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Registro Completo |
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Biblioteca(s): |
Embrapa Cerrados. |
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Data corrente: |
23/12/2016 |
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Data da última atualização: |
09/01/2017 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Autoria: |
OLIVEIRA, J. F. de; BROSSARD, M.; CORAZZA, E. J.; MARCHAO, R. L.; GUIMARÃES, M. de F. |
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Afiliação: |
José Francirlei de Oliveira, Universidade Estadual de Londrina; Michel Brossard, IRD (Institut de recherche pour le développement); EDEMAR JOAQUIM CORAZZA, SCT; ROBELIO LEANDRO MARCHAO, CPAC; Maria de Fátima Guimarães, Universidade Estadual de Londrina. |
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Título: |
Visible and near infrared spectra of Ferralsols according to their structural features. |
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Ano de publicação: |
2016 |
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Fonte/Imprenta: |
Journal of Near Infrared Spectroscopy, v. 24, n. 3, p. 243-254, March 2016. |
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DOI: |
https://doi.org/10.1255/jnirs.1202 |
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Idioma: |
Inglês |
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Conteúdo: |
ABSTRACT: In soil science, structural features of soils are an important attribute; soils can be characterised by proportional size distribution of aggregates and the pore space between and within those aggregates. The objective of this study was to evaluate the relationship between the visible and near infrared (Vis?NIR) spectra and microaggregates from a collection of Ferralsols. Our dataset consists of 56 spectra from seven soil profiles of kaolinitic and oxidic-gibbsitic Ferralsols. Soils were characterised according to their morphological features: those with a typical porous massive structure and those with a cohesive massive structure. Size distribution of five classes of microaggregate was determined (1000?2000 µm, 500?1000 µm, 250?500 µm, 105?250 µm and < 105?µm). From the soil spectra, we determined the CIE (Commission Internationale de l'Éclairage) red index (RICIE) and the absorption intensities of kaolinite (IKa) and gibbsite (IGb). The predominant fraction of microaggregates exhibited sizes between 250 and 1000µm (Φ250?1000). The proportional increase of this microaggregate class in the soils increased the scattering and variability of reflected light, particularly when soil samples showed more than 0.50 g g?1 of Φ250?1000. The microaggregate size explained over 55% of reflectance intensity variability of wavelengths in the vis?NIR regions, principally on reflectance intensity and concavity of the spectra at 436 nm, 546 nm and 2236 nm, which decreases with increased proportion of Φ250?1000. Thus, different structural features of Ferralsols can be directly evaluated through Vis?NIR spectroscopy, even in samples sieved through 2.00 mm. These results highlight the potential use of Vis?NIR spectroscopy in studies of soil classification, soil physical behaviour and soil physical fertility and environmental studies, principally by a new method of analysing bulk density and structure of soil directly from the soil spectra, without the need for predictive models. As well as spectra, RICIE,IKa and IGb can be used to characterise the different structural features of Ferralsols. MenosABSTRACT: In soil science, structural features of soils are an important attribute; soils can be characterised by proportional size distribution of aggregates and the pore space between and within those aggregates. The objective of this study was to evaluate the relationship between the visible and near infrared (Vis?NIR) spectra and microaggregates from a collection of Ferralsols. Our dataset consists of 56 spectra from seven soil profiles of kaolinitic and oxidic-gibbsitic Ferralsols. Soils were characterised according to their morphological features: those with a typical porous massive structure and those with a cohesive massive structure. Size distribution of five classes of microaggregate was determined (1000?2000 µm, 500?1000 µm, 250?500 µm, 105?250 µm and < 105?µm). From the soil spectra, we determined the CIE (Commission Internationale de l'Éclairage) red index (RICIE) and the absorption intensities of kaolinite (IKa) and gibbsite (IGb). The predominant fraction of microaggregates exhibited sizes between 250 and 1000µm (Φ250?1000). The proportional increase of this microaggregate class in the soils increased the scattering and variability of reflected light, particularly when soil samples showed more than 0.50 g g?1 of Φ250?1000. The microaggregate size explained over 55% of reflectance intensity variability of wavelengths in the vis?NIR regions, principally on reflectance intensity and concavity of the spectra at 436 nm, 546 nm and 2236 nm, which decreases... Mostrar Tudo |
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Palavras-Chave: |
Diffuse reflectance spectroscopy; Espectroscopia de refletância difusa; Latosol; Microped; Soil mineral; Solo mineral. |
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Thesagro: |
Estrutura do Solo; Latossolo. |
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Thesaurus Nal: |
Soil structure. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/152250/1/Oliveira-et-al-2016.pdf
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Marc: |
LEADER 03018naa a2200289 a 4500
001 2059216
005 2017-01-09
008 2016 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1255/jnirs.1202$2DOI
100 1 $aOLIVEIRA, J. F. de
245 $aVisible and near infrared spectra of Ferralsols according to their structural features.
