collaborators

12 papers

cond-mat.mtrl-sci2026

Nanosecond timescale plasticity in shock-compressed polycrystalline MgO: evidence for transition in mechanism above 100 GPa

A. Chakraborti, H. Ginestet, F. Bertrand +80

The mechanical properties of ceramics under extreme conditions directly impact applications ranging from shielding spacecrafts, designing plasma facing materials in nuclear fusion…

physics.optics2026

Probing laser-driven surface and subsurface dynamics via grazing-incidence XFEL scattering and diffraction

Lisa Randolph, Özgül Öztürk, Dmitriy Ksenzov +34

We demonstrate a grazing-incidence x-ray platform that simultaneously records time-resolved grazing-incidence small-angle x-ray scattering (GISAXS) and grazing-incidence x-ray diff…

physics.plasm-ph2026

A Momentum-Resolved X-ray Thomson Scattering Benchmark of Electronic-Response Models in Warm Dense Aluminium

Dmitrii S. Bespalov, Ulf Zastrau, Zhandos A. Moldabekov +58

The robust diagnosis of conditions generated in warm dense matter (WDM) experiments remains a persistent challenge. Here we describe the measurement of shock-compressed aluminium a…

cond-mat.mtrl-sci2026

Volume Collapse Without a Structural Transition in Shock-Compressed FeO

C. Crépisson, T. Stevens, M. Fitzgerald +121

We report x-ray diffraction and emission spectroscopy of FeO under laser-driven shock compression between 31-199 GPa. FeO retains the B1 (rocksalt) structure along the Hugoniot to…

physics.plasm-ph2026

Probing ultrafast heating and ionization dynamics in solid density plasmas with time-resolved resonant X-ray absorption and emission

Lingen Huang, Mikhail Mishchenko, Michal Šmíd +34

Heating and ionization are among the most fundamental processes in relativistic laser--solid interactions; however, their spatiotemporal evolution remains challenging to capture ex…

cond-mat.mtrl-sci2025

Structural evolution of iron oxides melts at Earth's outer-core pressures

Céline Crépisson, Mila Fitzgerald, Domenic Peake +32

Oxygen and other light elements comprise up to 5 wt% of the Earth's outer-core, and may significantly influence its physical properties and the operation of the geodynamo. Here we…