Thermodynamic and Thermoelastic properties of the NAL Phase

Subduction of Mid Ocean Ridge Basalt (MORB) transports crust elements to the deep Earth. Therefore, it is important to study MORB in order to understand geophysical processes in the mantle. The high Al2O3 content of the MORB gives rise to a new aluminous phase (NAL) that constitutes up to 25% of its composition [1]. Phase equilibrium study of MgAl2O4-CaAl2O4 generated the mineral CaMg2Al6O12 with hexagonal symmetry, which was proposed for the NAL phase [2,3]. The NAL chemical composition, however, shows significantly less calcium [1,4] and several compositions have been considered in previous studies of this phase [5,6]. Here we present an ab initio study of NAL phases at high temperatures with several possible compositions. We used the quasiharmonic approximation to address thermodynamic and thermoelastic properties and seismic velocities of this phase as function of composition. References[1] T. Irifune and A. E. Ringwood, Earth Planet. Sci. Lett. 117, 101 (1993). [2] H. Miura, Y. Hamada, T. Suzuki, M. Akaogi, N. Miyajima, and K. Fujino, Am. Mineral. 85, 1799 (2000). [3] M. Akaogi, Y. Hamada, T. Suzuki, M. Kobayashi, and M. Okada, Phys. Earth Planet. Inter. 115, 67 (1999). [4] A. Ricolleau, J. P. Perrillat, G. Fiquet, I. Daniel, J. Matas, A. Addad, N. Menguy, H. Cardon, M. Mezouar, and N. Guignot, J. Geophys. Res. Solid Earth 115, B08202 (2010). [5] M. Mookherjee, B. B. Karki, L. Stixrude, and C. Lithgow-Bertelloni, Geophys. Res. Lett. 39, L19306 (2012). [6] K. Kawai and T. Tsuchiya, Geophys. Res. Lett. 37, L17302 (2010).