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(narrow line in Figure 1.4a,b; central units of 1 (Figure 1.5) is decreased. In the same
manner a decreasing proportion of the sum over all fourfold Al species is found and,
contrary to that, an increasing amount of fivefold coordinated aluminium species AlO 5
(signals at about 35 ppm) [23].
27 Al
19 F
-156 ppm
-147 ppm
a
a
-165 ppm
-163 ppm
-161 ppm
-171 ppm
b
b
c
c
d
d
-200
-300
-400
-100
-120
-140
-160
-180
-200
500
400
300
200
100
0
-100
(ppm)
(ppm)
Figure 1.7 27 Al NMR and 19 F NMR spectra of different sols and wet gels(B 0 ¼9.4 T). For all:
solid line: experimental spectrum, dashed: simulation, dotted: decomposition. From a to d
increasing content of fluorine. Molar ratios Al: F: (a) 4:1,(b) 2:1,(c) 1:1,(d) 1 : 2. (Reprinted
with permission from [23] Copyright (2007) American Chemical Society.)
All 19 F spectra are characterized by a group of three sharp signals (-161 ppm, -163 ppm,
-165 ppm) with different intensities. All these signals are in a typical region for fluorine
bounded on aluminium centres in a mixed oxygen-fluorine coordination with different
fluorine ratios [13, 24-28]. With higher fluorine content, the intensity of the 19 FNMR
spectrum is more and more dominated by a broad peak at about -160 ppm (Figure 1.7,
19 F,d). These line-broadening effects result mainly from 19 F- 19 F homonuclear dipolar
couplings ending up in one broad peak in the static 19 F NMR spectrum for the gel with
molar ratio Al:F as 1:3. 1 H and 13 C NMR spectra of sols and gels show two main effects
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