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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifierx6e6X3pFwXQZ3DUS8rS5/C7d8L
Repositorycptec.inpe.br/walmeida/2004/05.10.08.28   (restricted access)
Last Update2005:04.18.03.00.00 (UTC) administrator
Metadata Repositorycptec.inpe.br/walmeida/2004/05.10.08.28.50
Metadata Last Update2022:03.26.17.59.59 (UTC) administrator
Secondary KeyINPE-11154-PRE/6610
ISSN0038-075X
Citation KeyTomasellaHodn:1997:EsUnHy
TitleEstimating unsaturated hydraulic conductivity of Brazilian soils using soil-water retention data
Year1997
Monthoct
Access Date2024, Apr. 28
Secondary TypePRE PI
Number of Files1
Size1187 KiB
2. Context
Author1 Tomasella, Javier
2 Hodnett, M. G.
Resume Identifier1 8JMKD3MGP5W/3C9JHE3
Group1 DMA-INPE-MCT-BR
Affiliation1 CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil
e-Mail Addressfabia@cptec.inpe.br
JournalSoil Science
Volume162
Number10
Pages703-712
History (UTC)2005-04-18 19:13:12 :: Fabia -> administrator ::
2008-06-10 19:45:56 :: administrator -> estagiario ::
2010-05-11 16:53:06 :: estagiario -> marciana ::
2010-05-18 13:38:15 :: marciana -> administrator ::
2022-03-26 17:59:59 :: administrator -> marciana :: 1997
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Keywordseffective porosity data models
AbstractStudies to predict the impact of deforestation on climate in Amazonia have stimulated interest in the hydraulic properties of the soils of the region and the surrounding areas, Few directly measured hydraulic conductivity data are available; these were used to derive parameters to allow the unsaturated hydraulic conductivity-water content (K-theta) curve to be obtained from the more easily measured water retention curve, Relative hydraulic conductivity was modeled using the Brooks-Corey formula, whereas the saturated conductivity was calculated as a function of effective porosity from the expression proposed by Ahuja et al, Empirical relationships were fitted to seven different Brazilian soils, from 13 different sites, assembling about 2650 field conductivity values, The data for six of the soil types could be represented by a single set of parameters, with kaolinitic yellow latosolic soils from Amazonia requiring a separate set, Fitted relationships showed very high statistical significance, and the parameters derived were significantly different from those derived by Ahuja et al, for North American soils, To verify the proposed methodology, the parameters were derived using the complete data set (without the kaolinitic yellow latosol), excluding one soil type at a time, and checking the ability of the relationships to predict the conductivity of the soil not included in the fitting, In addition, the parameters obtained from the complete data set predicted hydraulic conductivities from the water release curves of five other Brazilian soils for which measured conductivity values were available.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção até 2016 > DMA > Estimating unsaturated hydraulic...
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4. Conditions of access and use
Languageen
Target FileTomasella_Estimating unsaturated.PDF
User Groupadministrator
marciana
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher denyfinaldraft
Read Permissiondeny from all and allow from 150.163
5. Allied materials
Next Higher Units8JMKD3MGPCW/46JKC45
DisseminationWEBSCI
Host Collectioncptec.inpe.br/walmeida/2003/04.25.17.12
6. Notes
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7. Description control
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