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Registro Completo |
Biblioteca(s): |
Embrapa Cerrados. |
Data corrente: |
14/06/2022 |
Data da última atualização: |
14/06/2022 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
OLIVEIRA, J. F. de; BROSSARD, M.; CORAZZA, E. J.; GUIMARÃES, M. F.; MARCHAO, R. L. |
Afiliação: |
JOSE FRANCIRLEI DE OLIVEIRA; MICHEL BROSSARD; EDEMAR JOAQUIM CORAZZA, SPD; MARIA DE FATIMA GUIMARAES; ROBELIO LEANDRO MARCHAO, CPAC. |
Título: |
Field-scale spatial correlation between soil and Vis-NIR spectra in the Cerrado biome of Central Brazi. |
Ano de publicação: |
2022 |
Fonte/Imprenta: |
Geoderma Regional, v. 30, e00532, 2022. |
Páginas: |
13 p. |
Idioma: |
Inglês |
Conteúdo: |
Visible and near-infrared (Vis-NIR) spectroscopy is a tool to determine soil spatial variability and has been used to map soils and their properties. Considering that physical, chemical, mineralogical, and morphological soil properties can affect the intensity and the depth of the spectral reflectance band in the Vis-NIR region, the objectives of this work were to: (i) evaluate the potential of the reflectance inflection difference (RID) to discriminate soils; and (ii) verify potential spatial correlations of the RID with soil properties, compared with the full spectra, in order to build thematic maps at a field scale. In a farm of 375 ha, 78 soil samples from the 0.87?0.92-m depth were collected in a regular grid of 200 m, with a focus on the soil diagnostic horizon (Bw horizon). The sampled soils were a Latossolo Vermelho-Amarelo ´ acrico (Haplic Ferralsol) and a Latossolo Vermelho distrofico ´ (Rhodic Ferralsol). Twenty-two physical, chemical, mineralogical, and morphological soil properties were determined, and the Vis-NIR spectra between 400 and 2500 nm were measured. Considering the presence of an inflection band and its relationship with soil properties, the spectral bands used to calculate the RID were between (base 1/base 2): 400?510, 730?930, 1290?1450, 1800?1950, 2000?2218, and 2218?2290 nm. The RID failed to map the spatial variability of soil properties, with a Kappa index of 39%; therefore, it is not a good parameter for building thematic maps of soil parameters. In addition, the complete spectrum (mainly in 400?510, 730?930, 1290?1450, 1800?1950, 2000?2218, and 2218?2290 nm) was better spatially correlated with soil properties than the decomposition of the spectrum by the RID. Soil classification and level of discretization as affected by spectral variability were also discussed here. Three soil groups were discriminated mainly by the Ki and Kr indexes and clay content. Moreover, the variability of the spectra was conditioned by the spatial variability of the mentioned variables. The clay content for soils with a discrepant particle size (group 1 compared with groups 2 and 3) and the Ki and Kr indexes for soils with a homogeneous particle size (between groups 2 and 3), associated with the full Vis-NIR spectral analysis, allowed building thematic maps with a good precision, without the need of mathematical models; this was possible by the modification of the reflectance intensity and the size of the concavity of the spectral band. MenosVisible and near-infrared (Vis-NIR) spectroscopy is a tool to determine soil spatial variability and has been used to map soils and their properties. Considering that physical, chemical, mineralogical, and morphological soil properties can affect the intensity and the depth of the spectral reflectance band in the Vis-NIR region, the objectives of this work were to: (i) evaluate the potential of the reflectance inflection difference (RID) to discriminate soils; and (ii) verify potential spatial correlations of the RID with soil properties, compared with the full spectra, in order to build thematic maps at a field scale. In a farm of 375 ha, 78 soil samples from the 0.87?0.92-m depth were collected in a regular grid of 200 m, with a focus on the soil diagnostic horizon (Bw horizon). The sampled soils were a Latossolo Vermelho-Amarelo ´ acrico (Haplic Ferralsol) and a Latossolo Vermelho distrofico ´ (Rhodic Ferralsol). Twenty-two physical, chemical, mineralogical, and morphological soil properties were determined, and the Vis-NIR spectra between 400 and 2500 nm were measured. Considering the presence of an inflection band and its relationship with soil properties, the spectral bands used to calculate the RID were between (base 1/base 2): 400?510, 730?930, 1290?1450, 1800?1950, 2000?2218, and 2218?2290 nm. The RID failed to map the spatial variability of soil properties, with a Kappa index of 39%; therefore, it is not a good parameter for building thematic maps of soil parameter... Mostrar Tudo |
