Using
molecular dynamics simulation, we investigate the phase behavior
of water confined in graphene nanocapillaries at room temperature
(300 K). Here, the lateral pressure Pzz is used as the primary controlling variable, and
its effect on the behavior of trilayer water is systematically studied.
Three (meta)stable trilayer (TL) crystalline/amorphous ice phases,
namely, TL-ABAI, TL-ABA, and TL-AAAI, are observed in our simulations
with the lateral pressure in the range of 1.0 GPa ≤ Pzz ≤ 6.0 GPa. TL-ABAI
exhibits a square lattice in every layer, and the three layers exhibit
the ABA stacking pattern; i.e., the oxygen atoms in the two outer
layers are in registry. This new trilayer ice structure can also be
viewed as a bilayer clathrate hydrate with water molecules in the
middle layer serving as the guest molecules. With increasing lateral
pressure, typically, the solid-to-liquid-to-solid phase transition
occurs, during which the structural transformation from triangular
to square-like in the ice layer is accompanied by a sudden jump in P⊥ (normal pressure) and in potential
energy (per molecule). The oxygen density profiles of the three trilayer
structures show a common feature; that is, the peak of the middle
layer is markedly lower than that of the two outer layers. The computed
diffusivity suggests that water in the middle layer exhibits behavior
different from that in the two outer layers in contact with the graphene.
For TL-AAAI, the diffusion of water molecules in the layer next to
the graphene is faster than that in the middle layer.