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Researchers explore water locked in Earth's deep interior

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  • Researchers explore water locked in Earth's deep interior

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Chinese Academy of Sciences
The Chinese Academy of Sciences is the linchpin of China's drive to explore and harness high technology and the natural sciences for the benefit of China and the world.
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Schneider Electric
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The seismic discontinuity region, or called the D'' layer, above the core mantle boundary (CMB), contains strong seismic anisotropy, and is characterized by seismic discontinuity, large low-shear-velocity province (LLSVPs) and a strong variable topography. 

The presence of volatiles and major elements (Al, Fe) can remarkably affect the depth of D'' layer and seismic wave velocity anomaly. The existence of volatiles such as H sheds a new light on explaining the geologic feature in D'' layer. Water can incorporate into the crystal lattice as the constitution water of nominally anhydrous minerals (NAM) in mantle. However, the water storage capacity of the lowermost mantle remains controversial due to the inconsistent estimate of the water content at the deep Earth interior. 

By performing first principles calculations at the conditions of lower mantle pressures and temperatures, a research team led by Prof. ZHANG Feiwu from the Institute of Geochemistry of the Chinese Academy of Sciences (IGCAS) systematically investigated the incorporation mechanisms and elastic properties of hydrous Bridgmanite and post-Perovskite. 

The results indicated that the effect of hydration on the elastic wave velocities and moduli, especially the shear velocity and the shear modulus, was more noticeable in the Fe-bearing system than that in the (Al, Fe)-free and Al-bearing systems. 

In the case that coupled Fe3+ and H (0.55 wt.%) occupied Si site, the calculated shear wave anomalies were -2.9% for Bridgmanite and -3.1% for Post-perovskite, respectively, which were very close to the average anomaly value of LLSVPs. This result may imply Mg(Si1-xFex)O3Hx is likely a dominated mineral phase in LLSVPs. 

The calculated P-T phase diagram suggested that the stability range of post-Perovskite was relevant to hydrogen in crystal lattice. The phase transition boundary between Bridgmanite and post-Perovskite shifted to higher or lower pressures when the hydrogen atom substituted in the Mg or Si sites in the lattice, respectively, which could explain the laterally varying thickness of D'' layer. 

The study, published in Earth and Planetary Science Letters, was supported by the National Natural Science Foundation of China. 

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