In situ X-ray diffraction studies of iron to Earth-core conditions

By Yanzhang Ma, M. Somayazulu, G. Shen, H. Mao, J. Shu, Russell J. Hemley. 2004

186 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

Phase relations in the Fe-FeSi system at high pressures and temperatures (2013, background): “Dashed black line: melting 824 curve of iron from Ma et al. (2004).”
Density-Functional Perturbation Theory for Quasi-Harmonic Calculations (2011, unknown): “The c/a ratio of ε-Fe has been studied in (Sha & Cohen 2006c) up to temperatures of 6000 K and pressures of 400 GPa by using the QHA, resulting in good agreement with previous calculations (Gannarelli et al. 2003) and X-Ray diffraction experiment (Ma et al. 2004).”
Melting in the Fe–C system to 70 GPa (2009, background): “Although thermal expansion at the temperatures likely to be relevant to the core partially mitigates the problem (Boehler, 1993; Shen et al., 1998; Alfè et al., 2004; Luo and Ahrens, 2004; Ma et al., 2004), recent determinations of the thermal equation of state of iron at high pressures (Dubrovinsky”
Energetics of the Core (2015, result): “The melting curve of Alfe et al. (2002a,b) agrees well with the low-pressure diamond anvil cell results of Shen et al. (1998) and Ma et al. (2004), though not those of Boehler (1993).”