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| Registros recuperados : 246 | |
| 104. |  | PEREIRA, M. G.; VALLADARES, G. S.; ANJOS, L. H. C. DOS; BENITES, V. de M.; ESPÍNDULA JÚNIOR, A. Organic carbon determination in histosols and soil horizons with high organic matter content from Brazil. Scientia Agrícola, Piracicaba, v. 63, n. 2, p. 187-193, 2006.| Biblioteca(s): Embrapa Solos; Embrapa Territorial. |
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| 105. | | BARBOSA, A. M.; PINHEIRO, H. S. K.; ANJOS, L. H. C. dos; CARVALHO JUNIOR, W. de; CHAGAS, C. da S. Determinação de pontos amostrais através de atributos do terreno para mapeamento digital dos solos da bacia hidrográfica do Rio Guapi-Macacu, RJ. In: SIMPÓSIO BRASILEIRO DE SENSORIAMENTO REMOTO, 15., 2011, Curitiba, PR. Anais... Curitiba: INPE, 2011. 1690p. 8 p.| Biblioteca(s): Embrapa Solos. |
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| 107. | | SILVA, S. N. da; PINHEIRO, É. F. M.; ANJOS, L. H. C. dos; LIMA, E.; ALVES, B. J. R. Emissões de óxido nitroso em Argissolo Amarelo e influência da queima ou manutenção da palha na colheita de cana-de-açúcar. In: JORNADA DE INICIAÇÃO CIENTÍFICA DA UNIVERSIDADE FEDERAL RURAL DO RIO DE JANEIRO, 18., 2008, Seropédica, RJ. Seropédica, RJ, 2008. Parceria: UFRRJ.| Biblioteca(s): Embrapa Agrobiologia. |
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| 108. | | PINHEIRO, H. S. K; CHAGAS, C. da S.; CARVALHO JUNIOR, W. de; ANJOS, L. H. C. dos. Ferramentas de pedometria para caracterização da composição granulométrica de perfis de solos hidromórficos. Pesquisa Agropecuária Brasileira, Brasília, DF, v. 51, n. 9, p. 1326-1338, set. 2016.| Biblioteca(s): Embrapa Solos; Embrapa Unidades Centrais. |
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| 109. | | PIMENTA, L. M. M.; ZONTA, E.; BRASIL, F. C.; ANJOS, L. H. C. dos; PEREIRA, M. G.; STAFANATO, J. B. Fertilidade do solo em pastagens cultivadas sob diferentes manejos, no noroeste do Rio de Janeiro. Revista Brasileira de Engenharia Agrícola e Ambiental, v.14, n.11, p.1136–1142, nov., 2010.| Biblioteca(s): Embrapa Algodão. |
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| 110. | | COUTO, W. H. do; ANJOS, L. H. C. dos; TOLEDO, L. de O.; PEREIRA, M. G.; QUEIROS, M. M. Fitossociologia e diversidade florística em área de cerrado sob vários níveis de antropização, Rio Pardo de Minas, MG. Ciência Florestal, Santa Maria, v. 19, n. 4, p. 351-362, jul./set. 2009.| Biblioteca(s): Embrapa Florestas. |
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| 111. | | VALLADARES, G. S.; PEREIRA, M. G.; PEREZ, D. V.; SOUZA, J. M. P. F. de; ANJOS, L. H. C. dos. Fósforo remanescente e correlações com teores de carbono orgânico e argila em horizontes superficiais de solos do Estado do Rio de Janeiro. In: CONGRESSO LATINO AMERICANO DE CIÊNCIA DO SOLO, 13.; REUNIÃO BRASILEIRA DE BIOLOGIA DO SOLO, 1.; SIMPÓSIO BRASILEIRO SOBRE MICROBIOLOGIA DO SOLO, 4.; REUNIÃO BRASILEIRA SOBRE MICORRIZAS, 6.; REUNIÃO BRASILEIRA DE MANEJO E CONSERVAÇÃO DO SOLO E DA ÁGUA, 11., 1996, Águas de Lindóia. Solo suelo 96. Campinas: Sociedade Brasileira de Ciência do Solo, 1996. 1 CD-ROM.| Biblioteca(s): Embrapa Solos. |
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| 112. | | GOMES, F. W. de F.; EBELING, A. G.; ANJOS, L. H. C. dos; PEREIRA, M. G.; PEREZ, D. V. Fracionamento químico da matéria orgânica de Organossolos no estado do Rio de Janeiro. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 32., 2009, Fortaleza. O solo e a produção de bioenergia: perspectivas e desafios. [Viçosa, MG]: SBCS; Fortaleza: UFC, 2009. 1 CD-ROM.| Biblioteca(s): Embrapa Solos. |
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| 113. | | LOSS, A.; PEREIRA, M. G.; SCHULTZ, N.; ANJOS, L. H. C. dos; SILVA, E. M. R. da. Frações orgânicas e índice de manejo de carbono em diferentes sistemas de produção orgânico. In: REUNIÃO BRASILEIRA DE MANEJO E CONSERVAÇÃO DO SOLO E DA ÁGUA, 17., 2008, Rio de Janeiro. Manejo e conservação do solo e da água no contexto das mudanças ambientais. Rio de Janeiro: SBCS: Embrapa Solos: Embrapa Agrobiologia, 2008. 4 p. 1 CD-ROM. (Embrapa Solos. Documentos, 101). Parceria: UFRRJ.| Biblioteca(s): Embrapa Agrobiologia. |
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| Registros recuperados : 246 | |
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Registro Completo
