Articles | Volume 13, issue 3
Research article
12 Feb 2016
Research article |  | 12 Feb 2016

The impact of sedimentary alkalinity release on the water column CO2 system in the North Sea

H. Brenner, U. Braeckman, M. Le Guitton, and F. J. R. Meysman


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (08 Nov 2015) by Gerhard Herndl
AR by Heiko Brenner on behalf of the Authors (11 Nov 2015)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (15 Nov 2015) by Gerhard Herndl
RR by Johannes Paetsch (27 Nov 2015)
ED: Publish subject to minor revisions (Editor review) (28 Nov 2015) by Gerhard Herndl
AR by Heiko Brenner on behalf of the Authors (15 Jan 2016)  Author's response    Manuscript
ED: Publish as is (15 Jan 2016) by Gerhard Herndl
Short summary
Alkalinity released from sediments of the southern North Sea can play an important role in the carbon cycle of the North Sea by lowering the pCO2 of the seawater and thus increasing the CO2 flux between the atmosphere and the water. However, not every single mole alkalinity generated in sediments leads to an additional CO2 uptake, as certain reactions in the water column can negate the respective alkalinity release.
Final-revised paper