American Mineralogist · 2002 · 191 citations · 35 references
Natural SciencesChemistryMaterials ScienceInorganic ChemistryMaterials ChemistrySpectroscopyGlass MaterialsInfrared SpectroscopyInorganic SpectroscopyIron OxidesGlass CompositionMolar AbsorptivityMolar MassSilicate GlassesSpectral Absorption BandsTotal Water ContentVibrational Absorption Bands
We have determined infrared molar absorptivities for water absorption bands in Fe-bearing and Fe-free andesitic glasses. Water dissolves in andesitic glasses as both hydroxyl groups and molecular water as observed in other silicate glasses. Concentrations of molecular water and hydroxyl species are a strong function of total water content. IR molar absorptivities for Fe-bearing andesite are ε3570 = 62.32 ± 0.42 L/mol·cm, ε4500 = 0.79 ± 0.07 L/mol·cm, ε5200 = 1.07 ± 0.07 L/mol·cm, and ε1630 = 42.34 ± 2.77 L/mol·cm. Molar absorptivities for Fe-free andesite are 69.21 ± 0.52 L/mol·cm for e3570, 0.89 ± 0.07 L/mol·cm for e4500, 1.46 ± 0.07 L/mol·cm for e5200, and 52.05 ± 2.85 L/mol·cm for ε1630. Molar absorptivities show significant compositional dependencies that can be predicted based on tetrahedral cation (Si+4, Al+3)/total cation fraction
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Philosophical transactions of the Royal Society of London. B
HighWire Press · 1886 · 10K citations
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J. L. Bandfield, V. E. Hamilton, P. R. Christensen · Science · 2000 · 664 citations