The strongly correlated material FeSi displays several
unusual
thermal, magnetic, and structural properties under varying pressure–temperature
(P–T) conditions. It is a potential thermoelectric alloy and
a material with several geochemical implications as a possible constituent
at the Earth’s core-mantle boundary (CMB). Previous theoretical
studies predicted a pressure-induced B20–B2 transition at ambient
temperature below 40 GPa; however, experimentally, the structural
transition is observed only under high P–T conditions. In this
study, we have performed high-pressure powder X-ray diffraction (XRD)
up to 90 GPa and Nuclear Resonant Inelastic X-ray Scattering (NRIXS)
measurements up to 120 GPa to understand the phase stability and lattice
dynamics. Our study provides evidence for a nonhydrostatic stress-induced
B20–B2 transition in FeSi at around 36 GPa. We deduced the
Fe partial phonon density of states (PDOS) and thermal parameters
from NRIXS measurements up to 120 GPa and compared them with density
functional theory (DFT) calculations. Additionally, the computations
show pressure-induced metallization and band gap closing at around
12 GPa.