Pressure-induced structural transitions in MgH
arXiv:cond-mat/0210463 · doi:10.1103/PhysRevLett.89.175506
Abstract
The stability of MgH has been studied up to 20~GPa using density-functional total-energy calculations. At ambient pressure -MgH takes a TiO-rutile-type structure. -MgH is predicted to transform into -MgH at 0.39~GPa. The calculated structural data for - and -MgH are in very good agreement with experimental values. At equilibrium the energy difference between these modifications is very small, and as a result both phases coexist in a certain volume and pressure field. Above 3.84~GPa -MgH transforms into -MgH; consistent with experimental findings. Two further transformations have been identified at still higher pressure: i) - to -MgH at 6.73 GPa and (ii) - to -MgH at 10.26~GPa.
4 pages, 4 figures
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