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Modelling hydrogen in silicate materials

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Abstract

The expectation that the hydroxyl analogue state of positive muons implanted in quartz should be stabilized by a suitable charge compensation centre is supported by preliminary data. The diamagnetic fraction correlates with aluminium content over the narrow range investigated.

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Authors and Affiliations

  1. The Royal Institution of Great Britain, 21 Albemarle Street, London, W1X 4BS, UK

    C.R.A. Catlow & M. Cherry

  2. Department of Chemistry, University of Surrey, Guildford, GU2 5XH, UK

    M. Cherry

  3. Clarendon Laboratory, University of Oxford, Oxford, OX1 3PU, UK

    K.H. Chow

  4. Rutherford Appleton Laboratory, ISIS Facility, Chilton, Didcot, Oxfordshire, OX11 OQX, UK

    S.P. Cottrell & S.F.J. Cox

  5. Department of Physics, University College London, London, WC1E 6BT, UK

    S.F.J. Cox

  6. Department of Physics, University of Leicester, Leicester, LE1 7RH, UK

    E.A. Davis

  7. Department of Geology, University of Manchester, Manchester, M13 9LP, UK

    K.V. Wright

Authors
  1. C.R.A. Catlow
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  2. M. Cherry
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  3. K.H. Chow
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  4. S.P. Cottrell
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  5. S.F.J. Cox
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  6. E.A. Davis
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  7. K.V. Wright
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Catlow, C., Cherry, M., Chow, K. et al. Modelling hydrogen in silicate materials. Hyperfine Interactions 106, 119–122 (1997). https://doi.org/10.1023/A:1012629605599

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  • DOI: https://doi.org/10.1023/A:1012629605599

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