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| Registros recuperados : 2 | |
| 1. |  | CARVALHO, A. C. F. de; SILVA, D. D. de; VASCO NETO, H. L. S.; SILVA, T. I. B. da; CUNHA, W. R. X.; REVORÊDO, R. G.; MELO, L. E. H. de. Novos dados de soroprevalência da artrite-encefalite caprina em rebanhos do estado de Pernambuco. In: SIMPÓSIO INTERNACIONAL SOBRE CAPRINOS E OVINOS DE CORTE, 4.; FEIRA NACIONAL DO AGRONEGÓCIO DA CAPRINO-OVINOCULTURA DE CORTE, 3., 2009, João Pessoa. Anais... João Pessoa: EMEPA-PB, 2009. 1 CD-ROM. 3 f.| Biblioteca(s): Embrapa Caprinos e Ovinos. |
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| 2. | | BARROS, J. D.; ARCOVERDE, G. F. B.; CARVALHO, A. C. F. de; VILA, A. J. T.; FAUSTINO, A. B.; MELO, A. A. de; VERAS, A. L.; MARTINS, C. S. G.; MELO, D. M. A. de; SANTOS, D. C. dos; VERDE, D. C. A. L.; TROVÃO, D. M. de B. M.; SILVA, E. S. da; SILVA, E. D. da C.; BARBOSA, E.; SILVA, F. G. C. da; ARAÚJO, H. F. P. de; MAIA, I. C.; SA, I. B.; RODRIGUES, J. de D.; CUNHA, J. E.; COSTA, J. D. da; CARVALHO, J. V.; LIMA, L. de C.; SANTOS, L. M. dos; ARAÚJO, L. N. de; COELHO, L. F. M.; VEIGA, M. E. B. da; ARAÚJO, M. C.; OLIVEIRA, M. G. de; MELO, M. G. P. de; GADELHA, M. A. da M. B.; SANTOS, M. C. dos; LIRA FILHO, P. de B.; LIMA, R. B. de; BATISTA, R. D.; OLIVEIRA, T. C. T. de; BEZERRA, U. A.; SOUZA, V. N. de. Processo participativo sobre degradação da terra em regiões do Semiárido brasileiro. São José dos Campos: SP, INPE, 2023. 53 p. il. color sid.inpe.br/mtc-m21d/2023/04.18.16.48-RPQ| Biblioteca(s): Embrapa Semiárido. |
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| Registros recuperados : 2 | |
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Registro Completo
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Biblioteca(s): |
Embrapa Pantanal. |
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Data corrente: |
29/05/2017 |
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Data da última atualização: |
19/12/2022 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 1 |
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Autoria: |
FURQUIM, S. A. C.; SANTOS, M. A.; VIDOCA, T. T.; BALBINO, M de A.; CARDOSO, E. L. |
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Afiliação: |
SHEILA APARECIDA CORREIA FURQUIM, Universidade Federal de São Paulo-UNIFESP; MARJORY ARAUJO SANTOS, UNIVERSIDADE FEDERAL DE SÃO PAULO-UNIFESP; THIAGO TAVARES VIDOCA, Universidade Federal de São Paulo-UNIFESP; MARCELO DE ALMEIDA BALBINO, Universidade de São Paulo-USP, São Paulo; EVALDO LUIS CARDOSO, CPAP. |
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Título: |
Salt-affected soils evolution and fluvial dynamics in the Pantanal wetland, Brazil. |
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Ano de publicação: |
2017 |
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Fonte/Imprenta: |
Geoderma, v. 286, n. 15, p. 139-152, 2017. |
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DOI: |
10.1016/j.geoderma.2016.10.030 |
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Idioma: |
Português |
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Conteúdo: |
In the Nhecolândia, a subregion of the Pantanal wetland, saline lakes and their associated Saline-Sodic soils have been degraded due to the atypical input of freshwater from seasonal flooding. In the present work, the soils in and around three brackish lakes that have experienced degradation (Carandazal, Cerca and Banhado lakes) were studied through a detailed morphological survey and chemical analyses to understand their genesis and establish genetic relationship with the Saline-Sodic soils of the saline lakes. The studied soils have Bnc and Bc horizons with morphological and chemical similarities to the Bnx formed around the saline lakes, presenting greenish colors, hard consistencies and, generally, the highest values of pH, exchangeable sodium percentage (ESP), sodium adsorption ratio (SAR) and electrical conductivity in the saturated paste (ECs) of each profile. In contrast, the near-surface horizons tend to present the lowest values of pH and the highest amounts of Al3+ saturation and exchangeable H + Al. These data point to the replacement of salinization/solonization around the saline lakes to the solodization process in the studied soils, with leaching of exchangeable bases, their substitution by Al3+ and H+ and a consequent decrease in pH, first at shallow depths and later in the whole profile. Solodization occurs to a lower degree in the soils associated with the Carandazal lake, which has a predominance of Solonetzes and the closest water pH and electrical conductivity (EC) to the saline lakes, and to a higher degree in the soils related to the Banhado lake, which has a predominance of Solods and the most similar water pH and EC to the