Insights into magma ocean dynamics from the transport properties of basaltic melt.

Insights into magma ocean dynamics from the transport properties of basaltic melt.
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DOI:
10.1038/s41467-022-35171-y
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发表时间:
2022-12-08
影响因子:
16.6
通讯作者:
Karki, Bijaya B.
Karki, Bijaya B.
中科院分区:
综合性期刊1区
文献类型:
--
作者:
Bajgain, Suraj K.;Ashley, Aaron Wolfgang;Mookherjee, Mainak;Ghosh, Dipta B.;Karki, Bijaya B.

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The viscosity of magma plays a crucial role in the dynamics of the Earth: from the crystallization of a magma ocean during its initial stages to modern-day volcanic processes. However, the pressure-dependence behavior of viscosity at high pressure remains controversial. In this study, we report the results of first-principles molecular dynamics simulations of basaltic melt to show that the melt viscosity increases upon compression along each isotherm for the entire lower mantle after showing minima at ~6 GPa. However, elevated temperatures of the magma ocean translate to a narrow range of viscosity, i.e., 0.01–0.03 Pa.s. This low viscosity implies that the crystallization of the magma ocean could be complete within a few million years. These results also suggest that the crystallization of the magma ocean is likely to be fractional, thus supporting the hypothesis that present-day mantle heterogeneities could have been generated during the early crystallization of the primitive mantle. The viscosity of magma plays a crucial role in the dynamics of planet Earth. In this study, the authors show how transport properties of basaltic melt can give us insights into magma ocean dynamics.
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