The properties of materials under extreme conditions of pressure and density are of key interest to a number of fields, including planetary geophysics, materials science, and inertial confinement fusion. In geophysics, the equations of state of planetary materials, such as hydrogen and iron, under ultrahigh pressure and density provide a better understanding of their formation and interior structure [Celliers et al., āInsulator-metal transition in dense fluid deuterium,ā Science 361, 677ā682 (2018) and Smith et al., āEquation of state of iron under core conditions of large rocky exoplanets,ā Nat. Astron. 2, 591ā682 (2018)]. The processes of interest in these fields occur under conditions of high pressure (100 GPaā100 TPa), high temperature (>3000 K), and sometimes at high strain rates (>103 sā1) depending on the process. With the advent of high energy density (HED) facilities, such as the National Ignition Facility (NIF), Linear Coherent Light Source, Omega Laser Facility, and Z, these conditions are reachable and numerous experimental platforms have been developed. To measure compression under ultrahigh pressure, stepped targets are ramp-compressed and the sound velocity, measured by the velocity interferometer system for any reflector diagnostic technique, from which the stress-density of relevant materials is deduced at pulsed power [M. D. Knudson and M. P. Desjarlais, āHigh-precision shock wave measurements of deuterium: Evaluation of exchange-correlation functionals at the molecular-to-atomic transition,ā Phys. Rev. Lett. 118, 035501 (2017)] and laser [Smith et al., āEquation of state of iron under core conditions of large rocky exoplanets,ā Nat. Astron. 2, 591ā682 (2018)] facilities. To measure strength under high pressure and strain rates, experimenters measure the growth of RayleighāTaylor instabilities using face-on radiography [Park et al., āGrain-size-independent plastic flow at ultrahigh pressures and strain rates,ā Phys. Rev. Lett. 114, 065502 (2015)]. The crystal structure of materials under high compression is measured by dynamic x-ray diffraction [Rygg et al., āX-ray diffraction at the national ignition facility,ā Rev. Sci. Instrum. 91, 043902 (2020) and McBride et al., āPhase transition lowering in dynamically compressed silicon,ā Nat. Phys. 15, 89ā94 (2019)]. Medium range material temperatures (a few thousand degrees) can be measured by extended x-ray absorption fine structure techniques, Yaakobi et al., āExtended x-ray absorption fine structure measurements of laser-shocked V and Ti and crystal phase transformation in Ti,ā Phys. Rev. Lett. 92, 095504 (2004) and Ping et al., āSolid iron compressed up to 560 GPa,ā Phys. Rev. Lett. 111, 065501 (2013), whereas more extreme temperatures are measured using x-ray Thomson scattering or pyrometry. This manuscript will review the scientific motivations, experimental techniques, and the regimes that can be probed for the study of materials under extreme HED conditions.
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