The three sire-sire partial structure factors for water have been measured
as a function of pressure, using neutron diffraction, at a temperature of 2
68 K. It is found that the measured structure functions imply a continuous
transformation with increasing pressure from a low-density form of water (r
ho(L) similar to 0.0295 molecules/Angstrom(3)), with an open, hydrogen-bond
ed tetrahedral structure, to a high-density form of water (rho(H) similar t
o 0.0402 molecules/Angstrom(3)), with nontetrahedral O-O-O angles and a col
lapsed second coordination shell, which implies broken hydrogen bonds betwe
en the first and second coordination shells.