Sukenaga S, Cicconi MR, Yamada H, Wakihara T, Ohara K, Shibata H, Neuville DR (2024)
Publication Type: Journal article
Publication year: 2024
Book Volume: 161
Article Number: 244503
Journal Issue: 24
DOI: 10.1063/5.0243427
The viscosity of silicate melts is one of the most important physical properties for understanding high-temperature phenomena in magmatic systems and material processing. The effects of composition and temperature on viscosity have long been elucidated. Although iron ions are the main components of magmatic systems, their influence on viscosity remains unclear because the behavior of iron is complicated; iron ions have two redox states, Fe3+ and Fe2+. Here, we elucidate the viscosity of an iron-sodium-silicate system with a variety of iron redox states at temperatures close to its glass transition temperature (T
APA:
Sukenaga, S., Cicconi, M.R., Yamada, H., Wakihara, T., Ohara, K., Shibata, H., & Neuville, D.R. (2024). Iron redox effect on the structure and viscosity of a sodium silicate glass and melt. Journal of Chemical Physics, 161(24). https://doi.org/10.1063/5.0243427
MLA:
Sukenaga, Sohei, et al. "Iron redox effect on the structure and viscosity of a sodium silicate glass and melt." Journal of Chemical Physics 161.24 (2024).
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