First principles calculations on crystalline and liquid iron at Earth's core conditions

1997 ◽  
Vol 106 ◽  
pp. 205-218 ◽  
Author(s):  
Lidunka Vočadlo ◽  
Gilles A. de Wijs ◽  
Georg Kresse ◽  
Mike Gillan ◽  
Geoffrey D. Price
2015 ◽  
Vol 91 (21) ◽  
Author(s):  
Zamaan Raza ◽  
Nina Shulumba ◽  
Nuala M. Caffrey ◽  
Leonid Dubrovinsky ◽  
Igor A. Abrikosov

1998 ◽  
Vol 58 (13) ◽  
pp. 8248-8256 ◽  
Author(s):  
Dario Alfè ◽  
Michael J. Gillan

2014 ◽  
Vol 41 (19) ◽  
pp. 6712-6717 ◽  
Author(s):  
Koichiro Umemoto ◽  
Kei Hirose ◽  
Saori Imada ◽  
Yoichi Nakajima ◽  
Tetsuya Komabayashi ◽  
...  

2000 ◽  
Vol 61 (1) ◽  
pp. 132-142 ◽  
Author(s):  
D. Alfè ◽  
G. Kresse ◽  
M. J. Gillan

2003 ◽  
Vol 67 (1) ◽  
pp. 113-123 ◽  
Author(s):  
D. Alfé ◽  
M. J. Gillan ◽  
G. D. Price

AbstractWe summarize the main ideas used to determine the thermodynamic properties of pure systems and binary alloys from first principles calculations. These are based on the ab initio calculations of free energies. As an application we present the study of iron and iron alloys under Earth,s core conditions. In particular, we report the whole melting curve of iron under these conditions, and we put constraints on the composition of the core. We found that iron melts at 6350士600 K at the pressure corresponding to the boundary between the solid inner core and the liquid outer core (ICB). We show that the core could not have been formed from a binary mixture of Fe with S, Si or O and we propose a ternary or quaternary mixture with 8—10% of S/Si in both liquid and solid and an additional ~8% of oxygen in the liquid. Based on this proposed composition we calculate the shift of melting temperature with respect to the melting temperature of pure Fe of ~—700 K, so that our best estimate for the temperature of the Earth's core at ICB is 5650±600 K.


2018 ◽  
Vol 274 ◽  
pp. 218-221 ◽  
Author(s):  
Yunguo Li ◽  
Lidunka Vočadlo ◽  
Dario Alfè ◽  
John Brodholt

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