Water,
because of its anomalous properties, can exhibit complex
behavior under strong confinement. At room temperature and pressure,
water is assumed to exist in a single phase as a liquid under confinement
(e.g., in a carbon nanotube). In this study, using extensive molecular
dynamics simulations, we show the existence of multiple phases of
water when water meets a nanotube surface under atmospheric conditions
(T = 300 K, P = 1 atm). Vapor, high-density
ice, and liquid water phases coexist in the region within ∼1
nm from the surface. Structure factor, entropy, pressure, viscosity,
and rotational diffusion of water layers near the surface reveal substantial
phase anomalies induced by confinement. We show the presence of a
new high-density solid-state ice layer (ρ = 3.9 g/cm3) with rhombic structure coexisting adjacent to vapor and liquid
water. The existence of multiple phases of water near an interface
can explain, for example, the slip phenomena, self-filling behavior
of a carbon nanotube, and fast transport of water.