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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifierx6e6X3pFwXQZ3DUS8rS5/CkxN6
Repositorycptec.inpe.br/walmeida/2004/06.02.09.28
Last Update2004:11.26.02.00.00 (UTC) administrator
Metadata Repositorycptec.inpe.br/walmeida/2004/06.02.09.28.19
Metadata Last Update2022:03.26.18.00.03 (UTC) administrator
Secondary KeyINPE-11945-PRE/7291
ISSN1027-5606
Citation KeyHodnettVenMarOyaTom:1997:FlWaTa
TitleSoil water storage and groundwater behaviour in a catenary sequence beneath forest in central Amazonia. II. Floodplain water table behaviour and implications for streamflow generation
Year1997
Monthmay/jun
Access Date2025, May 09
Secondary TypePRE PI
Number of Files1
Size1687 KiB
2. Context
Author1 Hodnett, M. G.
2 Vendrame, I.
3 Marques Filho, A. de O.
4 Oyama, M. D.
5 Tomasella, Javier
Resume Identifier1
2
3
4
5 8JMKD3MGP5W/3C9JHE3
Group1 DMA-INPE-MCT-BR
Affiliation1 CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil
e-Mail Addressfabia@cptec.inpe.br
JournalHydrology and Earth System Sciences
Volume1
Number2
Pages279-290
History (UTC)2005-01-14 16:38:11 :: Fabia -> administrator ::
2008-06-10 19:46:30 :: administrator -> estagiario ::
2010-05-11 16:53:26 :: estagiario -> administrator ::
2022-03-26 18:00:03 :: administrator -> marciana :: 1997
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Keywordssoil storage
caternary sequence
water table
AbstractAbstract Valley floor groundwater level data collected during the ABRACOS project (Gash et al. 1996), and published streamflow data from small forested catchments in geomorphologically similar areas nearby have been analysed to improve the understanding of the processes of streamflow generation. Early in the wet season, the floodplain water table is typically at 0.8 m depth, or less, and receives only local, vertical recharge. Large storms may create a groundwater ridge beneath the floodplain, temporarily creating a gradient in the direction of the hilislope. Later in the wet season, floodpiain water levels are controlled primarily by the discharge of groundwater which maintains the dry season streamflow. The groundwater is recharged by deep drainage from beneath the plateau and slope areas once the dry season soil water deficit has been overcome. In the late wet season, the water level is almost at the floodplain surface and may create seeps on the lower slopes in very wet years. For the period 1966-1989, the recharge was estimated to range from 290 mm to 1601 mm with a mean of 1087 mm. Published data show that baseflow is 91% of annual runoff. Stormflow is generated on the floodplain, and water table recessions after rainfall events show that the runoff response depends on the depth to the water table. These results are from areas with deeply weathered and permeable soils; in areas of Amazonia with shallower soils, the predominant flow generation processes will differ (Elsenbeer and Lack, 1996).
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção até 2016 > DMA > Soil water storage...
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4. Conditions of access and use
data URLhttp://urlib.net/ibi/x6e6X3pFwXQZ3DUS8rS5/CkxN6
zipped data URLhttp://urlib.net/zip/x6e6X3pFwXQZ3DUS8rS5/CkxN6
Languageen
Target FileHodnett_Soil water_II_Floodp.pdf
User Groupadministrator
Visibilityshown
Copy HolderSID/SCD
Archiving Policyallowpublisher allowfinaldraft
Read Permissionallow from all
5. Allied materials
Next Higher Units8JMKD3MGPCW/46JKC45
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.14.50.34 16
sid.inpe.br/bibdigital/2022/03.26.17.47 5
DisseminationWEBSCI; PORTALCAPES.
Host Collectioncptec.inpe.br/walmeida/2003/04.25.17.12
6. Notes
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7. Description control
e-Mail (login)marciana
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