Diagenetic models of interstitial nitrate profiles in deep sea suboxic sediments1
- 1 July 1982
- journal article
- research article
- Published by Wiley in Limnology and Oceanography
- Vol. 27 (4), 624-638
- https://doi.org/10.4319/lo.1982.27.4.0624
Abstract
Quantitative models are developed to describe three different profiles of nitrate observed in the porewater of pelagic sediments: nitrification only is observed; a surficial zone of nitrification is underlain by a zone of denitrification; the zone of nitrification is underlain by a zone of no reaction and then a zone of denitrification. Oxygen consumption and nitrate re duction are assumed to be first‐order processes. by fitting the models to observed [NO3−] profiles, we have estimated benthic nitrate and oxygen fluxes, denitrification rates, first‐order rates constants for O2, organic matter, and NO3− consumption, and the stoichiometric ratio d[NO3−]:d[O2].This publication has 4 references indexed in Scilit:
- Oxygen Consumption in Pelagic Marine SedimentsScience, 1980
- Early oxidation of organic matter in pelagic sediments of the eastern equatorial Atlantic: suboxic diagenesisGeochimica et Cosmochimica Acta, 1979
- Benthic community respiration in the N.W. Atlantic Ocean: in situ measurements from 40 to 5200 mMarine Biology, 1978
- Kinetic models of diagenesis in disturbed sediments. Part 2. Nitrogen diagenesisLimnology and Oceanography, 1977