Liquid flow reversibly creates a macroscopic surface charge gradient

The charging and dissolution of mineral surfaces in contact with flowing liquids are ubiquitous in nature, as most minerals in water spontaneously acquire charge and dissolve. Mineral dissolution has been studied extensively under equilibrium conditions, even though non-equilibrium phenomena are per...

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Detalles Bibliográficos
Autores principales: Ober, Patrick, Boon, Willem Q., Dijkstra, Marjolein, Backus, Ellen H. G., van Roij, René, Bonn, Mischa
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8253779/
https://www.ncbi.nlm.nih.gov/pubmed/34215740
http://dx.doi.org/10.1038/s41467-021-24270-x

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8253779/
https://www.ncbi.nlm.nih.gov/pubmed/34215740
http://dx.doi.org/10.1038/s41467-021-24270-x

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