We have predicted a high-pressure hydrous phase of AlOOH stabilizing at {~}170 GPa by first-principles density-functional calculations. The structure predicted has a cubic pyrite-type AlO₂ framework with interstitial H atoms forming symmetric hydrogen bonds, whose symmetry is assigned to the space group Pa3̄ (No. 205). The predicted {δ}-AlOOH to the pyrite-type phase sequence is analogous to a recent theoretical and experimental discovery of high-pressure phase evolution in InOOH and invokes the high-pressure phase relationship in SiO₂, but the transition pressure is much greater in AlOOH than in InOOH. Relative enthalpies also indicate that the dissociation of this phase into a CaIrO₃-type phase of Al₂O₃ plus ice X finally occurs at a further pressure of 300 GPa. The present results suggest that AlOOH has an unexpectedly wide stability range in pressure compared to common hydrous materials.
No takes yet. Share an insight, caveat, or question.
Tsuchiya et al. (2011) studied this question.
Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context: