This contribution reports on a preliminary study of various phenomena,
that may occur during storage of natural gas in underground salt cave
rns. In these caverns the following substances are present: natural ga
s from different origins at pressures up to 300 bar, residual blanket
(diesel oil), water and sodium chloride. In the caverns temperatures a
s high as 353 K have to be expected. Retrograde condensation may occur
at pressure release, not only in the caverns, but also in the various
operating facilities. The first part of this study focuses on the var
ious aspects that govern the phase behavior inside the cavern. By mean
s of well-chosen model systems representative for natural gas and dies
el oil (octadecane), the main features of phase behavior have been stu
died. Also liquid dropout calculations were performed. Because natural
gas is stored in the caverns for only a limited period, it is plausib
le that inside the caverns concentration and temperature gradients wil
l be present, resulting in a variety of time-dependent processes. In t
he underlying study attention was also given to these aspects. Process
es like molecular diffusion and free convection applied for simplified
conditions have been studied, resulting in an insight how the dew poi
nt and liquid dropout may change in time.