STUDY OF FAUJASITE-TYPE ZEOLITE MODIFIED WITH LA AND NH41+
Pablo Sebastian Vizcaino Moreira, Hugo Javier Sánchez Moreno, Mishell Moreno Samaniego, Evelyn Carolina Macias Silva, Fabian Israel Heredia Moreno
The acidity of faujasite zeolite was modified through ion exchange, it is treated in the present study, the Na1+ cation, part of the initial structure of faujasite, was removed by cations such as NH41+ and La3+. The obtained molar ratio of the precursor oxides for the formulation of the seed gel was: SiO2/Al2O3 = 12.26; Na2O/Al2O3 = 13.27 and Na2O/SiO2 = 2.16. In the case of the structural gel, the following molar ratios were reported: SiO2/Al2O3 = 10.90; Na2O/Al2O3 = 11.92 and Na2O/SiO2 = 2.18. The optimum crystallization temperature was 90 °C for the seed gel and 80 °C for the structural gel. The zeolite obtained was characterized by X-ray diffraction (XRD), through comparative analysis between the diffractograms of the zeolite developed and NaY-type faujasite patterns. By means of BET surface area analysis, a specific surface area of 875 m2.g-1 and a pore radius of 5.88 Å were determined, and the morphological analysis was complemented by scanning electron microscopy (SEM). The ion exchange behavior for the case of ammonium ion, reported an exchange of 59.8 mg.g-1 under the best experimental conditions (8 h, 20 cm3.g-1), while in the case of lanthanum ion it was 38 mg.g-1 (24 h, 50 cm3.g-1).