Bentonite samples from Petrovac and Aleksinac were treated with sulfuric acid of different molarities. Differences in structure and texture of the initial and modified bentonite were determined by chemical analysis and X-raypowder diffraction (XRPD), infra-red spectroscopy (FTIR), scanning electron microscopy (SEM) and physisorption nitrogen at –196°C. Sulfuric acid caused an exchange of Al³⁺, Fe³⁺ and Mg²⁺ with H⁺ ions which led to a modification of the smectite crystalline structure. The Mg and Fe substitution in the octahedral sheet promoted the dispersion of those layers and forming of amorphous silicon. The sequence according to which the cations left the octahedral sheets was as follows: Mg²⁺>Fe³⁺>Al³⁺. The sulfuric acid activated bentonites exhibiting a lower cation exchange capacity (CEC) and а change of specific surface area (S_BET) from 6 to 387 for bentonite from Petrovac and from 44 to 1784 m² g^-1 for bentonite from Aleksinac,  positioning them as an excellent absorber in wine technology and in the protection of soil and environment.