Oxygen vacancy ordering in aluminous bridgmanite in the Earth’s lower mantle


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In this study, the MgAlO2.5 components within aluminous bridgmanite samples was characterized using 27Al nuclear magnetic resonance (NMR) spectroscopy. The NMR spectra exhibited six-, five -, and four -fold coordinated Al species in addition to near eight-fold coordinated Al substituting for Mg (Fig. 1). Five-fold coordinated Al is formed by single-oxygen vacancy sites but four-fold coordination must result from short range ordering of oxygen vacancies, producing oxygen-vacancy clusters (Fig. 2). Characterizing the occurrence of such oxygen-vacancy structures is an important prerequisite for understanding how transport properties change with depth and composition in the lower mantle.

Fig. 1. 2D 27Al satellite-transition MAS spectrum of aluminous bridgmanite, which reveals four distinct Al environments typical for IVAl, VAl and VIAl in addition to Al on the A site of bridgmanite (AAl)

 

Fig. 2. (a-f) Schematic representations of Al defect models within bridgmanite. Examples of potential Al defect structures in bridgmanite for the charge-coupled mechanisms (a, b) and the oxygen vacancy mechanism (c-f).


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