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Registro Completo |
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
04/02/2022 |
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Data da última atualização: |
11/03/2022 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Autoria: |
PEREIRA, M. G.; SILVA, R. C. da; PINHEIRO JUNIOR, C. R.; OLIVEIRA, F. S. de; SILVA NETO, E. C. da; FONTANA, A.; PACHECO, A. A.; PEDRON, F. de A. |
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Afiliação: |
MARCOS GERVASIO PEREIRA, UFRRJ; RAFAEL CIPRIANO DA SILVA, FUNCEME; CARLOS ROBERTO PINHEIRO JUNIOR, UFRRJ; FÁBIO SOARES DE OLIVEIRA, UFMG; EDUARDO CARVALHO DA SILVA NETO, UFRRJ; ADEMIR FONTANA, CNPS; ANDERSON ALMEIDA PACHECO, FUNDAÇÃO RENOVA; FABRÍCIO DE ARAÚJO PEDRON, UFSM. |
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Título: |
Soil genesis on the soft slopes of ancient coastal plains, southeastern Brazil. |
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Ano de publicação: |
2022 |
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Fonte/Imprenta: |
Catena, v. 210, 105894, Mar. 2022. |
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DOI: |
https://doi.org/10.1016/j.catena.2021.105894 |
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Idioma: |
Inglês |
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Conteúdo: |
Coastal plains are characterized by low-elevation and small altitude variation and occupy an area of 57 million km2 worldwide. Ancient coastal plains that occur in the State of Rio de Janeiro (RJ), Brazil, have their pedological diversity neglected due to the generalization of some soil classes, underestimating the diversity of soils in these regions, hence limiting the evaluation for use and management. The aim of this study was to characterize the diversity of soils in a toposequence along an ancient coastal plain and to understand the pedogenetic processes involved. For this, soil pits were opened in the lower third (P1), middle third (P2), upper third (P3) and at the top (P4) of a toposequence. Soil profiles were characterized for morphological, physical, chemical, mineralogical and micromorphological properties. Profile P1 was classified as Planosol, being formed from colluvial sediments. In this profile, a lithological discontinuity was identified based on the irregularity of the values of silt/clay and coarse sand/fine sand ratios in subsurface. In this profile, limited drainage conditions were also observed. The main formation processes identified were ferrolysis and clay eluviation/illuviation, which promoted the increase of the textural gradient and thickening of the E horizon. Profiles P2 and P3 were classified as Ferralsols, were kaolinitic, with no redox conditions, and with predominance of eluviation/illuviation processes associated with pedoturbation, with a small increment of clay in the subsurface in both profiles. In profile P2, more so than in P3, there was still a strong influence of colluvial sediments, identified by the presence of a lithological discontinuity. For profile P4, a Plinthosol, located at the top of the toposequence, its formation was related to the action of weathering on the underlying acidic granite-gneiss rock. Despite the presence of plinthite, which denoted the occurrence of plinthization, the micromorphological description made it possible to state that it was a relictual condition whose formation occurred under past climatic conditions with higher water table level and which is currently being destroyed. MenosCoastal plains are characterized by low-elevation and small altitude variation and occupy an area of 57 million km2 worldwide. Ancient coastal plains that occur in the State of Rio de Janeiro (RJ), Brazil, have their pedological diversity neglected due to the generalization of some soil classes, underestimating the diversity of soils in these regions, hence limiting the evaluation for use and management. The aim of this study was to characterize the diversity of soils in a toposequence along an ancient coastal plain and to understand the pedogenetic processes involved. For this, soil pits were opened in the lower third (P1), middle third (P2), upper third (P3) and at the top (P4) of a toposequence. Soil profiles were characterized for morphological, physical, chemical, mineralogical and micromorphological properties. Profile P1 was classified as Planosol, being formed from colluvial sediments. In this profile, a lithological discontinuity was identified based on the irregularity of the values of silt/clay and coarse sand/fine sand ratios in subsurface. In this profile, limited drainage conditions were also observed. The main formation processes identified were ferrolysis and clay eluviation/illuviation, which promoted the increase of the textural gradient and thickening of the E horizon. Profiles P2 and P3 were classified as Ferralsols, were kaolinitic, with no redox conditions, and with predominance of eluviation/illuviation processes associated with pedoturbation, with a s... Mostrar Tudo |
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Palavras-Chave: |
Ferrolysis; Lithological discontinuity; Micropedology; Pedogenesis. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02974naa a2200265 a 4500
001 2139674
005 2022-03-11
008 2022 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1016/j.catena.2021.105894$2DOI
100 1 $aPEREIRA, M. G.
