Origin of the anisotropic dielectric response of nanoconfined water

This text mentions work from 2024 on. Those parts were partly written without a live literature search and have not been checked by an editor yet.

In plain words

Water squeezed into a gap about a nanometer wide barely responds to an electric field across the gap, as if it were oil, yet it responds enormously to a field along the gap. A single microscopic explanation of both facts is missing.

Precise statement

For water in slits of height h between atomically flat graphite or hBN walls, the perpendicular dielectric constant falls to $\epsilon_{\mathrm{perp}} \sim 2$ for $h \sim 1\ \mathrm{nm}$ (2018 measurement), while a 2025 measurement found the in-plane constant $\epsilon_{\mathrm{par}}$ of about 1000 at few-layer thickness with superionic-level conductivity. Determine whether a model of interfacial layers with an anisotropic local dielectric tensor reproduces both $\epsilon_{\mathrm{perp}}(h)$ and $\epsilon_{\mathrm{par}}(h)$, or whether nonlocal correlated polarization and proton transport are required. An answer is a first-principles or simulation prediction of $\epsilon_{\mathrm{perp}}(h)$, $\epsilon_{\mathrm{par}}(h)$ and conductivity that matches both data sets.

What would settle it

Ab initio or validated force-field simulations of the measured geometries reproducing both dielectric components and the conductivity versus h, with the controlling molecular feature identified.

Status in the literature

Unverified note: it names recent work and was partly written without a live literature search; it awaits a check by an editor.

The 2025 Nature in-plane measurement attributed the enhancement to disordered hydrogen bonding and fast proton exchange; the low out-of-plane value is broadly reproduced by simulations of interfacial ordering.

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