International audienceWe present a detailed investigation of the molecular structure of montmorillonite, an aluminosilicate clay with important applications in materials sciences, such as for catalysis, drug delivery, or as a waste barrier. Solid-state 29Si, 27Al, 25Mg, and 1H nuclear magnetic resonance (NMR) measurements combined with density functional theory (DFT) calculations provide a comprehensive picture of the local structure and composition of a synthetic clay and its naturally-occurring analogue. A revised composition is proposed based on NMR results that allow the identification and quantification of the signatures of otherwise undetectable non-crystalline impurities, thus largely complementing the traditional elemental analyses. Solid-state 1H NMR at fast magic-angle spinning (MAS) and high magnetic field provide quantitative information on intra- and inter-layer local environments that are crucial for the determination of the amount of Mg/Al substitution within the octahedral layer. In combination with DFT calculations of energies, it suggests that pairs of adjacent Mg atoms are unfavorable, leading to a non-random cationic distribution within the layers

International audienceCO adsorption in Al-rich faujasite zeolite containing copper and alkali cations has been investigated using DFT methods in order to determine how CO interacts and may modify the original position of the cations. Whether a cluster or a periodic model is used, addition of CO induces the formation of stable complexes labeled DI(CO) in which CO interacts by both its C-end and its O-end, resulting from a cooperative rearrangement of cations. In addition to a CuI migration from site II to the supercage, a migration of alkali from site III′ to site III may occur. DI(CO) also induces a downshift of the νCO mode in comparison with the complex containing CO interacting with a single cation, SI(CO). These results suggest a new assignment of the IR spectra of CO adsorbed in YCuI and YNa+: for YCuI, the upshifted signal at ca. 2160 cm-1 in comparison with νCOgas at 2143 cm-1 could be assigned to a SI(CO) structure, whereas the downshifted signal at ca. 2140 cm-1 could be assigned to a DI(CO) complex. For YNa+, the upshifted signal at ca. 2170 cm-1 could be assigned to SI(CO) NaSII · · ·CO and/or to DI(CO) NaSII · · ·OC· · · NaSIII′, whereas the downshifted signal at ca. 2122 cm-1 could be assigned to DI(CO) complex NaSII · · ·CO· · ·NaSIII′. This study shows that the DI(CO) interaction is a key ingredient for understanding the metal-exchanged zeolite properties