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- W2796366107 abstract "Significance Presence of iron in Earth’s lower mantle may critically affect its physical properties and thermochemical structures. However, its effects on thermal conductivity and dynamics of deep mantle remain unknown. We studied lattice thermal conductivity of lower-mantle ferropericlase to 120 GPa using ultrafast optics. We observed an enhanced iron substitution effect in the low-spin iron-rich ferropericlase, with thermal conductivity that significantly drops across spin transition. Combined with bridgmanite data, we provided a self-consistent radial profile of lower-mantle thermal conductivity, which is dominated by pressure, temperature, and iron effects and shows a twofold increase throughout the lower mantle. If ultralow velocity zones are hot and strongly enriched in iron, their exceptionally low thermal conductivity will delay their cooling, influencing lowermost mantle dynamics." @default.
- W2796366107 created "2018-04-13" @default.
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- W2796366107 date "2018-04-02" @default.
- W2796366107 modified "2023-10-17" @default.
- W2796366107 title "Effects of iron on the lattice thermal conductivity of Earth’s deep mantle and implications for mantle dynamics" @default.
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- W2796366107 doi "https://doi.org/10.1073/pnas.1718557115" @default.
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