The
extra-large pore zeolite SSZ-59 was prepared with highly ordered
Al atoms in T6 positions within the double-zigzag chains (dzc) running
along the 14 MR channels. Narrow 1H MAS NMR signals of
bridging OH groups, which are responsible for Brønsted acidity,
emerge from this Al site ordering. The theoretically predicted residual 1H–27Al dipolar effect that is caused by
the large 27Al quadrupolar coupling associated with the
trigonally distorted Al coordination near this OH group was observed
here with an unprecedented spectral resolution. Three 1H NMR signals are separately observed at B
0 = 7.0 T for proximal 27Al spins with magnetic quantum
numbers of m = ±1/2, m = ±3/2,
or m = ±5/2. A short 1H–27Al distance of 2.52 ± 0.02 Å was measured by means
of 1H{27Al} rotational echo adiabatic passage
double-resonance (REAPDOR) characteristic for a Brønsted acid
site. This distance predominates the initial slope of the 1H{27Al} REAPDOR evolution curve, whereas additional much
weaker 1H–27Al dipolar interactions were
found by a second, less steep slope at longer evolution times. The
second slope can be modeled either by a second Al atom within the
dzc chain located at a distance of 6.7 Å to the bridging OH group
or, alternatively, by two Al atoms in the dzc, with H–Al distances
of 8.09 and 8.72 Å. The latter model with two Al is in excellent
agreement with the packing of the organic structure-directing agent
in the 14 MR pores of the as-made material, which places the heteroatomsin
this case boron atoms that are postsynthetically replaced by aluminum
after calcination/removal of the organicsinto a highly ordered
pattern in the dzc. The data indicate that the packing of the organics
in adjacent 14 MR channels is not independent and shifted by 1.5 unit
cells along the a-direction.