Sound velocities of delta-AlOOH up to core-mantle boundary pressures with implications for the seismic anomalies in the deep mantle

摘要

Recent studies show that -AlOOH is stable up to the base of the mantle. This phase is, therefore, a possible carrier and host of water in the deep mantle. To uncover the physical properties of -AlOOH under deep mantle pressure conditions, we have conducted high-pressure acoustic wave velocity measurements of -AlOOH by using Brillouin spectroscopy combined with high-pressure Raman spectroscopic measurements in a diamond anvil cell up to pressures of 134GPa. There is a precipitous increase by similar to 14% in the acoustic velocities of -AlOOH from 6 to 15GPa, which suggests that pressure-induced O-H bond symmetrization occurs in this pressure range. The best fit values for the high-pressure form of -AlOOH of K-0=190 (2) (GPa), G(0)=160.0 (9) (GPa), (K/P)(0)=K-0=3.7 (1), and (G/P)(0)=G(0)=1.32 (1) indicate that -AlOOH has a 20-30% higher V-S value compared to those of the major constituent minerals in the mantle transition zone, such as wadsleyite, ringwoodite, and majorite. On the other hand, the V-S of -AlOOH is similar to 7% lower than that of Mg-bridgmanite under lowermost mantle pressure conditions because of the significantly lower value of the pressure derivative of the shear modulus. By comparing our results with seismic observations, we can infer that -AlOOH could be one of the potential causes of a positive V-S anomaly observed at similar to 600km depth beneath the Korean peninsula and a negative V-S jump near 2800km depth near the northern margin of the large low-shear-velocity province beneath the Pacific.