Solute Exchange by Convection Within Estuarine Sediments

The rates of material transport through sediments are central to determining the biochemical status of sediments. Transport within sediments can occur by molecular diffusion through porewaters and by the activities of burrowing biological organisms, but a number of physical processes can enhance tra...

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Veröffentlicht in:	Estuarine, coastal and shelf science coastal and shelf science, 1996, Vol.42 (2), p.171-183
Hauptverfasser:	Webster, I.T., Norquay, S.J., Ross, F.C., Wooding, R.A.
Format:	Artikel
Sprache:	eng
Schlagworte:	Brackish convection Earth sciences Earth, ocean, space estuarine sediments Exact sciences and technology Geochemistry Marine Mineralogy porewater transport Silicates Water geochemistry
Online-Zugang:	Volltext
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