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Description
Time-domain Brillouin scattering (TDBS) technique uses ultrafast laser pulses to generate coherent acoustic pulses (CAPs) and monitor their propagation through transparent samples. Local velocity of a CAP along depth of a sample (VA, where A represents longitudinal (L) or transversal (T) sound velocity) is extracted from oscillating intensity of the probe light scattered by the CAP and interfering with that reflected by stationary interfaces [1]. Frequency of the oscillation, fB, is given by the well-known equation used in classical Brillouin light scattering in the backscattering geometry: fB=2 n VA/ λ, where λ is the wavelength in vacuum of the probe laser beam and n the refractive index of the examined material at this wavelength. Spatial distribution of the fB values can be extracted with micron and submicron resolution in lateral and axial directions, respectively. The latter capability of the TDBS technique permits measurement of single crystal elastic moduli, Cij(P), of any transparent solid compressed in a diamond anvil cell (DAC) to Mbar pressures [2] including polycrystalline cubic phases not available at ambient conditions, e.g. high pressure phases [3, 4]. Similarly, shear modulus of an amorphous or of an isotropic polycrystalline solid, G( P), can be determined if its bulk modulus, B( P), is known [5]. In the case of elastically anisotropic solids, the TDBS technique provides 3D-images of texture of the polycrystalline samples including orientation of individual crystallites in space [6]. Finally, it permits 3D-monitoring of progress of phase transitions or chemical reactions to pressures accessible using the DAC technique [7]. Combination of the TDBS technique with high-resolution X-ray diffraction in a DAC provides a straight-forward way to an assumption-free high-pressure scale. A novel secondary pressure scale based on the fB(P) dependence of the mixture of methanol and ethanol in the volume ratio 4:1 was already proposed and applied to measure pressure dependence of yield strength, σy(P), of this amorphous solid [5].
References:
1. Kuriakose M. et al., Ultrasonics 69, 259-267 (2016)
2. Zhang X. et al., J. Geophys. Res.-Solid Earth 128, e2022JB026311 (2023)
3. Raetz S. et al., Phys. Rev. B 99, 224102 (2019)
4. Xu F. et al., Appl. Phys. Lett. 125, 164102 (2024)
5. Hong C. et al., Phys. Rev. B 111, 184110 (2025)
6. Sandeep S. et al., J. Appl. Phys. 130, 053104 (2021)
7. Kuriakose M. et al., New J. Phys. 19, 053026 (2017)