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Registro Completo |
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
09/01/2023 |
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Data da última atualização: |
04/12/2023 |
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Tipo da produção científica: |
Capítulo em Livro Técnico-Científico |
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Autoria: |
ARAUJO FILHO, J. C. de; CORREA, M. M.; PAIVA, A. Q.; COSTA, O. V.; VALLADARES, G. S.; RIBEIRO, M. R.; SCHAEFER, C. E. G. R. |
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Afiliação: |
JOSE COELHO DE ARAUJO FILHO, CNPS; MARCELO METRI CORREA, UNIVERSIDADE FEDERAL DO AGRESTE DE PERNAMBUCO; ARLICELIO QUEIROZ PAIVA, UNIVERSIDADE ESTADUAL DE SANTA CRUZ; OLDAIR VINHAS COSTA, UNIVERSIDADE FEDERAL DO RECÔNCAVO DA BAHIA; GUSTAVO SOUZA VALLADARES, UNIVERSIDADE FEDERAL DO PIAUÍ; MATHEUS ROSA RIBEIRO; CARLOS ERNESTO GONÇALVES REYNAUD SCHAEFER, UNIVERSIDADE FEDERAL DE VIÇOSA. |
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Título: |
Semi-arid soils of the caatinga biome of Northeastern Brazil. |
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Ano de publicação: |
2023 |
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Fonte/Imprenta: |
In: SCHAEFER, C. E. G. R. (ed.). The soils of Brazil. Cham: Springer, 2023. cap. 6, p. 175-193. (World soils book series). |
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DOI: |
https://doi.org/10.1007/978-3-031-19949-3_6 |
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Idioma: |
Inglês |
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Conteúdo: |
Northeastern Brazil possesses a wide variety of environments, soils, substrates, and climates, although semi-arid conditions prevail in the core area of this biome, under thorny shrubby and succulent Caatinga vegetation. There, soils vary from shallow to deeply weathered, but in general, there is a predominance of a lower weathering degree and high fertility soils, compared with all other Brazilian regions. The high pedodiversity of this semi-arid domain is a consequence of a wide range of parent materials, especially on crystalline basement rocks (gneiss, granitoids, mica-schists). The most typical soils are Luvissolos (Luvisols), Planossolos (Planosols and Solonetz), and Neossolos Litólicos or Regolíticos (Leptosols and Regosols). On highland sedimentary basins, soils are pre-weathered and with very low fertility, predominantly Latossolos (Ferralsols) and Neossolos Quartzarênicos (Arenosols), where sandstone predominate. However, large areas of limestone also occur, giving way to soils with higher fertility, influenced by carbonates. The largest areas of these limestone soils comprise Cambissolos (Cambisols) with a small proportion of Vertissolos (Vertisols), and minor, restricted areas with Chernossolos (Chernozems). In the transitional zones with wetter areas, intermediary soils have low fertility, normally deeper, weathered, and degraded, notably Latossolos (Ferralsols), Argissolos (Acrisols and Lixisols), and Neossolos Quartzarênicos (Arenosols). |
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Palavras-Chave: |
Agricultura tropical; Brazilian semi-arid; Neotropical soils; Semiárido; Solos Neotropicais; Tropical pedology. |
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Thesagro: |
Mudança Climática; Solo Tropical. |
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Thesaurus Nal: |
Climate change; Tropical agriculture; Tropical soils. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02543naa a2200337 a 4500
001 2150787
005 2023-12-04
008 2023 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1007/978-3-031-19949-3_6$2DOI
100 1 $aARAUJO FILHO, J. C. de
245 $aSemi-arid soils of the caatinga biome of Northeastern Brazil.$h[electronic resource]
260 $c2023
520 $aNortheastern Brazil possesses a wide variety of environments, soils, substrates, and climates, although semi-arid conditions prevail in the core area of this biome, under thorny shrubby and succulent Caatinga vegetation. There, soils vary from shallow to deeply weathered, but in general, there is a predominance of a lower weathering degree and high fertility soils, compared with all other Brazilian regions. The high pedodiversity of this semi-arid domain is a consequence of a wide range of parent materials, especially on crystalline basement rocks (gneiss, granitoids, mica-schists). The most typical soils are Luvissolos (Luvisols), Planossolos (Planosols and Solonetz), and Neossolos Litólicos or Regolíticos (Leptosols and Regosols). On highland sedimentary basins, soils are pre-weathered and with very low fertility, predominantly Latossolos (Ferralsols) and Neossolos Quartzarênicos (Arenosols), where sandstone predominate. However, large areas of limestone also occur, giving way to soils with higher fertility, influenced by carbonates. The largest areas of these limestone soils comprise Cambissolos (Cambisols) with a small proportion of Vertissolos (Vertisols), and minor, restricted areas with Chernossolos (Chernozems). In the transitional zones with wetter areas, intermediary soils have low fertility, normally deeper, weathered, and degraded, notably Latossolos (Ferralsols), Argissolos (Acrisols and Lixisols), and Neossolos Quartzarênicos (Arenosols).
650 $aClimate change
650 $aTropical agriculture
650 $aTropical soils
650 $aMudança Climática
650 $aSolo Tropical
653 $aAgricultura tropical
653 $aBrazilian semi-arid
653 $aNeotropical soils
653 $aSemiárido
653 $aSolos Neotropicais
653 $aTropical pedology
700 1 $aCORREA, M. M.
700 1 $aPAIVA, A. Q.
700 1 $aCOSTA, O. V.
700 1 $aVALLADARES, G. S.
700 1 $aRIBEIRO, M. R.
700 1 $aSCHAEFER, C. E. G. R.
773 $tIn: SCHAEFER, C. E. G. R. (ed.). The soils of Brazil. Cham: Springer, 2023. cap. 6, p. 175-193. (World soils book series).
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| 1. |  | ARAUJO FILHO, J. C. de; CORREA, M. M.; PAIVA, A. Q.; COSTA, O. V.; VALLADARES, G. S.; RIBEIRO, M. R.; SCHAEFER, C. E. G. R. Semi-arid soils of the caatinga biome of Northeastern Brazil. In: SCHAEFER, C. E. G. R. (ed.). The soils of Brazil. Cham: Springer, 2023. cap. 6, p. 175-193. (World soils book series).| Tipo: Capítulo em Livro Técnico-Científico |
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