Quasi‐Saturated Layer: Implications for Estimating Recharge and Groundwater Modeling

This study presents an extension of the concept of “quasi‐saturation” to a quasi‐saturated layer, defined as the uppermost dynamic portion of the saturated zone subject to water table fluctuations. Entrapped air here may cause substantial reductions in the hydraulic conductivity (K) and fillable por...

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Detalles Bibliográficos
Autores principales: Gonçalves, Roger D., Teramoto, Elias H., Engelbrecht, Bruno Z., Alfaro Soto, Miguel A., Chang, Hung K., van Genuchten, Martinus Th.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Blackwell Publishing Ltd 2019
Materias:
Research Papers/
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7318159/
https://www.ncbi.nlm.nih.gov/pubmed/31187874
http://dx.doi.org/10.1111/gwat.12916

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7318159/
https://www.ncbi.nlm.nih.gov/pubmed/31187874
http://dx.doi.org/10.1111/gwat.12916

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