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| Registros recuperados : 198 | |
| 45. |  | CARVALHO, M. da C. S.; OLIVEIRA, J. P. de; MACHADO, P. L. O. de A.; NAUMOV, A. Severidade de brusone e produtividade de cultivares de arroz de várzea tropical adubadas com potássio. 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. 1 CD-ROM. FERTBIO 2012.| Biblioteca(s): Embrapa Arroz e Feijão. |
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| 47. | | SÁ, T. F. L. de; MADARI, B.; MACHADO, P. L. O. de A.; GUIMARÃES, C. M.; TORRES, E. O efeito do plantio e da rotação de culturas na agregação e no carbono orgânico de dois latossolos. In: REUNIÃO BRASILEIRA DE FERTILIDADE DO SOLO E NUTRIÇÃO DE PLANTAS, 25.; REUNIÃO BRASILEIRA SOBRE MICORRIZAS, 9.; SIMPÓSIO BRASILEIRO DE MICROBIOLOGIA DO SOLO, 7.; REUNIÃO BRASILEIRA DE BIOLOGIA DO SOLO, 4., 2002, Rio de Janeiro. Fertbio 2002: agricultura: bases ecológicas para o desenvolvimento social e econômico sustentado. Rio de Janeiro, 2002. p. 146. Guia do congressista e em CD-ROM.| Biblioteca(s): Embrapa Soja. |
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| 49. | | ALVES, S. de S.; WADT, P. G. S.; LIMA, M. A. de; MACHADO, P. L. O. de A. Estoque de carbono em um argissolo da Formação Solimões, sob três sistemas de uso da terra. In: SEMINÁRIO DE INICIAÇÃO CIENTÍFICA PIBIC/CNPq//UFAC, 14.; MOSTRA DE PESQUISA E PÓS-GRADUAÇÃO, 4., 2005, Rio Branco, AC. Anais... Rio Branco, AC: Ufac, 2005. 2 p. 1 CD-ROM.| Biblioteca(s): Embrapa Acre. |
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| 53. | | MADARI, B. E.; NOVOTNY, E. H.; MANGRICH, A. S.; MACHADO, P. L. O. de A.; CARVALHO, M. T. de M. Desenvolvimento de novas tecnologias para o seqüestro de carbono e consequente aumento da fertilidade dos solos tropicais. In: SIMPÓSIO SOBRE INOVAÇÃO E CRIATIVIDADE CIENTÍFICA NA EMBRAPA, 1., 2008, Brasília, DF. Comunicações selecionadas: resumos. Brasília, DF: Embrapa, 2008.| Biblioteca(s): Embrapa Arroz e Feijão. |
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| 58. | | PRADO, R. B.; BENITES, V. M.; MACHADO, P. L. O. de A.; POLIDORO, J. C.; DART, R. O.; NAUMOV, A. Mapping potassium availability from limited soil profile data in Brazil. In: HARTEMINK, A. E.; McBRATNEY, A.; MENDONÇA-SANTOS, M. de L. (Ed.). Digital soil mapping with limited data. New York: Springer, 2008. p. 91-101.| Biblioteca(s): Embrapa Arroz e Feijão; Embrapa Solos. |
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| Registros recuperados : 198 | |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Solos. Para informações adicionais entre em contato com cnps.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Arroz e Feijão; Embrapa Solos. |
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Data corrente: |
10/01/2007 |
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Data da última atualização: |
16/09/2021 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
Internacional - A |
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Autoria: |
BENITES, V. de M.; MACHADO, P. L. O. de A.; FIDALGO, E. C. C.; COELHO, M. R.; MADARI, B. E. |
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Afiliação: |
VINICIUS DE MELO BENITES, CNPS; PEDRO LUIZ OLIVEIRA DE A MACHADO, CNPAF; ELAINE CRISTINA CARDOSO FIDALGO, CNPS; MAURICIO RIZZATO COELHO, CNPS; BEATA EMOKE MADARI, CNPAF. |
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Título: |
Pedotransfer functions for estimating soil bulk density from existing soil survey reports in Brazil. |
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Ano de publicação: |
2007 |
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Fonte/Imprenta: |
Geoderma, v. 139, n. 1/2, p. 90-97, Apr. 2007. |
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DOI: |
https://doi.org/10.1016/j.geoderma.2007.01.005 |
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Idioma: |
Inglês |
|
Conteúdo: |
Soil bulk density (Db) measurement is essential to estimate soil carbon reserves. However, field sampling, specially at depth, and direct measurement of Db is labor intensive, tedious and often impractical. Thus regression models or pedotransfer functions (PTFs) based on easily measured soil properties are an alternative for laborious Db measurements. A forward stepwise multiple regression routine was used to predict Db from 17 soil properties using a data set (data set 1) constructed from the Soil Archives of Embrapa Solos, Rio de Janeiro, Brazil. A first exploratory regression model using 1002 soil samples of data set 1 led to the development of a model, which indicated that total nitrogen (N), clay content (Clay) and sum of basic cations (SB) were the three strongest contributors to Db prediction (Adjusted-R2=0.71, Standard error of the estimate=0.10). A simplified regression model was developed using easily-measured soil attributes, such as soil organic carbon (TOC), Clay and SB. This model described 66% of the variation of Db in 1396 soil samples distributed at all depths (Standard error of the estimate=0.11). Clay content showed a good correlation with predicted Db (Beta value=-0.58) followed by TOC (Beta value=-0.51) and SB (Beta value=0.21). Partitioning the data set 1 into groups by soil depth (0?30 and 30?100 cm) and soil order (Latossolos and Argissolos) did not improve the accuracy of regression equations. In addition, we tested the Db predictive potential of the proposed model and three existing