Unsteady diffusional mass transfer at the sediment/water interface: Theory and significance for SOD measurement

Dissolved oxygen uptake at a sediment/water interface (SOD) is controlled by mass transport and/or biochemical reactions in two adjacent boundary layers: the diffusive boundary layer δ D in the water and the penetration depth δ in the sediment. Either one of those boundary layers or both can be cont...

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Veröffentlicht in:	Water research (Oxford) 2004, Vol.38 (1), p.1-12
Hauptverfasser:	Higashino, Makoto, Gantzer, Charles J., Stefan, Heinz G.
Format:	Artikel
Sprache:	eng
Schlagworte:	Boundary layer Dissolved oxygen Earth sciences Earth, ocean, space Exact sciences and technology Forecasting Geochemistry Geologic Sediments - chemistry Hydrology Hydrology. Hydrogeology Mass transfer Mineralogy Models, Theoretical Oxygen Oxygen - analysis Oxygen - chemistry Oxygen demand Sediment Silicates Solubility Water - chemistry Water geochemistry
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