ANALYSIS OF THE SELF-ORGANIZING HYDRODYNAMIC STRUCTURES AND THE TOPOLOGY OF THE ROCK SALT DISSOLUTION RELIEF

摘要

The knowledge of the surface relief, which develops through mass transfer during the dissolution of rock salt, allows for drawing conclusions on the steering physical mechanisms.Until recent time not much attention has been paid to the study of self-organization phenomena within fluid systems. Principles of interrelation of structurization of a solution and self-organization of the whole system remain vague.