Ion exchange in atomically thin clays and micas
Yi-Chao Zou, Lucas Mogg, Nick Clark, Cihan Bacaksiz, Slavisa, Milanovic, Vishnu Sreepal, Guang-Ping Hao, Yi-Chi Wang, David G. Hopkinson,, Roman Gorbachev, Samuel Shaw, Kostya S. Novoselov, Rahul Raveendran-Nair,, Francois M. Peeters, Marcelo Lozada-Hidalgo, Sarah J. Haigh

TL;DR
This study reveals that ion exchange in atomically thin clays and micas occurs at significantly faster rates than in bulk, due to enhanced interlayer expandability, with implications for designing advanced membrane materials.
Contribution
It provides the first atomic-scale visualization of ion exchange dynamics and ion binding sites in atomically thin clays and micas, highlighting the role of layer twist and restacking.
Findings
Ion diffusion constant in atomically thin samples is up to 10^4 times larger than in bulk crystals.
Twisted and restacked mica layers exhibit fast ion exchange with ion islands influenced by moiré patterns.
Atomic-resolution images of surface cations reveal previously elusive details of ion binding.
Abstract
Clays and micas are receiving attention as materials that, in their atomically thin form, could allow for novel proton conductive, ion selective, osmotic power generation, or solvent filtration membranes. The interest arises from the possibility of controlling their properties by exchanging ions in the crystal lattice. However, the ion exchange process itself remains largely unexplored in atomically thin materials. Here we use atomic-resolution scanning transmission electron microscopy to study the dynamics of the process and reveal the binding sites of individual ions in atomically thin and artificially restacked clays and micas. Imaging ion exchange after different exposure time and for different crystal thicknesses, we find that the ion diffusion constant, D, for the interlayer space of atomically thin samples is up to 10^4 times larger than in bulk crystals and approaches its value…
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