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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Veröffentlicht in:	Scientific reports 2020-05, Vol.10 (1), p.8142-8142, Article 8142
Hauptverfasser:	Wogelius, R. A., Milodowski, A. E., Field, L. P., Metcalfe, R., Lowe, T., van Veelen, A., Carpenter, G., Norris, S., Yardley, B.
Format:	Artikel
Sprache:	eng
Schlagworte:	704/172 704/242 Contaminants Crystalline rocks Diffusion Environmental science Experiments Geology GEOSCIENCES Granite Groundwater Humanities and Social Sciences Laboratories Lithology Mass transport multidisciplinary Nutrients Permeability Science Science (multidisciplinary) Solutes Structural analysis Void space
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