Abstract
The local structural environments in a series of natural and synthetic alunite samples [ideally AAl3(SO4)2(OH)6, A = H3O+, D3O+, Na+, and K+] have been probed by solid-state 1H, 2H, 23Na, 27Al, and 39K NMR spectroscopy. The natural alunite [KAl3(SO4)2(OH)6] and synthetic hydronium alunite samples contain few structural defects, whereas the synthetic natroalunite and alunite samples have ca. 10% Al vacancies based on 27Al NMR. A new 27Al local environment (AlD) was observed and assigned to Al with one Al vacancy in the first cation sphere. Three different proton environments, Al2-OH, Al - OH2, and H3O+ are detected by 1H and 2H MAS NMR. The hydronium ion (H3O+) is only observed in hydronium alunite, and is associated with the stoichiometric regions of the sample. It was not detected in 1H and 2H NMR spectra of alunite and natroalunite despite K (Na) occupancies of significantly less than 100%, as determined from elemental analysis. Thus, our NMR results suggest that the common assumption, namely that an A vacancy and an Al3+ vacancy are compensated by adding an H3O+and 3H+ (creating 3 Al-OH2 groups), respectively, is too simplistic. Instead, a significant fraction of the Al3+ vacancies are compensated for by 4 H+ ions, resulting in 4 Al-OH2 groups per vacancy. This substitution is accompanied by the simultaneous deprotonation of a H3O+ ion present on the A site. The resultant H2O molecule is unnecessary for charge balance, accounting for the A-site deficiency often observed. The presence of Al3+ and A+ vacancies appears closely correlated based on NMR.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
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- Hammadah al Hamra 193: The first amphibole-bearing winonaite
- Crystal chemistry of trioctahedral micas in alkaline and subalkaline volcanic rocks: A case study from Mt. Sassetto (Tolfa district, Latium, central Italy)
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- The barometer tremolite + tschermakite + 2 albite = 2 pargasite + 8 quartz: Constraints from experimental data at unit silica activity, with application to garnet-free natural assemblages
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- Experimental investigation of the breakdown of dolomite in rock cores at 100 MPa, 650-750 °C
- Dissolution of the (001) surface of galena: An in situ assessment of surface speciation by fluid-cell micro-Raman spectroscopy
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- Co2+-Cu2+ substitution in bieberite solid-solution series, (Co1-xCux)SO4·7H2O, 0.00 ≤ x ≤ 0.46: Synthesis, single-crystal structure analysis, and optical spectroscopy
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- The effect of valence state and site geometry on Ti L3,2 and O K electron energy-loss spectra of TixOy phases
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