M. Feuerstein et al., CHARACTERIZATION OF SODIUM-CATIONS IN DEHYDRATED ZEOLITE NAX BY NA-23NMR-SPECTROSCOPY, Solid state nuclear magnetic resonance, 7(2), 1996, pp. 95-103
Na-23 MAS, 2D nutation MAS, and DOR NMR spectroscopy has been applied
to characterise the location of sodium cations in dehydrated zeolite N
aX (Si/Al = 1.23). The Na-23 MAS NMR spectra recorded at three differe
nt magnetic field strengths were decomposed by computer simulation int
o five lines, which were attributed to five crystallographically disti
nct cation sites known from X-ray diffraction studies. The assignments
of the lines follow from electric field gradient calculations at the
Na-23 nuclei applying a simple point charge model based on crystal str
ucture data. A weak Gaussian line at low field (delta(iso) = -6 ppm) i
s assigned to sodium cations at site I, two broad quadrupole patterns
at the high-field side of the spectra are attributed to site I' (delta
(iso) = -19 ppm, QCC = 5.2 MHz, eta = 0) and site II cations (delta(is
o) = -15 ppm, QCC = 4.6 MHz, eta = 0), and two quadrupolar lines domin
ating the central region of the spectra originate from Na+ at two diff
erent III' sites (delta(iso) = -13 and -29 ppm, QCC = 2.6 and 1.6 MHz,
eta = 0.7 and 0.9, respectively). Na+ ions located on a second I' sit
e could be identified from the DOR NMR spectra. The line assignment is
further corroborated by the reasonable agreement of the site occupanc
ies estimated from the line intensities with those determined by X-ray
diffraction. In addition, sodium site populations of five dehydrated
zeolites NaX and NaY with Si/Al ratios between 1.09 and 4.0 were deriv
ed from the Na-23 MAS NMR spectra.