Abstract

Evolutionary structure searches are used to predict stable phases with unique stoichiometries in the hydrogen-rich region of the magnesium/hydrogen phase diagram under pressure. MgH4_4, MgH12_{12} and MgH16_{16} are found to be thermodynamically stable with respect to decomposition into MgH2_2 and H2_2 near 100 GPa, and all lie on the convex hull by 200 GPa. MgH4_4 contains two H−^- anions and one H2_2 molecule per Mg2+^{2+} cation, whereas the hydrogenic sublattices of MgH12_{12} and MgH16_{16} are composed solely of H2δ−_2^{δ-} molecules. The high-hydrogen content stoichiometries have a large density of states at the Fermi level, and the TcT_c of MgH12_{12} at 140 GPa is calculated to be nearly three times greater than that of the classic hydride, MgH2_2, at 180 GPa.

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