Stabilization of AgI's polar surfaces by the aqueous environment, and its implications for ice formation
Thomas Sayer, Stephen J. Cox

TL;DR
This study uses advanced simulations to explore how aqueous environments stabilize polar AgI surfaces and their role in ice nucleation, highlighting the importance of dissolved ions in this process.
Contribution
It demonstrates that dissolved ions are essential for stabilizing polar AgI surfaces in water, impacting ice formation mechanisms and comparing simulation methods.
Findings
Pure water cannot stabilize AgI surfaces without ions
Dissolved ions are crucial for surface stabilization
Naive simulation methods can produce unphysical results
Abstract
Silver iodide is one of the most potent inorganic ice nucleating particles known, a feature generally attributed to the excellent lattice match between its basal Ag-(0001) and I-(000-1) surfaces, and ice. This crystal termination, however, is a type-III polar surface, and its surface energy therefore diverges with crystal size unless a polarity compensation mechanism prevails. In this simulation study, we investigate to what extent the surrounding aqueous environment is able to provide such polarity compensation. On its own, we find that pure water is unable to stabilize the AgI crystal in a physically reasonable manner, and that mobile charge carriers such as dissolved ions, are essential. In other words, proximate dissolved ions must be considered an integral part of the heterogeneous ice formation mechanism. The simulations we perform utilize recent advances in simulation methodology…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
