Characterisation of the Fe(III):H+ Defect Centre in Natural Amethyst

A natural single crystal of amethyst was investigated by means of continuous-wave and pulsed Electron Paramagnetic Resonance (EPR), with the aim of structurally characterizing the substitutional S2 Fe(III):H + centre. In this centre, Fe(III) replaces Si(IV) in the tetrahedral site, whereas H + is co...

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Bibliographic Details
Published inApplied magnetic resonance Vol. 51; no. 11; pp. 1607 - 1619
Main Authors Di Benedetto, Francesco, Zoleo, Alfonso, Romanelli, Maurizio
Format Journal Article
LanguageEnglish
Published Vienna Springer Vienna 01.11.2020
Springer Nature B.V
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Summary:A natural single crystal of amethyst was investigated by means of continuous-wave and pulsed Electron Paramagnetic Resonance (EPR), with the aim of structurally characterizing the substitutional S2 Fe(III):H + centre. In this centre, Fe(III) replaces Si(IV) in the tetrahedral site, whereas H + is coupled to Fe(III) to maintain the charge balance. The spectroscopic investigations, mainly the interpretation of the Electron Spin Echo Envelope Modulation, allowed a detailed localisation of the proton to be obtained. H + occurs in the channels crossing the crystal parallel to the crystallographic c axis, in a largely eccentric position. The Fe(III)-H + distance, evaluated in 2.70 Å, is found associated with a non-negligible isotropic hyperfine coupling, which can be linked to the relative stability of the S2 centre in natural amethyst.
ISSN:0937-9347
1613-7507
DOI:10.1007/s00723-020-01275-1