Scott Oliver, Alex Kuperman, Alan Lough and Geoffrey A. Ozin
The structure of an anionic aluminophosphate molecular sieve UT-6 has
been determined by single-crystal X-ray diffraction and19F MAS
NMR, 31P CP MAS NMR and 27Al MQ MAS spectroscopy.
Large crystals were grown in a non-aqueous synthesis system when hydrogen
fluoride was used in trace amounts. The title compound,
[Al3P3O12F]-
[C5H5NH]+ ·0.15H2O,
crystallizes in the triclinic space group P (no. 2), with
Z=2, a=9.118(1), b=9.161(1),
c=9.335(1) Å, α=85.98(1),
β=77.45(1), γ=89.01(1)°,
V=759.25(14) Å3 , R1=0.0280
and wR2=0.0830. UT-6 is a small pore material that has
a three-dimensional network of channels running through the structure. The
structure is closely related to that of chabazite. In addition to
alternating tetrahedral phosphorus and aluminium atoms connected by
bridging oxygens, there are also isolated pairs of octahedral aluminiums
in the four-membered rings of the UT-6 framework that share two bridging
fluorine atoms. The resulting negative charge on the framework is balanced
by pyridinium cations that reside in the chabazite cages. Upon thermal
treatment of UT-6, pyridine molecules and HF are removed from the
structure and the material transforms into rhombohedral
AlPO4-CHA, as evidenced by in situ high-temperature
powder X-ray diffraction, thermogravimetry and mass spectrometry. This
represents the first solid-state transformation of an anionic
aluminophosphate molecular sieve framework to an entirely neutral
one.