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

Pub. Date : 2004 Jan

PMID : 14630097






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1 Unsteady diffusional mass transfer at the sediment/water interface: Theory and significance for SOD measurement. Water superoxide dismutase 1 Homo sapiens
2 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 delta(D) in the water and the penetration depth delta in the sediment. Water superoxide dismutase 1 Homo sapiens
3 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 delta(D) in the water and the penetration depth delta in the sediment. Water superoxide dismutase 1 Homo sapiens
4 A model was developed for the unsteady response of SOD and DO profiles near the sediment/water interface. Water superoxide dismutase 1 Homo sapiens
5 If flow conditions in the chamber and at the natural sediment/water interface are much different, measured SOD values have to be adjusted. Water superoxide dismutase 1 Homo sapiens