Thermoelastic Anomaly of Iron Carbonitride Across the Spin Transition and Implications for Planetary Cores

Thermoelastic Anomaly of Iron Carbonitride Across the Spin Transition and Implications for Planetary Cores

Abstract Carbon and nitrogen are considered as candidate light elements present in planetary cores. However, there is limited understanding regarding the structure and physical properties of Fe‐C‐N alloys under extreme conditions. Here diamond anvil cell experiments were conducted, revealing the sta...

Full description

Bibliographic Details
Main Authors: Shengxuan Huang, Xiang Wu, Stella Chariton, Vitali Prakapenka, Shan Qin, Bin Chen
Format: Article
Language:English
Published: Wiley 2024-08-01
Series:Geophysical Research Letters
Subjects:
iron carbonitride
planetary core
spin transition
thermal equation of state
high pressure
Online Access:https://doi.org/10.1029/2024GL108973

Internet

https://doi.org/10.1029/2024GL108973

Similar Items