Organic
phosphates and phosphonates represent important yet understudied
constituents in our molecular understanding of the ocean. Herein,
we determined the critical concentration of sodium relating to the
onset of surface activity of alkyl phosphates and phosphonates at
the air–water interface to further understand the interfacial
environment of sea spray aerosols emitted from the ocean’s
surface. A low pH range (1–5.6) was chosen to represent a model
system for aged, acidic marine aerosols. The protonation state and
sodium binding properties of C16–C18 alkyl
phosphoric and phosphonic acids were explored using surface pressure–area
isotherms and infrared reflection–absorption spectroscopy.
We found that increasing pH and headgroup charge led to significant
desorption of these semi-soluble phosphorus-containing acids into
bulk solution, while the neutral, fully protonated, and sodium complexed
species were favored at the interface. For the phosphonate species,
the competition between sodium complexation and protonation reveals
a critical sodium chloride concentration of ≥2 M at pH 2 necessary
to outcompete the acid–base equilibrium. The onset of this
equilibrium shift begins at concentrations as low as 0.1 M NaCl at
pH 2, which demonstrates that ion pairing-mediated surface activity
is highly relevant in sea spray aerosol systems. We also show that
competitive interfacial equilibria between speciation and binding
cannot be modeled by known bulk processes for the fully soluble methylphosphonic
acid or through theoretical predictions from the Gouy–Chapman
model.