Pathways to dewetting in hydrophobic confinement
Richard C. Remsing, Erte Xi, Srivathsan Vembanur, Sumit, Sharma, Pablo G. Debenedetti, Shekhar Garde, Amish J. Patel

TL;DR
This study reveals that water dewetting in hydrophobic confinement often proceeds via non-classical pathways facilitated by water density fluctuations, reducing the energy barrier compared to classical nucleation theory.
Contribution
The paper demonstrates that dewetting transitions in nanoconfined water follow non-classical pathways driven by density fluctuations, challenging traditional macroscopic nucleation models.
Findings
Dewetting barriers are smaller than classical predictions.
Transition occurs via an abrupt cavity-to-vapor tube change.
Enhanced fluctuations stabilize non-classical dewetting pathways.
Abstract
Liquid water can become metastable with respect to its vapor in hydrophobic confinement. The resulting dewetting transitions are often impeded by large kinetic barriers. According to macroscopic theory, such barriers arise from the free energy required to nucleate a critical vapor tube that spans the region between two hydrophobic surfaces - tubes with smaller radii collapse, whereas larger ones grow to dry the entire confined region. Using extensive molecular simulations of water between two nanoscopic hydrophobic surfaces, in conjunction with advanced sampling techniques, here we show that for inter-surface separations that thermodynamically favor dewetting, the barrier to dewetting does not correspond to the formation of a (classical) critical vapor tube. Instead, it corresponds to an abrupt transition from an isolated cavity adjacent to one of the confining surfaces to a…
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