Abstract

Atmospheric aerosols contain a variety of compounds, among them free amino acids and salt ions. The pH of the aerosol droplets depends on their origin and environment. Consequently, compounds like free amino acids found in the droplets will be at different charge states, since these states to a great extent depend on the surrounding pH condition. In droplets of marine origin, amino acids are believed to drive salt ions to the water surface and a pH-dependent amino acid surface propensity will, therefore, indirectly affect many processes in atmospheric chemistry and physics such as for instance cloud condensation. To understand the surface propensity of glycine, valine, and phenylalanine at acidic, neutral, and basic pH, we used molecular dynamics (MD) simulations to investigate them at three different charge states in water. Their respective surface propensities were obtained by the means of a potential of mean force (PMF) in an umbrella sampling approach. Glycine was found to have no preference for the surface, while both valine and phenylalanine showed high propensities. Among the charge states of the surface-enriched ones, the cation, representing the amino acids at low pH, was found to have the highest affinity. Free energy decomposition revealed that the driving forces depend strongly on the nature of the amino acid and its charge state. In phenylalanine, the main factor was found to be a substantial entropy gain, likely related to the side chain, whereas in valine, hydrogen bonding to the functional groups leads to favorable energies and, in turn, affects the surface propensity. A significant gain in water–water enthalpy was seen for both valine and phenylalanine.

Highlights

  • Atmospheric aerosols of micrometer size, on which water condenses and forms cloud droplets, are called cloud condensation nuclei (CCN)

  • Activation of a particle to form cloud droplets is explained by the Köhler theory,[4] which describes the critical supersaturation for the nucleation and growth of droplets using two important parameters: water vapor pressure and surface tension

  • The potential of mean force (PMF) was obtained from umbrella sampling (US)[32] with starting configurations generated from a steered molecular dynamics (MD) (COM pulling) simulation

Read more

Summary

Introduction

Atmospheric aerosols of micrometer size, on which water condenses and forms cloud droplets, are called cloud condensation nuclei (CCN). Smaller-sized cloud droplets are formed, which increase the droplet density and thereby the reflectivity of the clouds.[5,6] The presence of surface-active organic molecules, for instance free amino acids, in the aerosol is one reason for a decrease in surface tension.[7−11] Free amino acids are essential components of aerosols[12,13] and play a significant role in atmospheric chemistry and physics They can react with atmospheric oxidants,[14,15] form brown carbon, which absorbs solar radiation,[16] and contribute to the global nitrogen cycle through atmospheric depositions.[17]

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call