Air-Sea CO2-Exchange in a Large Annular Wind-Wave Tank and the Effects of Surfactants

Wind, chemical enhancement, phytoplankton activity, and surfactants are potential factors driving the air-sea gas exchange of carbon dioxide (CO2). We investigated their effects on the gas transfer velocity of CO2 in a large annular wind-wave tank filled with natural seawater from the North Atlantic...

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Main Authors: Mariana Ribas-Ribas, Frank Helleis, Janina Rahlff, Oliver Wurl
Format: Article
Language:English
Published: Frontiers Media S.A. 2018-11-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/fmars.2018.00457/full
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spelling doaj-47f9eef9f44b40a8bbd6256cb61af6d92020-11-25T01:01:37ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452018-11-01510.3389/fmars.2018.00457405801Air-Sea CO2-Exchange in a Large Annular Wind-Wave Tank and the Effects of SurfactantsMariana Ribas-Ribas0Frank Helleis1Janina Rahlff2Oliver Wurl3Institute for Chemistry and Biology of the Marine Environment (ICBM), Carl-von-Ossietzky-University Oldenburg, Wilhelmshaven, GermanyMax-Planck-Institut für Chemie (Hahn Otto -Institut), Mainz, GermanyInstitute for Chemistry and Biology of the Marine Environment (ICBM), Carl-von-Ossietzky-University Oldenburg, Wilhelmshaven, GermanyInstitute for Chemistry and Biology of the Marine Environment (ICBM), Carl-von-Ossietzky-University Oldenburg, Wilhelmshaven, GermanyWind, chemical enhancement, phytoplankton activity, and surfactants are potential factors driving the air-sea gas exchange of carbon dioxide (CO2). We investigated their effects on the gas transfer velocity of CO2 in a large annular wind-wave tank filled with natural seawater from the North Atlantic Ocean. Experiments were run under 11 different wind speed conditions (ranging from 1.5 ms−1 to 22.8 ms−1), and we increased the water pCO2 concentration twice by more than 950 μatm for two of the seven experimental days. We develop a conceptual box model that incorporated the thermodynamics of the marine CO2 system. Surfactant concentrations in the sea surface microlayer (SML) ranged from 301 to 1015 μgL−1 (as Triton X-100 equivalents) with enrichments ranged from 1.0 to 5.7 in comparison to the samples from the underlying bulk water. With wind speeds up to 8.5 ms−1, surfactants in the SML can reduce the gas transfer velocity by 54%. Wind-wave tank experiments in combination with modeling are useful tools for obtaining a better understanding of the gas transfer velocities of CO2 across the air-sea boundary. The tank allowed for measuring the gas exchange velocity under extreme low and high wind speeds; in contrast, most previous parametrizations have fallen short because measurements of gas exchange velocities in the field are challenging, especially at low wind conditions. High variability in the CO2 transfer velocities suggests that gas exchange is a complex process not solely controlled by wind forces, especially in low wind conditions.https://www.frontiersin.org/article/10.3389/fmars.2018.00457/fullsea-surface microlayergas exchangegas transfer velocitylow wind speedsurfactantschemical enhancement
collection DOAJ
language English
format Article
sources DOAJ
author Mariana Ribas-Ribas
Frank Helleis
Janina Rahlff
Oliver Wurl
spellingShingle Mariana Ribas-Ribas
Frank Helleis
Janina Rahlff
Oliver Wurl
Air-Sea CO2-Exchange in a Large Annular Wind-Wave Tank and the Effects of Surfactants
Frontiers in Marine Science
sea-surface microlayer
gas exchange
gas transfer velocity
low wind speed
surfactants
chemical enhancement
author_facet Mariana Ribas-Ribas
Frank Helleis
Janina Rahlff
Oliver Wurl
author_sort Mariana Ribas-Ribas
title Air-Sea CO2-Exchange in a Large Annular Wind-Wave Tank and the Effects of Surfactants
title_short Air-Sea CO2-Exchange in a Large Annular Wind-Wave Tank and the Effects of Surfactants
title_full Air-Sea CO2-Exchange in a Large Annular Wind-Wave Tank and the Effects of Surfactants
title_fullStr Air-Sea CO2-Exchange in a Large Annular Wind-Wave Tank and the Effects of Surfactants
title_full_unstemmed Air-Sea CO2-Exchange in a Large Annular Wind-Wave Tank and the Effects of Surfactants
title_sort air-sea co2-exchange in a large annular wind-wave tank and the effects of surfactants
publisher Frontiers Media S.A.
series Frontiers in Marine Science
issn 2296-7745
publishDate 2018-11-01
description Wind, chemical enhancement, phytoplankton activity, and surfactants are potential factors driving the air-sea gas exchange of carbon dioxide (CO2). We investigated their effects on the gas transfer velocity of CO2 in a large annular wind-wave tank filled with natural seawater from the North Atlantic Ocean. Experiments were run under 11 different wind speed conditions (ranging from 1.5 ms−1 to 22.8 ms−1), and we increased the water pCO2 concentration twice by more than 950 μatm for two of the seven experimental days. We develop a conceptual box model that incorporated the thermodynamics of the marine CO2 system. Surfactant concentrations in the sea surface microlayer (SML) ranged from 301 to 1015 μgL−1 (as Triton X-100 equivalents) with enrichments ranged from 1.0 to 5.7 in comparison to the samples from the underlying bulk water. With wind speeds up to 8.5 ms−1, surfactants in the SML can reduce the gas transfer velocity by 54%. Wind-wave tank experiments in combination with modeling are useful tools for obtaining a better understanding of the gas transfer velocities of CO2 across the air-sea boundary. The tank allowed for measuring the gas exchange velocity under extreme low and high wind speeds; in contrast, most previous parametrizations have fallen short because measurements of gas exchange velocities in the field are challenging, especially at low wind conditions. High variability in the CO2 transfer velocities suggests that gas exchange is a complex process not solely controlled by wind forces, especially in low wind conditions.
topic sea-surface microlayer
gas exchange
gas transfer velocity
low wind speed
surfactants
chemical enhancement
url https://www.frontiersin.org/article/10.3389/fmars.2018.00457/full
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