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A visco-elastic model is suggested to recover the P−T−t paths of spherically symmetrical host-inclusion systems from residual pressure patterns. For a coesite–garnet, aragonite–garnet and diamond–garnet system with partial transition of high pressure polymorphs to low pressure ones, the model predicts that the exhumation history of ultra-high pressure metamorphic rocks from depths below 90 km began with pressure decrease to ∼1 GPa (∼40 km depth), while the temperature remained high (>800 C); then the system cooled and decompressed to ambient conditions. Non-spherical inclusion shapes in the 3-D model lead to heterogeneities in residual pressure and shear stress distributions as well as to significant gradients of shear stress, which may affect the kinetics and thermodynamics of phase transformation in the inclusions.

Results of experimental study of the effect of initial maldistribution of structured packing irrigation on efficiency of binary mixture separation are presented in this article. The studies were carried out in the experimental distillation column with the diameter of 0.9 m using the R114 and R21 freon mixture. Experiments were performed on the structured Mellapak 350.Y packing of stainless steel 316L, containing 19 layers with the total height of 4.016 m at the ratio of mole liquid and vapor flow rates L/V = 1 and 1.7, respectively, and the pressure in the upper part of the column ptop = 3 bars. Nonuniformity at the packing inlet was generated via the blocking of some holes in the liquid distributor. Here, we present some results on efficiency of mixture separation, pressure drop on the packing, distribution of local liquid flow rate under the packing over the cross-section and on the column wall within the range of vapor loading factor (0.69