Modeling denitrification in aquatic sediments
Modeling denitrification in aquatic sediments
Date
2008-10-10
Authors
Fennel, Katja
Brady, Damian C.
DiToro, Dominic
Fulweiler, Robinson W.
Gardner, Wayne S.
Giblin, Anne E.
McCarthy, Mark J.
Rao, Alexandra
Seitzinger, Sybil P.
Thouvenot-Korppoo, Marie
Tobias, Craig R.
Brady, Damian C.
DiToro, Dominic
Fulweiler, Robinson W.
Gardner, Wayne S.
Giblin, Anne E.
McCarthy, Mark J.
Rao, Alexandra
Seitzinger, Sybil P.
Thouvenot-Korppoo, Marie
Tobias, Craig R.
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Keywords
Denitrification
Diagenetic model
Sediment
Diagenetic model
Sediment
Abstract
Sediment denitrification is a major pathway of fixed nitrogen loss from aquatic systems. Due to technical difficulties in measuring this process and its spatial and temporal variability, estimates of local, regional and global denitrification have to rely on a combination of measurements and models. Here we review approaches to describing denitrification in aquatic sediments, ranging from mechanistic diagenetic models to empirical parameterizations of nitrogen fluxes across the sediment-water interface. We also present a compilation of denitrification measurements and ancillary data for different aquatic systems, ranging from freshwater to marine. Based on this data compilation we reevaluate published parameterizations of denitrification. We recommend that future models of denitrification use (1) a combination of mechanistic diagenetic models and measurements where bottom waters are temporally hypoxic or anoxic, and (2) the much simpler correlations between denitrification and sediment oxygen consumption for oxic bottom waters. For our data set, inclusion of bottom water oxygen and nitrate concentrations in a multivariate regression did not improve the statistical fit.
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Author Posting. © The Author(s), 2008. This is the author's version of the work. It is posted here by permission of Springer for personal use, not for redistribution. The definitive version was published in Biogeochemistry 93 (2009): 159-178, doi:10.1007/s10533-008-9270-z.