Determining a composite value for the saturated hydraulic conductivity in a recharge area of the Guarani Aquifer System, using pedotransfer functions

ABSTRACT The saturated hydraulic conductivity (Ks) is an essential property for modeling water and contaminants movement into aquifers. However, Ks is extremely variable, even when considering nearby locations, which poses a challenge for modeling at catchment scales. Field measurements of Ks are mo...

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Váldodahkkit:	Marcelo Eduardo Dias de Oliveira, Didier Gastmans, Marcelo Donadelli Sacchi, Rodrigo Esteves Rocha, Camila de Lima, Vinícius dos Santos
Materiálatiipa:	Artigo
Giella:	Inglês
Almmustuhtton:	Associação Brasileira de Recursos Hídricos 2021-12-01
Ráidu:	RBRH
Fáttát:	Guarani Aquifer System Hydraulic conductivity Pedotransfer function Recharge area
Liŋkkat:	http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2318-03312021000100237&tlng=en
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