Hydration numbers of methane hydrates with various water/gas ratios of the
sample were measured by Raman spectroscopy. Artificial methane hydrates wer
e formed at temperatures ranging from 273.2 to 278.4 K, and pressures from
3.0 to 7.0 MPa, with a stirring rate of approximately 500 rpm. Under such n
onequilibrium conditions, the obtained hydrate sample shad a water/gas rati
o ranging from 6.4 to 17.4, which was determined by mass measurements. The
spectroscopic analysis revealed, however, that the crystallographic hydrati
on number was almost constant at 6.2 +/- 0.2, which corresponds to the hydr
ation number estimated from the thermodynamic model. The same measurements
were carried out on natural gas hydrate samples obtained from the deep-sea
floor of Blake Ridge. The coincidence of the hydration numbers between natu
ral and artificial samples indicated that the crystallographic hydration nu
mber is independent of the formation conditions and the large variation in
the water/gas ratio of samples is described by the ratio between pure hydra
te and free water.