Abstract:
Since many years humanity is trying to understand processes deep inside
our planet. That's why in particular high-pressure research is developing
very fast these days. Thanks to the invention of the diamond anvil cells
(DAC) it is now possible to measure x-ray spectra and investigate
properties of matter under very high compression.
In recent experiments the applied pressure exceeds the Mbar range,
so we can put a sample into the conditions, corresponding to Earth's core.
Of course, such pressure affects electronic structure dramatically and
very often different phase transitions take place. It is of particular
interest to study transition metals because it is a direct way to
understand the relation between crystal structure and stability of
magnetism.
We try to address this problem by means of first-principle
calculations based on Density Functional Theory (DFT). Our major goal is
to understand pressure-driven changes in electronic and magnetic structure
on microscopic level.
In this talk I will show our results on iron-containing alloys: FePd3
and Fe3Al. Both of these systems exhibit different magnetic transtions
under applied pressure, which were observed experimentally. Our results
indicate strong changes in exchange interactions and significant
variation of the Curie temperature in these compounds under compression.