Synthetic, polycrystalline samples of alunite [K-0.88(H3O)(0.12)Al-2.64(SO4
)(2)(OH)(4.92)(H2O)(1.08)] and oxonium-substituted alunite [H3OAl2.87(SO4)(
2)(OH)(5.61)(H2O)(0.39)] have been investigated using incoherent, inelastic
neutron-scattering (IINS) methods in order to determine the nature of the
non-OH "H2O". IINS measurements were made on non-deuterated samples at 20 K
using the HRMECS chopper spectrometer with 250 and 600 meV incident energi
es. Alunite and oxonium-substituted alunite exhibit Similar spectral featur
es over the energy range of 120-550 meV, where assignments for local vibrat
ions can be made based on the presence of OH and H2O groups. Salient differ
ences in the intensities and positions of the observed low-energy vibration
al bands reflect the effects of chemical substitution on the structural env
ironment ofthe monovalent cation site and neighboring Al and OH sites in th
e framework.