260 $c2016
520 $aABSTRACT: In soil science, structural features of soils are an important attribute; soils can be characterised by proportional size distribution of aggregates and the pore space between and within those aggregates. The objective of this study was to evaluate the relationship between the visible and near infrared (Vis?NIR) spectra and microaggregates from a collection of Ferralsols. Our dataset consists of 56 spectra from seven soil profiles of kaolinitic and oxidic-gibbsitic Ferralsols. Soils were characterised according to their morphological features: those with a typical porous massive structure and those with a cohesive massive structure. Size distribution of five classes of microaggregate was determined (1000?2000 µm, 500?1000 µm, 250?500 µm, 105?250 µm and < 105?µm). From the soil spectra, we determined the CIE (Commission Internationale de l'Éclairage) red index (RICIE) and the absorption intensities of kaolinite (IKa) and gibbsite (IGb). The predominant fraction of microaggregates exhibited sizes between 250 and 1000µm (Φ250?1000). The proportional increase of this microaggregate class in the soils increased the scattering and variability of reflected light, particularly when soil samples showed more than 0.50 g g?1 of Φ250?1000. The microaggregate size explained over 55% of reflectance intensity variability of wavelengths in the vis?NIR regions, principally on reflectance intensity and concavity of the spectra at 436 nm, 546 nm and 2236 nm, which decreases with increased proportion of Φ250?1000. Thus, different structural features of Ferralsols can be directly evaluated through Vis?NIR spectroscopy, even in samples sieved through 2.00 mm. These results highlight the potential use of Vis?NIR spectroscopy in studies of soil classification, soil physical behaviour and soil physical fertility and environmental studies, principally by a new method of analysing bulk density and structure of soil directly from the soil spectra, without the need for predictive models. As well as spectra, RICIE,IKa and IGb can be used to characterise the different structural features of Ferralsols.
650 $aSoil structure
650 $aEstrutura do Solo
650 $aLatossolo
653 $aDiffuse reflectance spectroscopy
653 $aEspectroscopia de refletância difusa
653 $aLatosol
653 $aMicroped
653 $aSoil mineral
653 $aSolo mineral
700 1 $aBROSSARD, M.
700 1 $aCORAZZA, E. J.
700 1 $aMARCHAO, R. L.
700 1 $aGUIMARÃES, M. de F.
773 $tJournal of Near Infrared Spectroscopy$gv. 24, n. 3, p. 243-254, March 2016.
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Registro original: |
Embrapa Cerrados (CPAC) |
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| Registros recuperados : 73 | |
| 3. |  | SILVA, A. P.; BABUJIA, L. C.; MATSUMOTO, L. S.; GUIMARÃES, M. de F.; HUNGRIA, M. Bacterial diversity under different tillage and crop rotation systems. In: REUNIÃO BRASILEIRA DE FERTILIDADE DO SOLO E NUTRIÇÃO DE PLANTAS, 30.; REUNIÃO BRASILEIRA SOBRE MICORRIZAS, 14.; SIMPÓSIO BRASILEIRO DE MICROBIOLOGIA DO SOLO, 12.; REUNIÃO BRASILEIRA DE BIOLOGIA DO SOLO, 9.; SIMPÓSIO SOBRE SELÊNIO NO BRASIL, 1., 2012, Maceió. A responsabilidade socioambiental da pesquisa agrícola: anais. Viçosa: SBCS, 2012. 4 p. Trab. 1752. 1 CD-ROM. Fertbio.| Tipo: Artigo em Anais de Congresso |
| Biblioteca(s): Embrapa Soja. |
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| 6. | | CHIBEBA, A. M.; GUIMARAES, M. de F.; NOGUEIRA, M. A.; BOAHEN, S. K.; HUNGRIA, M. Characterization of indigenous rhizobia isolated from soybean [Glycine max (L.) Merrill] grown in mozambique. In: REUNIÃO LATINOAMERICANA DE RIZOBIOLOGIA - RELAR, 27., 2016, Londrina. Fortalecendo as parcerias Sul-Sul: anais. Curitiba: SBCS-NEPAR, 2016. p. 206. Editores: Mariangela Hungria, Douglas Fabiano Gomes, Arnaldo Colozzi Filho.| Tipo: Resumo em Anais de Congresso |
| Biblioteca(s): Embrapa Soja. |
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| 9. | | BROWN, G. G.; BENITO, N. P.; PASINI, A.; GUIMARÃES, M. de F.; TORRES, E. Earthworm populations under no-, minimum-, and conventional-tillage management systems near Londrina, Paraná, Brazil. In: INTERNATIONAL SOIL TILLAGE RESEARCH ORGANISATION CONFERENCE, 16., 2003, Brisbane. Soil management for sustainability. Brisbane: Grains Research & Development Corporation: The University of Queensland: Australian Centre for International Agricultural Research, 2003. p. 219-225. 1 CD-ROM.| Biblioteca(s): Embrapa Soja. |
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| 10. | | NEVES, C. S. V. J.; DECHEN, A. R.; MEDINA, C. de C.; GUIMARÃES, M. de F. Comparison of citrus rooting evaluationn methods using root images in soil profiles and root weight. Pesquisa Agropecuária Brasileira, Brasília, DF, v. 35, n. 12, p. 2537-41, dez. 2000 Notas Científicas.
