To
gain global understanding of the complex interactions marine
organics participate in at the surface of sea spray aerosols (SSAs),
thermodynamic parameters are needed as inputs for atmospheric models.
Traditional surface studies use Langmuir films that exist in pseudoequilibrium
and require assumptions to obtain thermodynamic properties. To address
these challenges, we have developed a new application for equilibrium
spreading pressure (ESP), an experimental value based on the true
thermodynamic equilibrium between a film and its solid form at the
aqueous interface. By changing the equilibrium phase state of a marine
relevant palmitic acid/palmitate (PA) monolayer as a function of temperature
(7.0–20.2 °C) and sodium chloride concentration (1–1000
mM), we can experimentally capture the thermodynamic values of three-dimensional
(3D) solid to two-dimensional (2D) monolayer spreading. Cooler temperatures
present more unfavorable and disordered conditions for spreading PA
into a 2D film. However, the addition of NaCl to the solution does
not follow a monotonical trend in thermodynamic values, exhibited
by an anomalous 100 mM NaCl condition, which is ∼20 and ∼35%
more enthalpically favorable than 10 and 1000 mM NaCl, respectively.
Our results represent some of the first thermodynamic data for spreading
PA from 3D solid to 2D film given atmospheric conditions and the first
study to utilize ESP to determine the thermodynamic properties of
PA–Na+ interactions. Our true equilibrium-based
approach helps to inform on the 3D to 2D phase-state transition of
organic coatings, presenting an essential input for climate models
and global understanding of SSA interfaces.