Root System Scale Models Significantly Overestimate Root Water Uptake at Drying Soil Conditions

Soil hydraulic conductivity (k(soil)) drops significantly in dry soils, resulting in steep soil water potential gradients (ψ(s)) near plant roots during water uptake. Coarse soil grid resolutions in root system scale (RSS) models of root water uptake (RWU) generally do not spatially resolve this gra...

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Detalles Bibliográficos
Autores principales: Khare, Deepanshu, Selzner, Tobias, Leitner, Daniel, Vanderborght, Jan, Vereecken, Harry, Schnepf, Andrea
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Frontiers Media S.A. 2022
Materias:
Plant Science
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8882956/
https://www.ncbi.nlm.nih.gov/pubmed/35237283
http://dx.doi.org/10.3389/fpls.2022.798741

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8882956/
https://www.ncbi.nlm.nih.gov/pubmed/35237283
http://dx.doi.org/10.3389/fpls.2022.798741

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