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| Registros recuperados : 219 | |
| 63. |  | IKEDA, F. S.; MARCHI, G.; MARCHAO, R. L.; VICTORIA FILHO, R. Doses reduzidas de glyphosate em três estádios de desenvolvimento de Urochloa ruzizensis (R. Germ. & C.M. Evrard) Morrone & Zuloaga In: CONGRESSO DE LA ASOCIACIÓN LATINOAMERICANA DE MALEZAS, 21.,; CONGRESO MEXICANO DE LA CIENCIA DE LA MALEZA, 34.,; SIMPOSIO INTERNACIONAL DE RESISTENCIA Y TOLERANCIA A HERBICIDAS, 1.,; SIMPOSIO INTERNACIONAL DE MALEZA ACUÁTICA, 9., 2013, Cancún, México. Memória... Cancún, QR: ALAM, 2013.| Biblioteca(s): Embrapa Agrossilvipastoril. |
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| 69. | | BUSSINGUER, A. P.; NIVA, C. C.; MARCHAO, R. L.; PULROLNIK, K.; GATTO, A.; JAMES, S. W. Caracterização de oligochaeta em diferentes sistemas silvipastoris no Cerrado. In: REUNIÃO BRASILEIRA DE FERTILIDADE DO SOLO E NUTRIÇÃO DE PLANTAS, 32.; REUNIÃO BRASILEIRA SOBRE MICORRIZAS, 16.; SIMPÓSIO BRASILEIRO DE MICROBIOLOGIA DO SOLO, 14.; REUNIÃO BRASILEIRA DE BIOLOGIA DO SOLO, 11., 2016, Goiânia. Rumo aos novos desafios: [anais]. Viçosa, MG: Sociedade Brasileira de Ciência do Solo, 2016. FertBio 2016. p. 1171.| Biblioteca(s): Embrapa Cerrados. |
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| 73. | | VILELA, L.; GUIMARAES JUNIOR, R.; MARCHAO, R. L.; PULROLNIK, K.; MACIEL, G. A. O papel da integração lavoura-pecuária na recuperação de pastagens degradadas. In: SIMPÓSIO DE FORRAGICULTURA E PASTAGENS, 8., 2011, Lavras. As forragens e suas relações com o solo, ambiente e o animal: anais. Lavras: UFLA, 2011. p. 37-51| Biblioteca(s): Embrapa Cerrados. |
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| 75. | | LOUZADA, G. A.; LOBO JUNIOR, M.; MARCHÃO, R, L.; BALBINO, L. C. Efeito da rotação de culturas sobre Fusarium spp. e atividade microbiológica em uma área de integração lavoura-pecuária. In: CONGRESSO NACIONAL DE PESQUISA DE FEIJÃO, 8., 2005, Goiânia. Anais... Santo Antônio de Goiás: Embrapa Arroz e Feijão, 2005. v. 1. p. 178-181. (Embrapa Arroz e Feijão. Documentos, 182).| Biblioteca(s): Embrapa Arroz e Feijão. |
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| 76. | | MARCHAO, R. L.; CORBEELS, M.; FERREIRA, E. G.; SIQUEIRA NETO, M.; MADARI, B. E. Estoques de carbono do solo após 20 anos de adoção em cronosequências de plantio direto na região de Rio Verde/Montividiu, Goiás. In: ENCONTRO NACIONAL DE PLANTIO DIRETO NA PALHA, 15., 2016, Goiânia. Palha, ambiente e renda: resumos apresentados. Santo Antônio de Goiás: Embrapa Arroz e Feijão, 2016. p. 36. (Embrapa Arroz e Feijão. Documentos, 313).| Biblioteca(s): Embrapa Arroz e Feijão. |
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| 77. | | SATO, J. H.; FIGUEIREDO, C. C. DE; MARCHAO, R. L.; BENEDITO, L. E. C. Métodos de determinação de carbono orgânico em solos cultivados e sob vegetação nativa de cerrado. 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, MG: Sociedade Brasileira de Ciência do Solo, 2012.| Biblioteca(s): Embrapa Cerrados. |
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| 79. | | BUSSINGUER, A. P.; NIVA, C. C.; MARCHAO, R. L.; PULROLNIK, K.; GATTO, A.; JAMES, S. W. Minhocas (Oligochaeta) em diferentes sistemas de uso do solo no Cerrado do Distrito Federal. In: ENCONTRO DE INICIAÇÃO CIENTÍFICA DA EMBRAPA CERRADOS. Jovens talentos 2016: resumos. Planaltina, DF: Embrapa Cerrados, 2016. 99 p. p. 27 (Embrapa Cerrados. Documentos, 334). Comissão organizadora: SOUZA, K. W. de; FALEIRO, A. S. G.; SALGUES, A. L. M.; ALONSO, A. M.; CARVALHO, A. M. de; LOBATO, B. R.; CRUZ, C. V.; SOUSA, E. dos S.; PELEGRINELLI, F.; SOARES, J. P. G.; LIMA, J. E. F. W.; ARBUES, J. F. de O.;...| Biblioteca(s): Embrapa Cerrados. |
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| Registros recuperados : 219 | |
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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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Circulação/Nível: |
B - 1 |
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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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