“…Theoretical models of transport and chemistry in water-filled nanopores routinely rely on the simplifying approximation that water properties are not modified by confinement 19 , but this approximation is expected to fail in nanoporous media where pore size approaches the diameter of a water molecule 20 . Studies of water in hydrophilic nanopores carried out with a range of techniques (thermoporometry 1,24 , capillary imbibition 25 , surface force apparatus 22,26 , infrared and Raman spectroscopy 4,17,18,21,27 , NMR spectroscopy 28 , X-ray and neutron diffraction 6,[29][30][31] , quasi-elastic neutron 4 scattering 2,32 , molecular dynamics simulations 26,[33][34][35][36] ) show that this failure occurs in pores narrower than ~20 nm and can be classified into two regimes. The first regime occurs in pores that are about 2 to 20 nm wide and results from "surface water" [water with structure and dynamics distinct from those of bulk liquid water, found within up to three statistical monolayers (~0.9 nm) from hydrophilic surfaces 34,35 ] constituting a nonnegligible part of the pore water 25,27,34 .…”