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...

وصف كامل

التفاصيل البيبلوغرافية

الحاوية / القاعدة:	Revista Brasileira de Recursos Hídricos
المؤلفون الرئيسيون:	Marcelo Eduardo Dias de Oliveira, Didier Gastmans, Marcelo Donadelli Sacchi, Rodrigo Esteves Rocha, Camila de Lima, Vinícius dos Santos
التنسيق:	مقال
اللغة:	الإنجليزية
منشور في:	Associação Brasileira de Recursos Hídricos 2021-12-01
الموضوعات:	Guarani Aquifer System Hydraulic conductivity Pedotransfer function Recharge area
الوصول للمادة أونلاين:	http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2318-03312021000100237&tlng=en