Título em português: Características de frutos de genótipos de aceroleira cultivados sob elevada altitude.| Biblioteca(s): Embrapa Unidades Centrais. |
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| 11. | | MULLER, M. M. L.; GUIMARÃES, M. de F.; DESJARDINS, T.; MARTINS, P. F. da S. Degradação de pastagens na Região Amazônica: propriedades físicas do solo e crescimento de raízes. Pesquisa Agropecuária Brasileira, Brasília, DF, v. 36, n. 11, p. 1409-1418, nov. 2001 Título em inglês: Pasture degradation in the Amazon region: soil physical properties and root growth.| Biblioteca(s): Embrapa Unidades Centrais. |
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| 16. | | PICCININ, J. L.; MEDINA, C. de C.; GUIMARAES, M. de F.; SARAIVA, O. F.; TORRES, E. Relacao entre organizacao estrutural, crescimento de raizes e propriedades fisicas de um latossolo roxo submetido ao sistema de semeadura direta. In: REUNIAO BRASILEIRA DE FERTILIDADE DO SOLO E NUTRICAO DE PLANTAS, 23.; REUNIAO BRASILEIRA SOBRE MICORRIZAS, 7.; SIMPOSIO BRASILEIRO DE MICROBIOLOGIA DO SOLO, 5.; REUNIAO BRASILEIRA DE BIOLOGIA DO SOLO, 2., 1998, Caxambu. FertBio 98: interrelacao fertilidade, biologia do solo e nutricao de plantas: consolidando um paradigma - resumos. Lavras: UFLA / SBCS / SBM, 1998. p.121.| Biblioteca(s): Embrapa Soja. |
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| 17. | | VENDRAME, P. R. S.; MARCHAO, R. L.; BRITO, O. R.; GUIMARÃES, M. de F.; BECQUER, T. Relationship between macrofauna, mineralogy and exchangeable calcium and magnesium in Cerrado Oxisols under pasture. Pesquisa Agropecuária Brasileira, Brasília, DF, v. 44, n. 8, p. 996-1001, ago. 2009 Título em português: Relações entre macrofauna, mineralogia, cálcio e magnésio trocáveis em Latossolos do Cerrado sob pastagem.| Biblioteca(s): Embrapa Unidades Centrais. |
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| 18. | | VENDRAME, P. R. S.; MARCHAO, R. L.; BRITO, O. R.; GUIMARÃES, M. de F.; BECQUER, T. Relationship between macrofauna, mineralogy and exchangeable calcium and magnesium in Cerrado Oxisols under pasture Pesquisa Agropecuária Brasileira, Brasília, v. 44, n. 8, p. 996-1001, ago. 2009.| Tipo: Artigo em Periódico Indexado | Circulação/Nível: B - 1 |
| Biblioteca(s): Embrapa Cerrados. |
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| 19. | | SILVA, R. F. da; AQUINO, A. M. de; MERCANTE, F. M.; GUIMARÃES, M. de F. Macrofauna invertebrada do solo em sistema integrado de produção agropecuária no cerrado. Acta Scientiarum, Agronomy, Maringá, v. 30, n. 5, p.725‑ 731, set./out. 2008.| Tipo: Artigo em Periódico Indexado | Circulação/Nível: Nacional - A |
| Biblioteca(s): Embrapa Agropecuária Oeste. |
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| Registros recuperados : 73 | |
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