Amino
acids (AAs), the building blocks of proteins, are enriched
by several orders of magnitude in sea spray aerosols compared to ocean
waters. This suggests that AAs may reside at the air–water
interface and be highly surface active. Using surface tension measurements,
infrared reflection–absorption spectroscopy, and molecular
dynamics simulations, we show that AAs are surface active and that
salts and low-pH environments are drivers of surface activity. At
typical sea spray salt concentrations and pH values, we determine
that the surface coverage of hydrophobic AAs increases by approximately
1 order of magnitude. Additionally, divalent cations such as Ca2+ and Mg2+ can further increase AA surface propensity,
particularly at neutral pH. Overall, these results indicate that AAs
are likely to be found at increased concentrations at the surface
of sea spray aerosols, where they can impact the cloud activation
properties of the aerosol and enhance peptide formation under certain
conditions.