Nano-confinement induced nucleation of ice-VII at room temperature

TL;DR

This study provides experimental evidence that extreme nano-confinement can induce the formation of ice-VII, a high-pressure ice phase, at room temperature, revealing new insights into water's behavior under confinement.

Contribution

The paper demonstrates direct measurement of ice-VII formation in confined water using tip-enhanced Raman spectroscopy, a novel approach for studying water's phase transitions at the nanoscale.

Findings

Ice-VII forms in water confined at sub-nanometer scales at room temperature.

A structural transition from ice-VII to tetrahedral ice occurs as confinement weakens.

Ice-VII's bcc DDAA network is mainly found inside the confined water, not at interfaces.

Abstract

The hydrogen bond (HB) network of water under confinement has been predicted to have distinct structures from that of bulk water. However, direct measurement of the structure has not been achieved. Here, we present experimental evidence of confinement-induced ice formation in water. We directly probe the HB network of a water nano-meniscus formed and confined between a mica substrate and a precisely-controlled-plasmonically active silver tip. By employing tip-enhanced Raman spectroscopy (TERS), we observe a novel double donor-double acceptor (DDAA) peak that emerges in the OH stretching band of water molecules at room temperature and at sub-nanometer confinement. This Raman peak indicates the presence of a solid phase of water, namely ice-VII with the body-centered cubic (bcc) unit. Interestingly, we observe a structural transition from bcc DDAA (ice-VII) to tetrahedral DDAA as the confinement is weakened. Moreover, by identifying the spatial distribution of the HB network, we find that the bcc DDAA network of ice-VII is predominantly present within the interior of the confined water, rather than at air/water or at solid/water interfaces. This suggest the possibility that the appearance of ice-VII in the strongly confined space could be a general characteristic of water under extreme confinement.