The structure of water around methane during hydrate crystallization from a
queous solutions of methane is studied using neutron diffraction with isoto
pic substitution over the temperature range 18 degrees C to 4 degrees C, an
d at two pressures, 14.5 and 3.4 MPa. The carbon-oxygen pair correlation fu
nctions, derived from empirical potential structure refinement of the data,
indicate that the hydration sphere around methane in the liquid changes dr
amatically only once hydrate has formed, with the water shell around methan
e being about 1 Angstrom larger in diameter in the crystal than in the liqu
id. The methane coordination number in the liquid is around 16 +/- 1 water
molecules during hydrate formation, which is significantly smaller than the
value of 21 +/- 1 water molecules found for the case when hydrate is fully
formed. Once hydrate starts to form, the hydration shell around methane be
comes marginally less ordered compared to that in the solution above the hy
drate formation temperature. This suggests that the hydration cage around m
ethane in the liquid may be different from that when hydrate is forming and
from that found in the hydrate crystal structure. Methane-methane radial d
istribution functions show that methane molecules can adopt a range of sepa
rations during hydrate formation, corresponding to the more distorted natur
e of the methane-water correlations. There is noticeable ordering of the me
thane molecules with a monolayer of water molecules between them once hydra
te has formed. The dipole moments of the hydrating water molecules lie most
ly tangential to the methane-water axis, both before, during, and after hyd
rate formation. (C) 2000 American Institute of Physics. [S0021-9606(00)7013
5-8].