crystals Article P–V–T Equation of State of Iridium Up to 80 GPa and 3100 K Simone Anzellini 1,* , Leonid Burakovsky 2, Robin Turnbull 3 , Enrico Bandiello 3 and Daniel Errandonea 3 1 Diamond Light Source Ltd., Harwell Science & Innovation Campus, Diamond House, Didcot OX11 0DE, UK 2 Los Alamos National Laboratory, Theoretical Divisions, Los Alamos, NM 87545, USA;
[email protected] 3 Departamento de Física Aplicada-Instituto de Ciencia de Materiales, Matter at High Pressure (MALTA) Consolider Team, Universidad de Valencia, Edificio de Investigación, C/Dr. Moliner 50, Burjassot, 46100 Valencia, Spain;
[email protected] (R.T.);
[email protected] (E.B.);
[email protected] (D.E.) * Correspondence:
[email protected] Abstract: In the present study, the high-pressure high-temperature equation of the state of iridium has been determined through a combination of in situ synchrotron X-ray diffraction experiments using laser-heating diamond-anvil cells (up to 48 GPa and 3100 K) and density-functional theory calcula- tions (up to 80 GPa and 3000 K). The melting temperature of iridium at 40 GPa was also determined experimentally as being 4260 (200) K. The results obtained with the two different methods are fully consistent and agree with previous thermal expansion studies performed at ambient pressure. The resulting thermal equation of state can be described using a third-order Birch–Murnaghan formalism with a Berman thermal-expansion model. The present equation of the state of iridium can be used as a reliable primary pressure standard for static experiments up to 80 GPa and 3100 K.