Mechanical Spectroscopy on Volcanic Glasses

dc.creatorWagner, Norman
dc.creatorHeide, Klaus
dc.date2005-07-25
dc.date2005-08-18
dc.date.accessioned2026-07-07T06:41:25Z
dc.date.available2026-07-07T06:41:25Z
dc.descriptionMechanical relaxation behaviour of various natural volcanic glasses have been investigated in the temperature range RT-1200K using special low frequency flexure (f~0.63Hz) pendulum experiments. The rheological properties complex Young's modulus M* and internal friction 1/Q have been studied from a pure elastic solid at room temperature to pure viscous melt at log(eta[Pas])=8. Several relaxation processes are assumed to act: the primary alpha-relaxation (viscoelastic process, E_a=(344...554)kJ/mol) above the glass transition temperature T_g=(935...1105)K and secondary anelastic beta', beta and gamma-relaxation processes below T_g. With a simple fractional Maxwell model with asymmetrical relaxation time distribution, phenomenological the mechanical relaxation behaviour, is described. This establish a basis of realistic concepts for modelling of volcanic or magmatic processes.
dc.description52 pages, 20 figures
dc.identifierhttps://arxiv.org/abs/cond-mat/0507559
dc.identifierhttp://arxiv.org/abs/cond-mat/0507559
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/101660
dc.subjectDisordered Systems and Neural Networks
dc.subjectMaterials Science
dc.subjectOther Condensed Matter
dc.subjectGeophysics
dc.titleMechanical Spectroscopy on Volcanic Glasses
dc.typetext

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