Palavras-Chave: |
Diferença de inflexão de refletância; Índices Ki e Kr; Variabilidade espacial do solo. |
Thesagro: |
Argila; Espectrometria; Raio Infravermelho; Solo. |
Categoria do assunto: |
-- |
Marc: |
LEADER 03277naa a2200265 a 4500 001 2144045 005 2022-06-14 008 2022 bl uuuu u00u1 u #d 100 1 $aOLIVEIRA, J. F. de 245 $aField-scale spatial correlation between soil and Vis-NIR spectra in the Cerrado biome of Central Brazi.$h[electronic resource] 260 $c2022 300 $a13 p. 520 $aVisible and near-infrared (Vis-NIR) spectroscopy is a tool to determine soil spatial variability and has been used to map soils and their properties. Considering that physical, chemical, mineralogical, and morphological soil properties can affect the intensity and the depth of the spectral reflectance band in the Vis-NIR region, the objectives of this work were to: (i) evaluate the potential of the reflectance inflection difference (RID) to discriminate soils; and (ii) verify potential spatial correlations of the RID with soil properties, compared with the full spectra, in order to build thematic maps at a field scale. In a farm of 375 ha, 78 soil samples from the 0.87?0.92-m depth were collected in a regular grid of 200 m, with a focus on the soil diagnostic horizon (Bw horizon). The sampled soils were a Latossolo Vermelho-Amarelo ´ acrico (Haplic Ferralsol) and a Latossolo Vermelho distrofico ´ (Rhodic Ferralsol). Twenty-two physical, chemical, mineralogical, and morphological soil properties were determined, and the Vis-NIR spectra between 400 and 2500 nm were measured. Considering the presence of an inflection band and its relationship with soil properties, the spectral bands used to calculate the RID were between (base 1/base 2): 400?510, 730?930, 1290?1450, 1800?1950, 2000?2218, and 2218?2290 nm. The RID failed to map the spatial variability of soil properties, with a Kappa index of 39%; therefore, it is not a good parameter for building thematic maps of soil parameters. In addition, the complete spectrum (mainly in 400?510, 730?930, 1290?1450, 1800?1950, 2000?2218, and 2218?2290 nm) was better spatially correlated with soil properties than the decomposition of the spectrum by the RID. Soil classification and level of discretization as affected by spectral variability were also discussed here. Three soil groups were discriminated mainly by the Ki and Kr indexes and clay content. Moreover, the variability of the spectra was conditioned by the spatial variability of the mentioned variables. The clay content for soils with a discrepant particle size (group 1 compared with groups 2 and 3) and the Ki and Kr indexes for soils with a homogeneous particle size (between groups 2 and 3), associated with the full Vis-NIR spectral analysis, allowed building thematic maps with a good precision, without the need of mathematical models; this was possible by the modification of the reflectance intensity and the size of the concavity of the spectral band. 650 $aArgila 650 $aEspectrometria 650 $aRaio Infravermelho 650 $aSolo 653 $aDiferença de inflexão de refletância 653 $aÍndices Ki e Kr 653 $aVariabilidade espacial do solo 700 1 $aBROSSARD, M. 700 1 $aCORAZZA, E. J. 700 1 $aGUIMARÃES, M. F. 700 1 $aMARCHAO, R. L. 773 $tGeoderma Regional$gv. 30, e00532, 2022.
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Registros recuperados : 61 | |
22. | | BROSSARD, M.; LOPES ASSAD, M. L.; CHAPUIS, L.; BARCELLOS, A. O. Estoques de carbono em solos sob diferentes fitofisionomias de cerrados. In: LEITE, L.L.; SAITO, C.H., ed. Contribuicao ao conhecimento ecologico do cerrado. Brasilia: UnB, 1997. p.272-277. Trabalho apresentado no 3o. Congresso de Ecologia do Brasil, Brasilia, 1996.Biblioteca(s): Embrapa Cerrados. |
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26. | | BALBINO, L.; BRUAND, A.; BROSSARD, M.; GUIMARAES, M. F.; QUETIN, P. Degradation de la structure de latosols sous paturage dans les savanes bresiliennes (Cerrados). In: JOURNEES NATIONALES DE l'ETUDE DES SOLS, 6., 2000, Nancy, France. Les enjeux actuels de l'anthropisation des sols: programme & resumes. Nancy: AFES, 2000. p.16.Biblioteca(s): Embrapa Cerrados. |
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27. | | BALBINO, L.; BRUAND, A.; BROSSARD, M.; GUIMARÃES, M. F.; QUÉTIN, P. Degradation de la structure de latosols sous paturage dans les savanes bresiliennes (Cerrados). In: JOURNEES NATIONALES DE L'ETUDE DES SOLS, 6., 2000, Nancy, Franca. Les enjeux actuels de l'anthropisation des sols: programme & resumes. Nancy: Association Francaise pour L'Etude des Sols, 2000. p. 16.Tipo: Resumo em Anais de Congresso |
Biblioteca(s): Embrapa Arroz e Feijão. |