freshwaters of the Nhecolândia. The Cerca lake has an intermediate water geochemistry between the studied lakes and an equal prevalence of Solodized Solonetzes and Solods. Soil leaching occurs due to increasing inundation by freshwater through erosion around the saline lakes, primarily involving formation of new intermittent watercourses. MenosIn the Nhecolândia, a subregion of the Pantanal wetland, saline lakes and their associated Saline-Sodic soils have been degraded due to the atypical input of freshwater from seasonal flooding. In the present work, the soils in and around three brackish lakes that have experienced degradation (Carandazal, Cerca and Banhado lakes) were studied through a detailed morphological survey and chemical analyses to understand their genesis and establish genetic relationship with the Saline-Sodic soils of the saline lakes. The studied soils have Bnc and Bc horizons with morphological and chemical similarities to the Bnx formed around the saline lakes, presenting greenish colors, hard consistencies and, generally, the highest values of pH, exchangeable sodium percentage (ESP), sodium adsorption ratio (SAR) and electrical conductivity in the saturated paste (ECs) of each profile. In contrast, the near-surface horizons tend to present the lowest values of pH and the highest amounts of Al3+ saturation and exchangeable H + Al. These data point to the replacement of salinization/solonization around the saline lakes to the solodization process in the studied soils, with leaching of exchangeable bases, their substitution by Al3+ and H+ and a consequent decrease in pH, first at shallow depths and later in the whole profile. Solodization occurs to a lower degree in the soils associated with the Carandazal lake, which has a predominance of Solonetzes and the closest water pH and electrical conduc... Mostrar Tudo |
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Palavras-Chave: |
Fluvial dynamics. |
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Thesagro: |
Água Salina; Solo Sódico. |
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Thesaurus NAL: |
Saline sodic soils; Saline water; Soil salts. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 02752naa a2200253 a 4500
001 2070180
005 2022-12-19
008 2017 bl uuuu u00u1 u #d
024 7 $a10.1016/j.geoderma.2016.10.030$2DOI
100 1 $aFURQUIM, S. A. C.
245 $aSalt-affected soils evolution and fluvial dynamics in the Pantanal wetland, Brazil.$h[electronic resource]
260 $c2017
520 $aIn the Nhecolândia, a subregion of the Pantanal wetland, saline lakes and their associated Saline-Sodic soils have been degraded due to the atypical input of freshwater from seasonal flooding. In the present work, the soils in and around three brackish lakes that have experienced degradation (Carandazal, Cerca and Banhado lakes) were studied through a detailed morphological survey and chemical analyses to understand their genesis and establish genetic relationship with the Saline-Sodic soils of the saline lakes. The studied soils have Bnc and Bc horizons with morphological and chemical similarities to the Bnx formed around the saline lakes, presenting greenish colors, hard consistencies and, generally, the highest values of pH, exchangeable sodium percentage (ESP), sodium adsorption ratio (SAR) and electrical conductivity in the saturated paste (ECs) of each profile. In contrast, the near-surface horizons tend to present the lowest values of pH and the highest amounts of Al3+ saturation and exchangeable H + Al. These data point to the replacement of salinization/solonization around the saline lakes to the solodization process in the studied soils, with leaching of exchangeable bases, their substitution by Al3+ and H+ and a consequent decrease in pH, first at shallow depths and later in the whole profile. Solodization occurs to a lower degree in the soils associated with the Carandazal lake, which has a predominance of Solonetzes and the closest water pH and electrical conductivity (EC) to the saline lakes, and to a higher degree in the soils related to the Banhado lake, which has a predominance of Solods and the most similar water pH and EC to the freshwaters of the Nhecolândia. The Cerca lake has an intermediate water geochemistry between the studied lakes and an equal prevalence of Solodized Solonetzes and Solods. Soil leaching occurs due to increasing inundation by freshwater through erosion around the saline lakes, primarily involving formation of new intermittent watercourses.
650 $aSaline sodic soils
650 $aSaline water
650 $aSoil salts
650 $aÁgua Salina
650 $aSolo Sódico
653 $aFluvial dynamics
700 1 $aSANTOS, M. A.
700 1 $aVIDOCA, T. T.
700 1 $aBALBINO, M de A.
700 1 $aCARDOSO, E. L.
773 $tGeoderma$gv. 286, n. 15, p. 139-152, 2017.
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