A computer simulation study of natural silicate melts. Part I: Low pressure properties
By B. Guillot, N. Sator. 2007
303 citations recorded by the source corpus.
Subfields: Ceramics and Composites, Geophysics
View Paper: https://www.semanticscholar.org/paper/481cf8554a5415f77077f81e1a0f6fd3650bb792
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In Ceramics and Composites
In Geophysics
Citations in the corpus
- Nitrogen solubility in molten metal and silicate at high pressure and temperature (2012, methodology): “By assuming a 10 5, and using the 3rd order Birch–Murnaghan equation of state (with K0 = 26 GPa and K 00 ¼ 7 as reported by Guillot and Sator (2007) for a similar silicate melt composition), the pressure correction in our experiments at 4 GPa is about 0.6 and 0.8 GPa at 2500 and 3000 K.”
- Quantitative study of the reactivity of fly ash in geopolymerization by FTIR (2012, background): “In addition, Fe and other cations may also act as network modifiers [25,26].”
- A new transferable interatomic potential for molecular dynamics simulations of borosilicate glasses (2017, methodology): “.172 34.5778 *Fe3+–O 8020.27 0.19 0.0 *Fe2+–O 13032.93 0.19 0.0 *Mg–O 32652.64 0.178 27.2810 *K–O 2284.77 0.29 0.0 * These parameters are sourced from the original Guillot–Sator interatomic potential [39]. They are indicated herein for reference, although these elements are not considered in the pre”