Japan Geoscience Union Meeting 2025

Presentation information

[J] Oral

S (Solid Earth Sciences ) » S-MP Mineralogy & Petrology

[S-MP29] Physics and Chemistry of Minerals

Wed. May 28, 2025 10:45 AM - 12:15 PM 201A (International Conference Hall, Makuhari Messe)

convener:Nozomi Kondo(Institute for Planetary Materials, Okayama University), Sota Takagi(Korea University), Yuuki Hagiwara(Japan Agency for Marine-Earth Science and Technology), Chairperson:Sota Takagi(Korea University), Yuuki Hagiwara(Japan Agency for Marine-Earth Science and Technology)

12:00 PM - 12:15 PM

[SMP29-11] Rapid increase in sound velocity of calcium aluminosilicate glasses near 10 GPa

*Itaru Ohira1, Steeve Gréaux2, Yoshio Kono3, Jiejun Jing2, Yoshihiro Inoue2, Sho Kakizawa4, Noriyoshi Tsujino4, Yuji Higo4 (1.Department of Chemistry, Faculty of Science, Gakushuin University, 2.Geodynamics Research Center (GRC), Ehime University, 3.Department of Physics and Astronomy, Kwansei Gakuin University, 4.Japan Synchrotron Radiation Research Institute (JASRI))

Keywords:Aluminosilicate glass, High pressure, Sound velocity, Synchrotron X-ray

Aluminum ion is considered to play a key role in densification of aluminosilicate glasses, structural and compositional analogs of magmas. Al–O coordination number (CN) starts to increase at lower pressure condition than Si–O CN (e.g., [1]), suggesting that Al-rich aluminosilicate glasses may undergoes densification at lower pressures than Al-poor glasses. In addition to this change in short-range order, the recent study on CaAl2O4 glass found the quick densification by shrinking the voids between Ca and O at a narrow pressure range of 8–10 GPa [2]. The intermediate-range order change and the subsequent short-range order change may be a general process of the rapid densification of aluminosilicate glasses and melts. To clarify the possible existence of this densification process in more natural and complex systems, we conducted the combined in situ X-ray and ultrasonic measurements on CaO–Al2O3–SiO2 (CAS) glasses in a wide range of Al/Si molar ratio (Al/Si = 1–4).
The sample glasses are CaAl2Si2O8 (anorthite, Al/Si = 1), CaAl2SiO6 (Al/Si = 2), Ca2Al6Si2O15 (Al/Si = 3), and CaAl4SiO9 (Al/Si = 4) glasses, synthesized by the container-less aerodynamic heating system at GRC, Ehime University [2]. The ultrasonic measurements were carried out at the beamline BL04B1, SPring-8, and we obtained the VP and VS of the four glass samples up to 25 GPa. Under compression, all the samples showed the modest decrease in VP and VS, followed by an abrupt increase in both values over ~7–10 GPa. Above 10 GPa, the VP and VS continue to increase gradually and linearly with increasing pressure. In addition to the rapid increase in velocity, ~10% reduction of the sample lengths was also observed at ~7–10 GPa. The abrupt changes in elastic behavior are consistent with CaAl2O4 glass [2]. The present results indicate that the rapid densification at ~7–10 GPa might be a common process in CAS glass, and its pressure condition and the degree of velocity increase are independent of the Al/Si ratio.

References
[1] B. Mysen & P. Richet. Silicate glasses and melts: second edition. Elsevier (2019).
[2] I. Ohira et al. Phys. Rev. B 110, 054115 (2024).