Transport properties of high albite crystals, near-endmember feldspar and pyroxene glasses, and their melts to high temperature

Anne M. Hofmeister, Alan G. Whittington, Maik Pertermann

Research output: Contribution to journalArticlepeer-review

77 Scopus citations

Abstract

Thermal diffusivity (D) was measured using laser-flash analysis (LFA) from oriented single-crystal albite and glasses near LiAlSi3 O8, NaAlSi3O8, CaAl2 Si2O8, LiAlSi2O6 and CaMgSi2O6 compositions. Viscosity measurements of the supercooled liquids, over 2.6× 108 to 8.9× 1012 Pa s, confirm strongly non-Arrhenian behavior for CaAl2Si2O8, and CaMgSi2 O6, and near-Arrhenian behavior for the others. As T increases, Dglass decreases, approaching a constant near 1,000 K. Upon crossing the glass transition, D decreases rapidly. For feldspars, D for the melt is ∼15% below D of the bulk crystal, whereas for pyroxenes, this difference is ∼40%. Thermal conductivity (klat = pCPD) of crystals decreases with increasing T, but klat of glasses increases with T because heat capacity (CP) increases with T more strongly than density (p) and D decrease. For feldspars, klat for the melt is ∼10% below that of the bulk crystal or glass, whereas this decrease for pyroxene is ∼50%. Therefore, melting substantially impedes heat transport, providing positive thermal feedback that could promote further melting.

Original languageEnglish
Pages (from-to)381-400
Number of pages20
JournalContributions to Mineralogy and Petrology
Volume158
Issue number3
DOIs
StatePublished - 2009

Keywords

  • Albite
  • Anorthite
  • Density
  • Diopside
  • Glass
  • High-temperature
  • Laser-flash analysis
  • LiAlSiO
  • Melt
  • Spodumene
  • Thermal diffusivity
  • Viscosity

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