Mineral reaction kinetics constrain the length scale of rock matrix diffusion

Mass transport by aqueous fluids is a dynamic process in shallow crustal systems, redistributing nutrients as well as contaminants. Rock matrix diffusion into fractures (void space) within crystalline rock has been postulated to play an important role in the transient storage of solutes. The reacted...

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Detalles Bibliográficos
Autores principales: Wogelius, R. A., Milodowski, A. E., Field, L. P., Metcalfe, R., Lowe, T., van Veelen, A., Carpenter, G., Norris, S., Yardley, B.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7235024/
https://www.ncbi.nlm.nih.gov/pubmed/32424316
http://dx.doi.org/10.1038/s41598-020-65113-x

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7235024/
https://www.ncbi.nlm.nih.gov/pubmed/32424316
http://dx.doi.org/10.1038/s41598-020-65113-x

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