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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifierx6e6X3pFwXQZ3DUS8rS5/Ckxxm
Repositorycptec.inpe.br/walmeida/2004/06.02.09.15
Last Update2004:11.26.02.00.00 (UTC) administrator
Metadata Repositorycptec.inpe.br/walmeida/2004/06.02.09.15.30
Metadata Last Update2022:03.26.18.00.03 (UTC) administrator
Secondary KeyINPE-11946-PRE/7292
ISSN1027-5606
Citation KeyHodnettVenMarOyaTom:1997:I.CoPl
TitleSoil water storage and groundwater behaviour in a catenary sequence beneath forest in central Amazonia: I. Comparisons between plateau, slope and valley floor
Year1997
Monthmay/jun
Access Date2024, May 16
Secondary TypePRE PI
Number of Files1
Size1720 KiB
2. Context
Author1 Hodnett, M. G.
2 Vendrame, I.
3 Marques Filho, A. de O.
4 Oyama, Marcos D.
5 Tomasella, Javier
Resume Identifier1
2
3
4
5 8JMKD3MGP5W/3C9JHE3
Group1 DMA-INPE-MCT-BR
Affiliation1 CPTEC-INPE-Cachoeria Paulista-12630-000-SP-Brasil
e-Mail Addressfabia@cptec.inpe.br
JournalHydrology and Earth System Sciences
Volume1
Number2
Pages265-278
History (UTC)2005-01-14 16:39:16 :: Fabia -> administrator ::
2008-06-10 19:46:29 :: administrator -> estagiario ::
2010-05-11 16:53:25 :: 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
central Amazonia
topo sequence
AbstractSoil water storage was monitored in three landscape elements in the forest (plateau, slope and valley floor) over a 3 year period to identify differences in sub-surface hydrological response. Under the plateau and slope, the changes of storage were very similar and there was no indication of surface runoff on the slope. The mean maximum seasonal storage change was 156 mm in the 2 m profile but it was clear that, in the dry season, the forest was able to take up water from below 3.6 m. Soil water availability was low. Soil water storage changes in the valley were dominated by the behaviour of a shallow water table which, in normal years, varied between 0.1 m below the surface at the end of the wet season and 0.8 m at the end of the dry season. Soil water storage changes were small because root uptake was largely replenished by groundwater flow towards the stream. The groundwater behaviour is controlled mainly by the deep drainage from beneath the plateau and slope areas. The groundwater gradient beneath the slope indicated that recharge beneath the plateau and slope commences only after the soil water deficits from the previous dry season have been replenished. Following a wet season with little recharge, the water table fell, ceasing to influence the valley soil water storage, and the stream dried up. The plateau and slope, a zone of very high porosity between 0.4 and 1.1 m, underlain by a less conductive layer, is a probable route for interflow during, and for a few hours after, heavy and prolonged rainfall.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção até 2016 > DMA > Soil water storage...
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4. Conditions of access and use
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zipped data URLhttp://mtc-m16b.sid.inpe.br/zip/x6e6X3pFwXQZ3DUS8rS5/Ckxxm
Languageen
Target FileHodnett_Soil water_I_Comparisons.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/bibdigital/2022/03.26.17.47 3
DisseminationWEBSCI; PORTALCAPES.
Host Collectioncptec.inpe.br/walmeida/2003/04.25.17.12
6. Notes
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