Abstract
The results of an electronic band structure calculation for fcc Fe are used to obtain an equation of state for the inner core. Various seismic models of the inner core were used to estimate the temperature distribution and the Grüneisen parameter. The results indicate that the PEM model gives the most consistent description, with an adiabatic temperature distribution starting at 5,500 ± 500°K and a Grüneisen parameter of 1.8 ± 0.4.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.