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
02/04/2018 |
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Data da última atualização: |
11/11/2021 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 2 |
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Autoria: |
PINHEIRO, H. S. K.; CARVALHO JUNIOR, W. de; CHAGAS, C. da S.; ANJOS, L. H. C. dos; OWENS, P. R. |
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Afiliação: |
HELENA SARAIVA KOENOW PINHEIRO, UFRRJ; WALDIR DE CARVALHO JUNIOR, CNPS; CESAR DA SILVA CHAGAS, CNPS; LÚCIA HELENA CUNHA DOS ANJOS, UFRRJ; PHILLIP RAY OWENS, USDA. |
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Título: |
Prediction of topsoil texture through regression trees and multiple linear regressions. |
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Ano de publicação: |
2018 |
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Fonte/Imprenta: |
Revista Brasileira de Ciência do Solo, v. 42, article e0170167, 2018. |
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DOI: |
https://doi.org/10.1590/18069657rbcs20170167 |
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Idioma: |
Inglês |
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Conteúdo: |
Users of soil survey products are mostly interested in understanding how soil properties vary in space and time. The aim of digital soil mapping (DSM) is to represent the spatial variability of soil properties quantitatively to support decision-making. The goal of this study is to evaluate DSM techniques (Regression Trees - RT and Multiple Linear Regressions - MLR) and the ability of these tools to predict mineral fraction content under a wide variability of landscapes. The study site was the entire Guapi-Macacu watershed (1,250.78 km²) in the state of Rio de Janeiro in the Southeast region of Brazil. Terrain attributes and remote sensing data (with 30 m of spatial resolution) were used to represent landscape co-variables selected as an input in predictive models in order to develop the explanatory variables. The selection of sampling sites was based on the Latin Hypercube algorithm. A representative set of one hundred points with feasible field access was chosen. Different input databases were tested for prediction of mineral fraction content (harmonized and original data). The Spline algorithm was used to harmonize data according to the GlobalSoil.Net consortium standards. The results showed better performance from the RT models, using input from an average of six covariates; the simplest MLR model used twice as many input variables, creating more complex models without gaining precision. Furthermore, better R² values were obtained using RT models, irrespective of harmonization of soil data. The harmonized dataset from the 0.00-0.05 and 0.05-0.15 m layers, in general, presented better results for the clay and silt, with R2 values of 0.52 (0.00-0.05 m) and 0.69 (0.05-0.15 m), respectively. Prediction of sand content showed better results when the original depth data was used as an input, although all regression tree models had R2 values greater than 0.52. The RT models provided a better statistical index than MLR for all predicted properties; however, the variance between models suggests similarity of performance. Regarding harmonization of soil data, both input databases (harmonized or not) can be used to predict soil properties, since the variance of model performance was low and generalization of the soil maps showed similar trends. The products obtained from the digital soil mapping approach make it possible to integrate the factor of uncertainties, providing easier interpretation for soil management and land use decisions. MenosUsers of soil survey products are mostly interested in understanding how soil properties vary in space and time. The aim of digital soil mapping (DSM) is to represent the spatial variability of soil properties quantitatively to support decision-making. The goal of this study is to evaluate DSM techniques (Regression Trees - RT and Multiple Linear Regressions - MLR) and the ability of these tools to predict mineral fraction content under a wide variability of landscapes. The study site was the entire Guapi-Macacu watershed (1,250.78 km²) in the state of Rio de Janeiro in the Southeast region of Brazil. Terrain attributes and remote sensing data (with 30 m of spatial resolution) were used to represent landscape co-variables selected as an input in predictive models in order to develop the explanatory variables. The selection of sampling sites was based on the Latin Hypercube algorithm. A representative set of one hundred points with feasible field access was chosen. Different input databases were tested for prediction of mineral fraction content (harmonized and original data). The Spline algorithm was used to harmonize data according to the GlobalSoil.Net consortium standards. The results showed better performance from the RT models, using input from an average of six covariates; the simplest MLR model used twice as many input variables, creating more complex models without gaining precision. Furthermore, better R² values were obtained using RT models, irrespective of harmoniz... Mostrar Tudo |
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Palavras-Chave: |
Atributos do terreno; Funções de profundidade do solo; Mapeamento digital do solo; Modelos de regressão. |
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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/174786/1/2018-010.pdf
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Marc: |
LEADER 03254naa a2200229 a 4500
001 2089994
005 2021-11-11
008 2018 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1590/18069657rbcs20170167$2DOI
100 1 $aPINHEIRO, H. S. K.
245 $aPrediction of topsoil texture through regression trees and multiple linear regressions.$h[electronic resource]
260 $c2018
520 $aUsers of soil survey products are mostly interested in understanding how soil properties vary in space and time. The aim of digital soil mapping (DSM) is to represent the spatial variability of soil properties quantitatively to support decision-making. The goal of this study is to evaluate DSM techniques (Regression Trees - RT and Multiple Linear Regressions - MLR) and the ability of these tools to predict mineral fraction content under a wide variability of landscapes. The study site was the entire Guapi-Macacu watershed (1,250.78 km²) in the state of Rio de Janeiro in the Southeast region of Brazil. Terrain attributes and remote sensing data (with 30 m of spatial resolution) were used to represent landscape co-variables selected as an input in predictive models in order to develop the explanatory variables. The selection of sampling sites was based on the Latin Hypercube algorithm. A representative set of one hundred points with feasible field access was chosen. Different input databases were tested for prediction of mineral fraction content (harmonized and original data). The Spline algorithm was used to harmonize data according to the GlobalSoil.Net consortium standards. The results showed better performance from the RT models, using input from an average of six covariates; the simplest MLR model used twice as many input variables, creating more complex models without gaining precision. Furthermore, better R² values were obtained using RT models, irrespective of harmonization of soil data. The harmonized dataset from the 0.00-0.05 and 0.05-0.15 m layers, in general, presented better results for the clay and silt, with R2 values of 0.52 (0.00-0.05 m) and 0.69 (0.05-0.15 m), respectively. Prediction of sand content showed better results when the original depth data was used as an input, although all regression tree models had R2 values greater than 0.52. The RT models provided a better statistical index than MLR for all predicted properties; however, the variance between models suggests similarity of performance. Regarding harmonization of soil data, both input databases (harmonized or not) can be used to predict soil properties, since the variance of model performance was low and generalization of the soil maps showed similar trends. The products obtained from the digital soil mapping approach make it possible to integrate the factor of uncertainties, providing easier interpretation for soil management and land use decisions.
653 $aAtributos do terreno
653 $aFunções de profundidade do solo
653 $aMapeamento digital do solo
653 $aModelos de regressão
700 1 $aCARVALHO JUNIOR, W. de
700 1 $aCHAGAS, C. da S.
700 1 $aANJOS, L. H. C. dos
700 1 $aOWENS, P. R.
773 $tRevista Brasileira de Ciência do Solo$gv. 42, article e0170167, 2018.
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