The notion of \"distinguishibility\" between bulk elastic parameters on the basis of the Gibbs energy deformation energy. (Articolo in rivista)

Type
Label
  • The notion of \"distinguishibility\" between bulk elastic parameters on the basis of the Gibbs energy deformation energy. (Articolo in rivista) (literal)
Anno
  • 2010-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1007/s00269-010-0354-7 (literal)
Alternative label
  • Pavese A.; Diella V. (2010)
    The notion of "distinguishibility" between bulk elastic parameters on the basis of the Gibbs energy deformation energy.
    in Physics and chemistry of minerals
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Pavese A.; Diella V. (literal)
Pagina inizio
  • 535 (literal)
Pagina fine
  • 541 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 37 (literal)
Rivista
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • Pavese A. - Dipartimento Scienze della terra università di Milano; Diella V. CNR Istituto per la dinamica dei processi ambientali (literal)
Titolo
  • The notion of \"distinguishibility\" between bulk elastic parameters on the basis of the Gibbs energy deformation energy. (literal)
Abstract
  • The present work aims in discussing a principle that distinguishes between elastic parameters sets ( Ko, K', Vo,...), on the basis of an energetic criterion: once a reference set is given, another one can be fixed (minimum), so that they are as close as possible to each other, but yield non-equivalent deformation energy curves, deltaGdeform. Delta G deform calculated using the equation of state (EoS), and its uncertainty, sigma [delta Gdeform], obtained by a propagation of the errors affecting parameters set are crucial to fix which mineral assemblage forms at P-T conditions and allow one to assess the reliability of such a prediction. We explore some properties related to the principle introduced, using the average values of the elastic parameters found in literature and related uncertainties for di-octahedral mica, olivine, garnet and clinopyroxene. Two elementary applications are briefly discussed: the effect of refining V0 in fitting EoSs to P-V experimental data, in the case of garnet and omphacite, and the phengite 3T-2M1 relative stability, controlled by pressure. (literal)
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