Water is a demanding partner. It strongly attracts ions, yet some halide anions-chloride, bromide, and iodide-are expelled to the air/water interface. This has important implications for chemistry in the atmosphere, including the ozone cycle. We present a quantitative analysis of the energetics of ion solvation based on molecular simulations of all stable alkali and halide ions in water droplets. The potentials of mean force for Cl − , Br − , and I − have shallow minima near the surface. We demonstrate that these minima derive from more favorable water-water interaction energy when the ions are partially desolvated. Alkali cations are on the inside because of the favorable ion-water energy, whereas F − is driven inside by entropy. Models attempting to explain the surface preference based on one or more ion properties such as polarizability or size are shown to lead to qualitative and quantitative errors, prompting a paradigm shift in chemistry away from such simplifications.ozone layer | GROMACS | aerosol | thermodynamics S ea water becomes airborne in the form of droplets formed at the sea surface by the action of waves (1). These droplets can be carried by the wind, and they interact with other constituents of the atmosphere (Fig. 1A). On the surface of the small water droplets, halide anions can be converted into halogen atoms by absorption of light (2, 3), and the air-water interface serves to increase certain reaction probabilities (4, 5). One example is the oxidation of Cl − and Br − by OH radicals or O 3 that can occur at the air-water interface, with mechanisms different from those in the bulk phase (6), leading to natural ozone depletion in the stratosphere.Both theoretical and experimental studies have shown that Cl − , Br − and I − prefer to be at the surface of water droplets (Fig. 1A), whereas F − and alkali cations strive to become fully solvated in the bulk of water droplets (7-12). The Br − concentration is enhanced more at the surface than the Cl − concentration (13), an effect that may be enhanced in mixtures containing both Br − and Cl − , such as seawater (14). Because Br − is more reactive than Cl − , the surface preference has an impact on the chemistry in the atmosphere, despite the fact that the content of Cl − in bulk sea water is about three orders of magnitude higher than that of Br − (15). The energetic and structural mechanisms underlying the surface preference of large halide anions have been studied in quite some detail (16-18), but the phenomenon is still not understood quantitatively (10). Only very recently has the surface absorption free energy of one halide anion, Br − , been determined experimentally (19). Recent progress in development of force fields for water (20) and ions (21) finally allows establishment of the surface preferences for all halide and alkali ions quantitatively.Here we present the energetics of ion solvation in a water droplet with a radius of approximately 1.1 nm for all stable halide anions (F − , Cl − , Br − , I − ) and alkali cations (Li þ , Na þ , K þ...