During the 2007 UK SOLAS Deep Ocean Gas Exchange Experiment in the northeast Atlantic Ocean, we conducted the first ever study of the effect of a deliberately released surfactant (oleyl alcohol) on gas transfer velocities ( k w ) in the open ocean. Exchange rates were estimated with the 3 He/SF 6 dual tracer technique and from measured sea‐to‐air DMS fluxes and surface water concentrations. A total of seven k w estimates derived from 3 He/SF 6 were made, two of which were deemed to be influenced by the surfactant. These exhibited suppression from ∼5% to 55% at intermediate wind speeds ( U 10 ) in the range 7.2–10.7 m s −1 . Similarly, k w determined from DMS data ( k DMS ) was also depressed by the surfactant; suppression ranged from ∼39% at 5.0 m s −1 to ∼24% at 10.8 m s −1 . Surfactant thus has the potential to measurably suppress gas exchange rates even at moderate to high wind speeds.
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Salter et al. (2011) studied this question.
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