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29. | | MARCHAO, R. L.; BECQUER, T.; BRUNET, D.; BALBINO, L. C.; VILELA, L.; BROSSARD, M. Integrated crop-livestock management system: C and N stocks in a Brazilian clayey oxisol using NIRS. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 31., 2007, Gramado. Conquistas e desafios da ciência do solo brasileira: anais. Porto Alegre: SBCS, 2007. 1 CD-ROM. 5 p.Tipo: Artigo em Anais de Congresso / Nota Técnica |
Biblioteca(s): Embrapa Cerrados. |
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30. | | AYARZA, M. A.; VILELA, L.; BARCELLOS, A. de O.; BALBINO, L. C.; BROSSARD, M.; PASINI, A. Integration culture-elevage dans les cerrados au Brasil: une solution pour des systemes durables. Agriculture et Developpement, Montpellier, n.18, p.91-98, juin 1998.Biblioteca(s): Embrapa Cerrados. |
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31. | | AYARZA, M. A.; VILELA, L.; BARCELLOS, A. de O.; BALBINO, L. C.; BROSSARD, M.; PASINI, A. Integration culture-elevage dans les cerrados au Bresil: une solution pour des systemes durables. Agriculture et Developpement, Montpellier, n. 18, p. 91-98, juin 1998.Tipo: Artigo em Periódico Indexado |
Biblioteca(s): Embrapa Arroz e Feijão. |
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33. | | FUJISAKI, K.; PERRIN, A.-S.; DESJARDINS, T.; BERNOUX, M.; BALBINO, L. C.; BROSSARD, M. From forest to cropland and pasture systems: a critical review of soil organic carbon stocks changes in Amazonia. Global Change Biology, v. 21, n. 7, p. 2773-2786, Jul. 2015.Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
Biblioteca(s): Embrapa Cerrados. |
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35. | | SILVA, A. V.; REATTO, A.; BROSSARD, M.; MARTINS, E. M.; CARVALHO, A. M. Quantificacao de raizes utilizando softwares de tratamento de imagens. In: CONGRESSO BRASILEIRO DE CIENCIA DO SOLO, 28., 2001, Londrina, PR. Ciencia do solo: fator de produtividade competitiva com sustentabilidade. Londrina: SBCS, 2001. p. 254. Resumo.Biblioteca(s): Embrapa Cerrados. |
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37. | | BENITO, N. P.; BROSSARD, M.; JOST, C.; FOURCASSIE, V.; CAMARGO, A. In vitro tunnel network construction by Cornitermes cumulans (Isoptera: Termitidae) and resulting soil structures. In: INTERNATIONAL COLLOQUIUM ON SOIL ZOOLOGY, 15; INTERNATIONAL COLLOQUIUM ON APTERYGOTA, 12., 2008, Curitiba. Biodiversity, conservation and sustainabele management of soil animal: abstracts. Colombo: Embrapa Florestas. Editors: George Gardner Brown; Klaus Dieter Sautter; Renato Marques; Amarildo Pasini. 1 CD-ROM.Biblioteca(s): Embrapa Florestas. |
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38. | | OLIVEIRA, M. I. L. DE.; BENITO, N. P.; CAMARGO, A. J. A. de; GUIMARÃES, M. DE F.; BROSSARD, M. Atividade de colônias de Cornitermes Cumulans (Isoptera, Nasutitermitinae) sobre estruturas edáficas macro e microagregadas em casa de vegetação. Semina: Ciências Agrárias, Londrina, v. 33, n. 5, p. 1733-1744, set./out. 2012.Tipo: Artigo em Periódico Indexado | Circulação/Nível: B - 1 |
Biblioteca(s): Embrapa Cerrados; Embrapa Recursos Genéticos e Biotecnologia. |
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39. | | BROSSARD, M.; REATTO BRAGA, A.; OLIVEIRA, M. I. L.; BENITO, N. P.; BRUAND, A.; GUIMARÃES, M. F.; LÓPEZ HERNÁNDEZ, D. Análise de interações modelos térmita-solo em ambientes tropicais: impactos na física e geoquímica do solo. In: REUNIÃO BRASILEIRA DE FERTILIDADE DO SOLO E NUTRIÇÃO DE PLANTAS, 28.; REUNIÃO BRASILEIRA SOBRE MICORRIZAS, 12.; SIMPÓSIO BRASILEIRO DE MICROBIOLOGIA DO SOLO, 10.; REUNIÃO BRASILEIRA DE BIOLOGIA DO SOLO, 7., 2008, Londrina. Desafios para o uso do solo com eficiência e qualidade ambiental : anais. Londrina: SBCS: Embrapa Soja: IAPAR: UEL, 2008. 1 CD-ROM FertBio 2008. Palestra.Tipo: Artigo em Anais de Congresso / Nota Técnica |
Biblioteca(s): Embrapa Recursos Genéticos e Biotecnologia. |
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40. | | SILVA, A. V.; FARIAS, M. F. R.; REATTO, A.; MARTINS, E. S.; BROSSARD, M.; BECQUER, T.; OLIVEIRA, O. R. Caracterização e distribuição das principais classes pedológicas do Planalto Central brasileiro. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 30., 2005, Recife. Solos, sustentabilidade e qualidade ambiental: anais. Recife: SBCS: Embrapa Solos - UEP Recife: UFRPE, 2005. 1 CD-ROM.Biblioteca(s): Embrapa Cerrados. |
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Registros recuperados : 61 | |
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Nenhum registro encontrado para a expressão de busca informada. |
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