Control of the diffusive boundary layer on benthic fluxes: a model study

A simple, steady state, reaction-diffusion diagenesis model is used to quantify the possible error associated with benthic flux measurements which neglect the presence of the diffusive boundary layer (DBL). Model application is restricted to non-bioturbated, fine-grained sediments in which oxygen co...

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Veröffentlicht in:Marine ecology. Progress series (Halstenbek) 2005-05, Vol.292, p.61-74
Hauptverfasser: Kelly-Gerreyn, B. A., Hydes, D. J., Waniek, J. J.
Format: Artikel
Sprache:eng
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Zusammenfassung:A simple, steady state, reaction-diffusion diagenesis model is used to quantify the possible error associated with benthic flux measurements which neglect the presence of the diffusive boundary layer (DBL). Model application is restricted to non-bioturbated, fine-grained sediments in which oxygen consumption is dominated (~65% of the consumption budget) by organic carbon degradation, oxygen penetration depths are low (
ISSN:0171-8630
1616-1599
DOI:10.3354/meps292061