Raman spectroscopic measurements on synthetic air clathrates, prepared
at different pressures and temperatures, are presented. The gas fract
ionation for clathrates formed at -2 and -20 degrees C is determined f
rom the integrated vibron mode intensities of nitrogen and oxygen mole
cules. An increasing fractionation in favour of oxygen with increasing
pressure is found. An asymmetric peak shape for the O-2 vibron mode w
as observed in air clathrates prepared at 300 bar and -2 degrees C. Th
e asymmetry of the N-2 vibron mode in the same sample is much less pro
nounced.