27Al spin-echo, high-speed MAS (νrot
= 30 kHz), and MQMAS NMR spectroscopy in magnetic fields of B0
= 9.4, 14.1, and 17.6 T were applied for the study of aluminum species at framework and extra-framework positions in non-hydrated zeolites Y. Non-hydrated γ-Al2O3 and non-hydrated aluminum-exchanged zeolite Y (Al,Na-Y) and zeolite H,Na-Y were utilized as reference materials. The solid-state 27Al NMR spectra of steamed zeolite deH,Na-Y/81.5 were found to consist of four signals. The broad low-field signal is caused by a superposition of the signals of framework aluminum atoms in the vicinity of bridging hydroxyl protons and framework aluminum atoms compensated in their negative charge by aluminum cations (δiso
= 70 ± 10 ppm, CQCC
= 15.0 ± 1.0 MHz). The second signal is due to a superposition of the signals of framework aluminum atoms compensated by sodium cations and tetrahedrally coordinated aluminum atoms in neutral extra-framework aluminum oxide clusters (δiso
= 65 ± 5 ppm, CQCC
= 8.0 ± 0.5 MHz). The residual two signals were attributed to aluminum cations (δiso
= 35 ± 5 ppm, CQCC
= 7.5 ± 0.5 MHz) and octahedrally coordinated aluminum atoms in neutral extra-framework aluminum oxide clusters (δiso
= 10 ± 5 ppm, CQCC
= 5.0 ± 0.5 MHz). By chemical analysis and evaluating the relative solid-state 27Al NMR intensities of the different signals of aluminum species occurring in zeolite deH,Na-Y/81.5 in the non-hydrated state, the aluminum distribution in this material was determined.
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