Abstract

We have performed sound velocity and unit cell volume measurements of three synthetic, ultrafine micro/nanocrystalline grossular samples up to 50 GPa using Brillouin spectroscopy and synchrotron X-ray diffraction. The samples are characterized by average grain sizes of 90 nm, 93 nm and 179 nm (hereinafter referred to as samples Gr90, Gr93, and Gr179, respectively). The experimentally determined sound velocities and elastic properties of Gr179 sample are comparable with previous measurements, but slightly higher than those of Gr90 and Gr93 under ambient conditions. However, the differences diminish with increasing pressure, and the velocity crossover eventually takes place at approximately 20–30 GPa. The X-ray diffraction peaks of the ultrafine micro/nanocrystalline grossular samples significantly broaden between 15–40 GPa, especially for Gr179. The velocity or elasticity crossover observed at pressures over 30 GPa might be explained by different grain size reduction and/or inhomogeneous strain within the individual grains for the three grossular samples, which is supported by both the pressure-induced peak broadening observed in the X-ray diffraction experiments and transmission electron microscopy observations. The elastic behavior of ultrafine micro/nanocrystalline silicates, in this case, grossular, is both grain size and pressure dependent.

Highlights

  • Mg-Fe-Ca bearing garnet with approximate composition (Mg, Fe, Ca)3Al2Si3O12, is one of the major minerals in Earth’s upper m­ antle[1]

  • We report new high-pressure sound velocity and unit cell volume measurements for synthetic ultrafine micro/nanocrystalline grossular samples Gr90, Gr93, and Gr179 with 90 nm, 93 nm, and 179 nm average grain sizes, respectively, up to 50 GPa using Brillouin spectroscopy and synchrotron X-ray diffraction

  • This study provides the first elasticity measurements beyond the stability field of garnet in the Earth’s interior, and the first Brillouin spectroscopy measurements for ultrafine micro/nanocrystalline silicate samples synthesized at ultra-high pressure–temperature conditions

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Summary

Introduction

Mg-Fe-Ca bearing garnet with approximate composition (Mg, Fe, Ca)3Al2Si3O12, is one of the major minerals in Earth’s upper m­ antle[1]. Previous high-pressure sound velocity measurements of endmember grossular samples include a single-crystal Brillouin spectroscopy study up to 10 GPa at 300 ­K5, an ambient temperature micro-polycrystalline ultrasonic study up to 3 ­GPa16, as well as two recent in-situ micropolycrystalline ultrasonic studies combined with X-ray diffraction at simultaneous high pressure–temperature ­conditions[17,18].

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