ABSTRACT
The thermodynamic stability of coagulation contacts is established at a defined thickness of hydrate coatings, which comply with the “α” and “β ” sections of adsorption isotherms (Fig. 2).
The first part of the curve “α” corresponds to thickness of coating of several hundreds of A
, and
1 GENERAL INSTRUCTIONS
Landslide processes always involve the presence of clayey minerals. Sliding surfaces or zones are usually formed at the contacts between clayey minerals, which are determined by the structural bonds among them.
