EGU2020-1555
https://doi.org/10.5194/egusphere-egu2020-1555
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

In-situ investigation of alkalinity - denitrification coupling in the sediment - water column interface

Mona Norbisrath
Mona Norbisrath
  • Helmholtz-Zentrum Geesthacht, Institute for Coastal Research, Germany (mona.norbisrath@hzg.de)

Abstract: EGU 2020

Session: BG4.1: Biogeochemistry of coastal seas and continental shelves (Helmuth Thomas)

Mona Norbisrath1, Kirstin Dähnke1, Andreas Neumann1, Justus van Beusekom1, Nele Treblin1, Bryce van Dam1, Helmuth Thomas1

1Institute for Coastal Research, Helmholtz-Zentrum Geesthacht

Contact: mona.norbisrath@hzg.de

 

In-situ investigation of alkalinity - denitrification coupling in the sediment - water column interface

 

As a shallow shelf sea, the North Sea is very vulnerable to anthropogenic impacts like rising CO2 concentrations, increasing nutrient inflows and coincident oxygen loss.

Two important processes that determine the role of the coastal ocean as a net sink for anthropogenic CO2 are alkalinity and denitrification. Alkalinity, the acid binding capacity of the ocean, buffers natural and anthropogenic changes in the oceans’ CO2 and pH system. Denitrification, an anaerobic microbial process in which organic matter is respired, uses NO3- instead of O2 as a terminal electron acceptor. Denitrification reduces NO3- to N2 and in turn produces alkalinity.

Eutrophication, caused by leaching of excess fertilizer nutrients into coastal seas, leads to enhanced denitrification and therefore to enhanced alkalinity as well as an increased uptake of CO2. However, the quantitative relationship between denitrification and alkalinity production and its control under changing environmental conditions is yet to be determined.

In the German Bight, denitrification is usually restricted to anoxic sediments. In this study, we therefore focus on in-situ experiments in the sediment - water column interface. Batch core incubations in combination with the isotope pairing technique (IPT) and labelled nitrate additions were used to detect denitrification and gauge its effect on alkalinity production during a cruise on RV Heincke (HE541) in September 2019 in the German Bight. To quantify denitrification, the production of all three N2 isotope species (28N2, 29N2 and 30N2) is measured using a membrane inlet mass spectrometer (MIMS). We expect an increase of denitrification rates with nitrate concentrations and incubation times, and we will quantify benthic denitrification. We will further evaluate the assumption of concurrent increases in alkalinity production and will investigate the benthic-pelagic coupling of these processes. Investigating the in-situ interaction of metabolic alkalinity and denitrification will give an estimation of the alkalinity impact on the reduction of anthropogenic CO2 in the atmosphere.

 

How to cite: Norbisrath, M.: In-situ investigation of alkalinity - denitrification coupling in the sediment - water column interface, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1555, https://doi.org/10.5194/egusphere-egu2020-1555, 2019

This abstract will not be presented.