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Registro Completo |
Biblioteca(s): |
Embrapa Gado de Corte. |
Data corrente: |
11/12/1998 |
Data da última atualização: |
15/01/2014 |
Autoria: |
SOUZA, O. C. de. |
Título: |
Modern geomorphic processes along the Taquari river in the pantanal: a model for development of a humid tropical alluvial fam. |
Ano de publicação: |
1998 |
Fonte/Imprenta: |
Santa Barbara : University of California, 1998. |
Páginas: |
135p. |
Idioma: |
Inglês |
Notas: |
CNPGC. |
Conteúdo: |
Wetland management within the alluvial fan for the Taquari River in the Pantanal of Brazil requires understanding the channel-feomorphology. The alluvial fan of Taquari has an area of about 50,000km2, Analyses of hydrologic, geomorphic, grain size distribution, and remote sensing data allowed the development of a conceptual model that accounts for the identification of two distinct sections of the alluvial fan of the Taquari River, a meandering section and an anastromosing section. The meandering section is located in the region of the fan head. Temporal variability of discharge in this reach is due to seasonality of precipitation. Channel and active floodplain are entrenched within walls of older terrace deposits. There is a predominance of coarse material (>0,063 mm) in the river, river margins, and fllodplain. The anastromosing section begins at the intersection point of the fan approximately 100 km down the fan head. The unconfined character of the floodplain in the distral region of the fan is due to lower bank heights and progressive descrease of floodplain elevation in relation to river water level. Decreasing downstrean discharge is due to overbank flow. The decrease in suspended sediment concentration downstrean reveals that almost all the sediment load is deposited along the distal region of the alluvial fan. Decreasing grain size within sediments of the river, margins, and floodplain indicates that fine material is deposited in the fllodplain, while coarse material remains within the channels. Spectral mixture analysis of Landsat TM imagery, usiing sediment-laden water, clear water and vegetation revealed changes in the hydrological behavior of the Taquari River as enlarging floodplain area in the distral fan. MenosWetland management within the alluvial fan for the Taquari River in the Pantanal of Brazil requires understanding the channel-feomorphology. The alluvial fan of Taquari has an area of about 50,000km2, Analyses of hydrologic, geomorphic, grain size distribution, and remote sensing data allowed the development of a conceptual model that accounts for the identification of two distinct sections of the alluvial fan of the Taquari River, a meandering section and an anastromosing section. The meandering section is located in the region of the fan head. Temporal variability of discharge in this reach is due to seasonality of precipitation. Channel and active floodplain are entrenched within walls of older terrace deposits. There is a predominance of coarse material (>0,063 mm) in the river, river margins, and fllodplain. The anastromosing section begins at the intersection point of the fan approximately 100 km down the fan head. The unconfined character of the floodplain in the distral region of the fan is due to lower bank heights and progressive descrease of floodplain elevation in relation to river water level. Decreasing downstrean discharge is due to overbank flow. The decrease in suspended sediment concentration downstrean reveals that almost all the sediment load is deposited along the distal region of the alluvial fan. Decreasing grain size within sediments of the river, margins, and floodplain indicates that fine material is deposited in the fllodplain, while coarse ... Mostrar Tudo |
Palavras-Chave: |
Alluvial fan; Brasil; Leque aluvial; Model; Modelo; Rio Taquari; Taquari River. |
Thesagro: |
Geomorfologia; Hidrologia; Sensoriamento Remoto. |
Thesaurus Nal: |
Brazil; geomorphology; hydrology; Pantanal; remote sensing. |
Categoria do assunto: |
-- |
Marc: |
