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Biogeosciences An interactive open-access journal of the European Geosciences Union
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In low oxygen environments, the lack of oxygen influences sediment biogeochemistry and in turn sediment-water fluxes. These nonlinear interactions are often missing from biogeochemical circulation models because sediment models are computationally expensive. A method for parameterizing realistic sediment-water fluxes is presented and applied to the Mississippi River Dead Zone where high primary production, stimulated by excess nutrient loads, promotes low bottom water conditions in summer.
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Articles | Volume 13, issue 1
Biogeosciences, 13, 77–94, 2016
https://doi.org/10.5194/bg-13-77-2016

Special issue: Low oxygen environments in marine, fresh and estuarine...

Biogeosciences, 13, 77–94, 2016
https://doi.org/10.5194/bg-13-77-2016

Research article 15 Jan 2016

Research article | 15 Jan 2016

Parameterization of biogeochemical sediment–water fluxes using in situ measurements and a diagenetic model

A. Laurent et al.

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Short summary
In low oxygen environments, the lack of oxygen influences sediment biogeochemistry and in turn sediment-water fluxes. These nonlinear interactions are often missing from biogeochemical circulation models because sediment models are computationally expensive. A method for parameterizing realistic sediment-water fluxes is presented and applied to the Mississippi River Dead Zone where high primary production, stimulated by excess nutrient loads, promotes low bottom water conditions in summer.
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