• journal_title：American Mineralogist
• Contributor：Qiong Liu ; Rebecca A. Lange
• Publisher：Mineralogical Society of America
• Date：2006-
• Format：text/html
• Language：en
• Identifier：10.2138/am.2006.1902
• journal_abbrev：American Mineralogist
• issn：0003-004X
• volume：91
• issue：2-3
• firstpage：385
• section：Articles

High-temperature (867–1534 °C) density measurements were performed in air on 10 liquids in the Na₂O-Fe₂O₃-FeO-SiO₂ (NFS) system and 5 liquids in the K₂O-Fe₂O₃-FeO-SiO₂ (KFS) system using Pt double-bob Archimedean method. Replicate measurements indicate an average reproducibility of 0.22%. Compositions (in mol%) range from 4 to 18 Fe₂O₃, 0 to 3 FeO, 18 to 39 Na₂O, 25 to 37 K₂O, and 43 to 67 SiO₂. Errors in the gram formula weight are ~0.4%. The molar volumes were fitted to a linear compositional model, which gives a compositionally independent partial molar volume (±2σ) for the Fe₂O₃ component (V̄_Fe2O3) of 41.52 ± 0.34 cm³/mol and zero thermal expansivity. The average residual to the fit is ±0.36% for our 57 measurements on 15 liquids at various temperatures. The value for V̄_Fe2O3 in silicate liquids when Fe³⁺ is in fourfold vs. sixfold coordination is estimated to be ~45.5 ± 1 vs. ~34 ± 1 cm³/mol, respectively. Thus, the fitted value of 41.5 cm³/mol appears to reflect an average Fe³⁺ coordination number between 4.5 and 5.0, which is consistent with recently published X-ray absorption fine structure (XAFS) spectroscopy and molecular dynamics (MD) simulations on Fe³⁺-bearing silicate glasses. In the literature, ^VFe³⁺ is inferred to be present in trigonal bipyramidal sites, in contrast to the square pyramidal sites for ^VTi⁴⁺. The lack of a strong compositional or temperature dependence for V̄_Fe2O3 in these alkaline silicate liquids, in contrast to what is observed in the literature for V̄_TiO2 in similar melts, may reflect the different geometries for ^VFe³⁺ and ^VTi⁴⁺.