OS Ocean Science OS Ocean Sci. 1812-0792 Copernicus Publications Göttingen, Germany 10.5194/os-10-587-2014 An automated gas exchange tank for determining gas transfer velocities in natural seawater samples Schneider-Zapp K. 1 Salter M. E. 2 Upstill-Goddard R. C. 1 Ocean Research Group, School of Marine Science and Technology, Newcastle University, Newcastle upon Tyne, UK Department of Applied Environmental Science, Stockholm University, Stockholm, Sweden 03 07 2014 10 4 587 600 Copyright: © 2014 K. Schneider-Zapp et al. 2014 This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit https://creativecommons.org/licenses/by/3.0/ This article is available from https://os.copernicus.org/articles/10/587/2014/os-10-587-2014.html The full text article is available as a PDF file from https://os.copernicus.org/articles/10/587/2014/os-10-587-2014.pdf

In order to advance understanding of the role of seawater surfactants in the air–sea exchange of climatically active trace gases via suppression of the gas transfer velocity (<i>k</i><sub>w</sub>), we constructed a fully automated, closed air–water gas exchange tank and coupled analytical system. The system allows water-side turbulence in the tank to be precisely controlled with an electronically operated baffle. Two coupled gas chromatographs and an integral equilibrator, connected to the tank in a continuous gas-tight system, allow temporal changes in the partial pressures of SF<sub>6</sub>, CH<sub>4</sub> and N<sub>2</sub>O to be measured simultaneously in the tank water and headspace at multiple turbulence settings, during a typical experimental run of 3.25 h. PC software developed by the authors controls all operations and data acquisition, enabling the optimisation of experimental conditions with high reproducibility. The use of three gases allows three independent estimates of <i>k</i><sub>w</sub> for each turbulence setting; these values are subsequently normalised to a constant Schmidt number for direct comparison. The normalised <i>k</i><sub>w</sub> estimates show close agreement. Repeated experiments with Milli-Q water demonstrate a typical measurement accuracy of 4% for <i>k</i><sub>w</sub>. Experiments with natural seawater show that the system clearly resolves the effects on <i>k</i><sub>w</sub> of spatial and temporal trends in natural surfactant activity. The system is an effective tool with which to probe the relationships between <i>k</i><sub>w</sub>, surfactant activity and biogeochemical indices of primary productivity, and should assist in providing valuable new insights into the air–sea gas exchange process.

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