LEADER 02596nam a2200313 a 4500 001 1321143 005 2014-01-15 008 1998 bl uuuu m 00u1 u #d 100 1 $aSOUZA, O. C. de 245 $aModern geomorphic processes along the Taquari river in the pantanal$ba model for development of a humid tropical alluvial fam. 260 $aSanta Barbara : University of California$c1998 300 $a135p. 500 $aCNPGC. 520 $aWetland management within the alluvial fan for the Taquari River in the Pantanal of Brazil requires understanding the channel-feomorphology. The alluvial fan of Taquari has an area of about 50,000km2, Analyses of hydrologic, geomorphic, grain size distribution, and remote sensing data allowed the development of a conceptual model that accounts for the identification of two distinct sections of the alluvial fan of the Taquari River, a meandering section and an anastromosing section. The meandering section is located in the region of the fan head. Temporal variability of discharge in this reach is due to seasonality of precipitation. Channel and active floodplain are entrenched within walls of older terrace deposits. There is a predominance of coarse material (>0,063 mm) in the river, river margins, and fllodplain. The anastromosing section begins at the intersection point of the fan approximately 100 km down the fan head. The unconfined character of the floodplain in the distral region of the fan is due to lower bank heights and progressive descrease of floodplain elevation in relation to river water level. Decreasing downstrean discharge is due to overbank flow. The decrease in suspended sediment concentration downstrean reveals that almost all the sediment load is deposited along the distal region of the alluvial fan. Decreasing grain size within sediments of the river, margins, and floodplain indicates that fine material is deposited in the fllodplain, while coarse material remains within the channels. Spectral mixture analysis of Landsat TM imagery, usiing sediment-laden water, clear water and vegetation revealed changes in the hydrological behavior of the Taquari River as enlarging floodplain area in the distral fan. 650 $aBrazil 650 $ageomorphology 650 $ahydrology 650 $aPantanal 650 $aremote sensing 650 $aGeomorfologia 650 $aHidrologia 650 $aSensoriamento Remoto 653 $aAlluvial fan 653 $aBrasil 653 $aLeque aluvial 653 $aModel 653 $aModelo 653 $aRio Taquari 653 $aTaquari River
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Embrapa Gado de Corte (CNPGC) |
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Biblioteca(s): |
Embrapa Trigo. |
Data corrente: |
24/04/2010 |
Data da última atualização: |
10/08/2015 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Circulação/Nível: |
B - 1 |
Autoria: |
GUIMARÃES, A. A.; FERREIRA, E. A.; VARGAS, L.; SILVA, A. A.; VIANA, R. G.; DEMUNER, A. J.; CONCENÇO, G.; ASPIAZU, I.; GALON, L.; REIS, M. R.; SILVA, A. F. |
Afiliação: |
Guimarães, estudante UFLA; Ferreira, estudante UFV; LEANDRO VARGAS, CNPT; Silva, UFV; Viana, estudante UFV; Demuner, UFV; Concenço, estudante UFV; Aspiazu, estudante UFV; Galon, estudante UFV; Reis, estudante UFV; Silva, estudante UFV. |
Título: |
Composição química da cera epicuticular de biótipos de azevém resistente e suscetível ao Glyphosate. |
Ano de publicação: |
2009 |
Fonte/Imprenta: |
Planta Daninha, Viçosa, v. 27, n. 1, p. 149-154, 2009. |
Idioma: |
Português |
Palavras-Chave: |
Transgenia. |
Thesagro: |
Cromatografia; Lolium Multiflorum; Resistência. |
Categoria do assunto: |
-- |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/127666/1/SP-15727.pdf
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Marc: |
LEADER 00782naa a2200277 a 4500 001 1852657 005 2015-08-10 008 2009 bl uuuu u00u1 u #d 100 1 $aGUIMARÃES, A. A. 245 $aComposição química da cera epicuticular de biótipos de azevém resistente e suscetível ao Glyphosate. 260 $c2009 650 $aCromatografia 650 $aLolium Multiflorum 650 $aResistência 653 $aTransgenia 700 1 $aFERREIRA, E. A. 700 1 $aVARGAS, L. 700 1 $aSILVA, A. A. 700 1 $aVIANA, R. G. 700 1 $aDEMUNER, A. J. 700 1 $aCONCENÇO, G. 700 1 $aASPIAZU, I. 700 1 $aGALON, L. 700 1 $aREIS, M. R. 700 1 $aSILVA, A. F. 773 $tPlanta Daninha, Viçosa$gv. 27, n. 1, p. 149-154, 2009.
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