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1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemtc-m16b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositóriocptec.inpe.br/walmeida/2004/08.04.11.14
Última Atualização2007:08.24.12.45.12 (UTC) administrator
Repositório de Metadadoscptec.inpe.br/walmeida/2004/08.04.11.14.45
Última Atualização dos Metadados2022:03.26.18.02.25 (UTC) administrator
Chave SecundáriaINPE-14836-PRE/9750
Chave de CitaçãoHodnettToCuNoWaOlMú:2004:PrStGe
TítuloProcesses of streamflow generation in a headwater catchment in central Amazonia
FormatoCD-ROM
ProjetoLBA
Ano2004
Data de Acesso01 maio 2024
Tipo SecundárioPRE CN
Número de Arquivos1
Tamanho2612 KiB
2. Contextualização
Autor1 Hodnett, Martin George
2 Tomasella, Javier
3 Cuartas, Luz Adriana
4 Nobre, Antonio Donato
5 Waterloo, Maarten
6 Oliveira, Sylvia Mota de
7 Múnera, J.
Identificador de Curriculo1
2 8JMKD3MGP5W/3C9JHE3
Grupo1 DMA-INPE-MCT-BR
2 DMA-INPE-MCT-BR
Afiliação1 CPTEC-INPE-Cachoeira -12630-000-SP-Brasil
Endereço de e-Mailfabia@cptec.inpe.br
Nome do EventoConferencia Cientifica do LBA, 3.
Localização do EventoBrasilia
Data27-29 jul.
Título do LivroAnais
Tipo TerciárioPosters
OrganizaçãoLBA
Histórico (UTC)2006-11-17 21:45:55 :: administrator -> estagiario ::
2007-11-09 11:41:27 :: estagiario -> administrator ::
2008-06-10 21:19:55 :: administrator -> estagiario ::
2010-05-11 16:54:11 :: estagiario -> administrator ::
2022-03-26 18:02:25 :: administrator -> marciana :: 2004
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
ResumoIn 2002 and 2003, runoff from the Asu catchment (6.37 km2) was 1455 mm and 832 mm, of which 45% and 31% was stormflow respectively. Earlier studies in the Barro Branco catchment (1.3 km2) in Reserva Ducke (with similar geology and soils) showed that stormflow was 9% of total runoff in 1981, 1982 and 1983. Other studies in the same catchment suggested that the storm runoff was mainly generated from the valley floor, where the water table is close to the soil surface, leading to saturation excess overland flow (SOF). The Asu data confirm that the valley floor is the source of the storm runoff. The water table in the valley floor is controlled by two factors, (i) in the short-term, local vertical recharge direct to the water table and (ii) in the longer term, the discharge of groundwater from beneath the plateau and slope areas, fed by deep drainage (recharge) from these areas. There is also some evidence that interflow and return flow contribute to storm runoff in very large events. The main reason for the large difference in storm runoff between the catchments is that in the much larger Asu catchment, the proportion of the catchment occupied by valley floor (32%), with a shallow water table, is much greater than in the Barro Branco. In addition, the rainfall was well above average in 2002. These results show that it may not be appropriate to scale up from process studies in very small catchments, because of scale-related changes in processes.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção até 2016 > DMA > Processes of streamflow...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/cptec.inpe.br/walmeida/2004/08.04.11.14
URL dos dados zipadoshttp://urlib.net/zip/cptec.inpe.br/walmeida/2004/08.04.11.14
Idiomaen
Arquivo Alvohodnett_processes.pdf
Grupo de UsuáriosFabia
administrator
estagiario
Visibilidadeshown
Detentor da CópiaSID/SCD
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/46JKC45
Acervo Hospedeirocptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Campos Vaziosarchivingpolicy archivist callnumber copyright creatorhistory descriptionlevel dissemination documentstage doi edition editor electronicmailaddress identifier isbn issn keywords label lineage mark mirrorrepository nextedition notes numberofvolumes orcid pages parameterlist parentrepositories previousedition previouslowerunit progress publisher publisheraddress readergroup readpermission rightsholder schedulinginformation secondarydate secondarymark serieseditor session shorttitle sponsor subject tertiarymark type url versiontype volume
7. Controle da descrição
e-Mail (login)marciana
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