We present the results of a high-resolution neutron diffraction experiment
with a fully deuterated methane hydrate type I at temperatures of 2, 100, a
nd 150 K. Precise crystallographic parameters of the ice-like D2O lattice a
nd the thermal parameters of the encaged methane molecules have been obtain
ed. The parameters of the host lattice differ only slightly from values fou
nd for hydrates with asymmetric guests included, which leads to the conclus
ion that the host lattice of structure I is only a little adaptive. At low
temperatures (2 K) the methane molecules in both types of cages present in
structure I occupy positions in the center of the cages. At higher temperat
ures the thermal parameters in both types of cages reflect the surrounding
cage geometries or more precisely the translational potentials of the cages
. The orientational scattering length density of the CD4 molecules has been
analyzed in terms of a multipole expansion with symmetry adapted functions
[Press and Huller, Acta Crystallogr., Sect. A: Cryst. Phys., Diffr., Theor
. Gen. Crystallogr. A29, 252 (1972); Press, ibid. A29, 257 (1972)]. In both
types of cages we found only small modulations of a spherically symmetric
scattering density accounting for almost free rotations of the methane mole
cules. The large and asymmetric cage leads to a somewhat more pronounced mo
dulation of the orientational density than in the small dodecahedral cage.
The orientational probability distribution function (PDF) remains nearly un
changed from 2 to 150 K. At 200 K we observed the time-resolved decompositi
on of the hydrate structure I into hexagonal ice Ih. (C) 2000 American Inst
itute of Physics. [S0021- 9606(00)00735-2].