First-order theory for Earth's inner-core anisotropy due to super-rotation and Ramachandran interaction

Solidification mechanism at the Lehmann (inner core) boundary are postulated on the basis of Ramachandran interaction by taking the fluctuating inner core super-rotation into account. The postulates are found to be consistent with compressional or P-wave velocity obtained from seismic data analysis. We justify these postulates to be physically sound and precise, and show that the fluctuating inner core super-rotation causes significant changes to the strength of Fe-Fe Ramachandran interaction, which then leads to the observed asymmetric and anisotropic inner core. Our postulates also reliably explain that the depth-dependent anisotropic P-wave attenuation close to inner core surface (to about 100 km deep) is due to phonon excitation probability and different atomic orientation. We also discuss the consistency of our postulates with respect to asymmetric inner core anisotropy (between western and eastern inner core hemispheres).