245 $aSoil genesis on the soft slopes of ancient coastal plains, southeastern Brazil.$h[electronic resource]
260 $c2022
520 $aCoastal plains are characterized by low-elevation and small altitude variation and occupy an area of 57 million km2 worldwide. Ancient coastal plains that occur in the State of Rio de Janeiro (RJ), Brazil, have their pedological diversity neglected due to the generalization of some soil classes, underestimating the diversity of soils in these regions, hence limiting the evaluation for use and management. The aim of this study was to characterize the diversity of soils in a toposequence along an ancient coastal plain and to understand the pedogenetic processes involved. For this, soil pits were opened in the lower third (P1), middle third (P2), upper third (P3) and at the top (P4) of a toposequence. Soil profiles were characterized for morphological, physical, chemical, mineralogical and micromorphological properties. Profile P1 was classified as Planosol, being formed from colluvial sediments. In this profile, a lithological discontinuity was identified based on the irregularity of the values of silt/clay and coarse sand/fine sand ratios in subsurface. In this profile, limited drainage conditions were also observed. The main formation processes identified were ferrolysis and clay eluviation/illuviation, which promoted the increase of the textural gradient and thickening of the E horizon. Profiles P2 and P3 were classified as Ferralsols, were kaolinitic, with no redox conditions, and with predominance of eluviation/illuviation processes associated with pedoturbation, with a small increment of clay in the subsurface in both profiles. In profile P2, more so than in P3, there was still a strong influence of colluvial sediments, identified by the presence of a lithological discontinuity. For profile P4, a Plinthosol, located at the top of the toposequence, its formation was related to the action of weathering on the underlying acidic granite-gneiss rock. Despite the presence of plinthite, which denoted the occurrence of plinthization, the micromorphological description made it possible to state that it was a relictual condition whose formation occurred under past climatic conditions with higher water table level and which is currently being destroyed.
653 $aFerrolysis
653 $aLithological discontinuity
653 $aMicropedology
653 $aPedogenesis
700 1 $aSILVA, R. C. da
700 1 $aPINHEIRO JUNIOR, C. R.
700 1 $aOLIVEIRA, F. S. de
700 1 $aSILVA NETO, E. C. da
700 1 $aFONTANA, A.
700 1 $aPACHECO, A. A.
700 1 $aPEDRON, F. de A.
773 $tCatena$gv. 210, 105894, Mar. 2022.
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Embrapa Solos (CNPS) |
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| Registros recuperados : 183 | |
| 4. |  | DUTRA, S. Estabelecimento de pastagens. Belém, PA, 1981. 6 p. il. Trabalho apresentado no Treinamento sobre Pastagem e Forrageiras, 1981, Belém. Publicação não convencional. Datilografado.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 5. | | DUTRA, S. Manejo de pastagens. Belém, PA, 1981. Não paginado. il. Trabalho apresentado no Treinamento sobre Pastagem e Forrageiras, 1981, Belém. Publicação não convencional. Datilografado.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 11. | | WOLLERSEN, T. W.; DUTRA, S. Matéria orgânica e algumas propriedades físico-químicas de Latossolos e Podzolicos da Amazônia. In: SIMPÓSIO DO TRÓPICO ÚMIDO, 1., 1984, Belém, PA. Anais. Belém, PA: EMBRAPA-CPATU, 1986. v. 1, p. 192-199. (EMBRAPA-CPATU. Documentos, 36). v.1 Clima e solo.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 14. | | SOUZA FILHO, A. P. S.; DUTRA, S. Desempenho de plantas forrageiras em consorciação em áreas de savana bem drenada no Estado do Amapá. In: REUNIÃO ANUAL DA SOCIEDADE BRASILEIRA DE ZOOTECNIA, 37., 2000, Viçosa, MG. Anais. Viçosa: SBZ, 2000. 1 CD-ROM. Resumo também publicado em: REUNIÃO ANUAL DA SOCIEDADE BRASILEIRA DE ZOOTECNIA, 37., 2000, Viçosa, MG. Resumos dos trabalhos apresentados. Viçosa, MG: Sociedade Brasileira de Zootecnia, 2000. p. 69.| Tipo: Artigo em Anais de Congresso |
| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 15. | | BAENA, A. R. C.; DUTRA, S. Teor de umidade em Latossolo Amarelo textura média sob diferentes tipos de cobertura utilizando-se sonda de nêutrons. In: SIMPÓSIO DO TRÓPICO ÚMIDO, 1., 1984, Belém, PA. Anais. Belém, PA: EMBRAPA-CPATU, 1986. v. 1, p. 466-473. (EMBRAPA-CPATU. Documentos, 36). v.1 Clima e solo.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 17. | | SOUZA FILHO, A. P. S.; DUTRA, S. Desempenho de bovinos em pastagens nativas de savana e de Brachiaria humidícola em diferentes cargas animais. In: REUNIÃO ANUAL DA SOCIEDADE BRASILEIRA DE ZOOTECNIA, 37., 2000, Viçosa, MG. Anais. Viçosa: SBZ, 2000. 1 CD-ROM. Resumo também publicado em: REUNIÃO ANUAL DA SOCIEDADE BRASILEIRA DE ZOOTECNIA, 37., 2000, Viçosa, MG. Resumos dos trabalhos apresentados. Viçosa, MG: Sociedade Brasileira de Zootecnia, 2000. p. 68.| Tipo: Artigo em Anais de Congresso |
| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 19. | | FLOHRSCHUTZ, G. H. H.; DUTRA, S. Relações técnicas na agricultura tradicional da zona Bragantina. In: SIMPÓSIO DO TRÓPICO ÚMIDO, 1., 1984, Belém, PA. Anais. Belém, PA: EMBRAPA-CPATU, 1986. v. 6, p. 373-385. (EMBRAPA-CPATU. Documentos, 36). v.6 Temas multidisciplinares.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| Registros recuperados : 183 | |
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| Nenhum registro encontrado para a expressão de busca informada. |
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