models (two from Brazil and one from the US) on an independent soil data set (data set 2). A general overestimation of predicted Db by the US model, with mean predicted error (MPE) of 0.11 shows that published PTFs developed on different environments should be used with care. Existing Brazilian models developed for the Amazon biome, on the other hand, were found to produce a slight underestimation with MPE values ranging from -0.03 to -0.16. The proposed simple regression model including Clay, TOC and SB was observed to be the most accurate and least biased. MenosSoil bulk density (Db) measurement is essential to estimate soil carbon reserves. However, field sampling, specially at depth, and direct measurement of Db is labor intensive, tedious and often impractical. Thus regression models or pedotransfer functions (PTFs) based on easily measured soil properties are an alternative for laborious Db measurements. A forward stepwise multiple regression routine was used to predict Db from 17 soil properties using a data set (data set 1) constructed from the Soil Archives of Embrapa Solos, Rio de Janeiro, Brazil. A first exploratory regression model using 1002 soil samples of data set 1 led to the development of a model, which indicated that total nitrogen (N), clay content (Clay) and sum of basic cations (SB) were the three strongest contributors to Db prediction (Adjusted-R2=0.71, Standard error of the estimate=0.10). A simplified regression model was developed using easily-measured soil attributes, such as soil organic carbon (TOC), Clay and SB. This model described 66% of the variation of Db in 1396 soil samples distributed at all depths (Standard error of the estimate=0.11). Clay content showed a good correlation with predicted Db (Beta value=-0.58) followed by TOC (Beta value=-0.51) and SB (Beta value=0.21). Partitioning the data set 1 into groups by soil depth (0?30 and 30?100 cm) and soil order (Latossolos and Argissolos) did not improve the accuracy of regression equations. In addition, we tested the Db predictive potential of the... Mostrar Tudo |
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Palavras-Chave: |
Carbono orgânico do solo; Clay content; Funções de pedotransferência; Validação do modelo. |
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Thesagro: |
Argila; Carbono; Solo; Solo Orgânico. |
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Thesaurus NAL: |
Clay; Model validation; Pedotransfer functions; Soil organic carbon. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
|
Marc: |
LEADER 03082naa a2200325 a 4500
001 1339174
005 2021-09-16
008 2007 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1016/j.geoderma.2007.01.005$2DOI
100 1 $aBENITES, V. de M.
245 $aPedotransfer functions for estimating soil bulk density from existing soil survey reports in Brazil.$h[electronic resource]
260 $c2007
520 $aSoil bulk density (Db) measurement is essential to estimate soil carbon reserves. However, field sampling, specially at depth, and direct measurement of Db is labor intensive, tedious and often impractical. Thus regression models or pedotransfer functions (PTFs) based on easily measured soil properties are an alternative for laborious Db measurements. A forward stepwise multiple regression routine was used to predict Db from 17 soil properties using a data set (data set 1) constructed from the Soil Archives of Embrapa Solos, Rio de Janeiro, Brazil. A first exploratory regression model using 1002 soil samples of data set 1 led to the development of a model, which indicated that total nitrogen (N), clay content (Clay) and sum of basic cations (SB) were the three strongest contributors to Db prediction (Adjusted-R2=0.71, Standard error of the estimate=0.10). A simplified regression model was developed using easily-measured soil attributes, such as soil organic carbon (TOC), Clay and SB. This model described 66% of the variation of Db in 1396 soil samples distributed at all depths (Standard error of the estimate=0.11). Clay content showed a good correlation with predicted Db (Beta value=-0.58) followed by TOC (Beta value=-0.51) and SB (Beta value=0.21). Partitioning the data set 1 into groups by soil depth (0?30 and 30?100 cm) and soil order (Latossolos and Argissolos) did not improve the accuracy of regression equations. In addition, we tested the Db predictive potential of the proposed model and three existing models (two from Brazil and one from the US) on an independent soil data set (data set 2). A general overestimation of predicted Db by the US model, with mean predicted error (MPE) of 0.11 shows that published PTFs developed on different environments should be used with care. Existing Brazilian models developed for the Amazon biome, on the other hand, were found to produce a slight underestimation with MPE values ranging from -0.03 to -0.16. The proposed simple regression model including Clay, TOC and SB was observed to be the most accurate and least biased.
650 $aClay
650 $aModel validation
650 $aPedotransfer functions
650 $aSoil organic carbon
650 $aArgila
650 $aCarbono
650 $aSolo
650 $aSolo Orgânico
653 $aCarbono orgânico do solo
653 $aClay content
653 $aFunções de pedotransferência
653 $aValidação do modelo
700 1 $aMACHADO, P. L. O. de A.
700 1 $aFIDALGO, E. C. C.
700 1 $aCOELHO, M. R.
700 1 $aMADARI, B. E.
773 $tGeoderma$gv. 139, n. 1/2, p. 90-97, Apr. 2007.
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