Author:
Clark G. R.,Rodgers K. A.,Henderson G. S.
Abstract
Abstract
The structure of doyleite, a rare polymorph of Al(OH)3, has been determined by a three-dimensional single-crystal diffraction study as triclinic, space group P[unk], a = 4.9997(8) Å, b = 5.1681(6) Å, c = 4.9832(6) Å, α = 97.444(10)°, β = 118.688(12)°, γ = 104.661(12)°, V = 104.39(3) Å3, Z = 2. Doyleite has a similar bilayer structure to the other modifications of Al(OH)3, comprising double layers of hcp O atoms with Al atoms occupying two-thirds of the octahedral interstices but is distinct from the other forms in its lateral displacement of adjacent layers and in aspects of the hydrogen bonding pattern. A good correspondence exists between the calculated structure and AFM images of doyleite's (010) surface. The OH-stretching Raman spectrum shows a single broad band centred near 3345 cm−1 with a weaker shoulder at 3615 cm−1 in some spectra. Intra-layer interactions between hydroxyl groups appear to involve limited, if any, bonding between a hydrogen and the next-nearest-neighbour oxygen and show no Raman scattering, in contrast to other Al(OH)3 polymorphs. The ∼100 cm−1 width of doyleite's OH-stretching band is taken as describing the time-averaged hydrogen bondstrength distribution throughout the crystal, with a continuous range of bond strengths consequential upon interchanging positional disorder of the hydrogen atoms and their varying involvement in interplane hydrogen bonds.
Subject
Inorganic Chemistry,Condensed Matter Physics,General Materials Science
Cited by
32 articles.
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