It is evidenced that due to the kinetic character of the glass transit
ion as a 'freeze in' process, PVT measurements extended over the glass
transition range depend not only on the thermal history but also on t
he pressure acting during the formation of the polymeric glasses. As a
consequence metastable glasses are formed which show during heating o
f the glassy polymer through the glass transition range 'volume relaxa
tion zones', characterized by a retarded increase or even decrease of
the volume. The width of the 'relaxation zone' increases with increasi
ng pressure and depends additional on the mode of operation used durin
g the PVT measurements. In the same time a pressure induced shift of t
he glass temperature to higher temperatures is observed, the shift bei
ng the greater the stiffer the polymer, i.e. the higher the glass temp
erature of the polymer at atmospheric pressure. Due to the metastable
character of polymeric glasses the evaluation of universal equations o
f states is thus not ingenious for polymeric glasses, because the dedu
ced EOS will be valid only for that given glass characterized by a wel
l defined thermal and pressure history. Additionally the EOS is influe
nced by the unknown time dependent aging and relaxation processes with
in polymeric glasses.