demonstrated that while calibrations can b... Mostrar Tudo |
Palavras-Chave: |
DRIFTS; Mid-infrared; Near-infrared; NIRS; PLS. |
Thesagro: |
Carbono; Solo. |
Thesaurus Nal: |
carbon; chemometrics; soil. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
Marc: |
LEADER 02877naa a2200349 a 4500 001 1213859 005 2022-05-14 008 2005 bl uuuu u00u1 u #d 024 7 $ahttps://doi.org/10.1080/00387010500315876$2DOI 100 1 $aMADARI, B. E. 245 $aMid- and near-infrared spectroscopic determination of carbon in a diverse set of soils from the Brazilian national soil collection.$h[electronic resource] 260 $c2005 520 $aCalibrations for soil carbon content measured by combustion (total carbon, TC) and chromate oxidation by a modified Walkley-Black method (Walkley-Black carbon, WBC) from the Brazilian National Soil Collection were made using Fourier-transform near (1100 to 2500 nm; NIRS) and mid-infrared diffuse reflectance (2,500 to 25,000 nm; DRIFTS) spectroscopy combined with partial least squares (PLS). Calibration sets of sample populations of different carbon ranges, soil taxonomic classes, and soil textural groups were established. These are for TC ranges between 0.4 to 555.0, 0.4 to 99.1, and 0.4 to 39.9 g kg21: for WBC 0.2 to 401.0, 0.2 to 66.0, and 0.2 to 66.0, and 0.2 to 30.0 g kg21: for soil taxonomic classes Ferralsols and Acrisols; and for soil textural groups very clayey, clayey, and medium textures were examined. Calibrations obtained for the largest TC and WBC ranges were better compared to the lower ones, but lower root mean squared deviation (RMSD) and relative difference (RD ¼ RMSD/mean value) were found for the lower carbon ranges. Taxonomic soil class was not an adequate criterium for calibration set formation. Soil texture had effect on calibrations, especially using NIR, because of the particle size effect to which NIR was more sensitive than mid-IR. In general, DRIFTS showed better performance than NIRS. NIRS only outperformed DRIFTS when used with calibration set fairly homogeneous in its particle size distribution. Results demonstrated that while calibrations can be developed using either DRIFTS or NIRS for even a very diverse set of soil samples, which will determine C over a wide range of concentrations inherent in such a diverse set, it is desirable to seperate sample populations by soil textural properties and choose the adequate spectral range (NIR or mid-IR) based on the textural group, for calibration development to achieve more accurate results. 650 $acarbon 650 $achemometrics 650 $asoil 650 $aCarbono 650 $aSolo 653 $aDRIFTS 653 $aMid-infrared 653 $aNear-infrared 653 $aNIRS 653 $aPLS 700 1 $aREEVES, J. B. 700 1 $aCOELHO, M. R. 700 1 $aMACHADO, P. L. O. A. 700 1 $aDE-POLLI, H. 700 1 $aCOELHO, R. M. 700 1 $aBENITES, V. M. 700 1 $aSOUZA, L. F. 700 1 $aMcCARTY, G. W. 773 $tSpectroscopy Letters$gv. 38, n. 6, p. 721-740, 2005.
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1. | | BARRETTI, P. B.; FARIA, C. C. M. D. R.; CAMPOS, V. P.; SOUZA, R. M. de; CASTRO, J. M.; MOURA, B.; BETTIOL, W. Efeito de filtrado de culturas bacterianas do lodo de esgoto na eclosão, mobilidade e mortalidade de juvenis de segundo sstádio de meloidogyne javanica. Fitopatologia Brasileira, Brasília, v. 29, p. 100, ago. 2004. Suplemento. R 261. Edição de Resumos do 37 Congresso Brasileiro de Fitopatologia, ago. 2004. p S231Tipo: Resumo em Anais de Congresso |
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