Theoretical study of Cu(I)Y zeolite: structure and electronic properties.

The structural and electronic properties of the accessible Cu(I) site of a faujasite-type zeolite have been studied, by use of large cluster models and a density functional theory-based methodology. We demonstrate that the local ideal C(3) symmetry of the Cu(I) site II is broken. The Cu(I) cation is bonded to the zeolite framework by one bond of about 2.26 A and two shorter ones of 2.07 A. We demonstrate that only one cation position exists at this site. This result is also confirmed by a molecular electrostatic potential analysis. We show that local properties at site II, as well as the global properties of the solid (frontier orbitals), do not depend on the Al and cation distribution and only slightly on the cocation nature. Taking into account the present results and well-known experimental data, we propose that specific catalytic behaviors are correlated with local response properties, such as the local acid strength or, in other reactions, specific local architecture or confinement.

Probing Cu(I)-exchanged zeolite with CO: DFT modeling and experiment.

Addition of CO on Cu-exchanged zeolite was investigated by means of quantum chemical calculations based on density functional theory. The aim of this investigation was to get insights about changes of electronic properties of a copper site with zeolite composition by using a CO probe molecule. Calculated nu(CO) frequency values show that various Si/Al ratios of faujasite zeolite reproduce the expected experimental decrease of the nu(CO) values with decreasing Si/Al ratio. These calculations predict that H/Na ratio variations also induce changes in the nu(CO) values. These results illustrate that different compositions of the zeolite change the electronic properties of copper that are reflected in the nu(CO) frequency values. DFT results showed also that different structures and CO adsorption energies are obtained due to various Si/Al and H/Na ratios of the zeolite. Finally, these calculations evidence the possibility for CO to be connected at the same time to Cu(I) and to a close Na cation, Cu being at site II and Na at site II in Cu(I)-exchanged faujasite. A DRIFT experiment on two samples of faujasite, Cu(28)H(51)NaY and Cu(25)H(0)NaY, supports nu(CO) displacements to higher energy values with increasing H/Na ratio.