Physics
Scientific paper
Feb 1993
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993jgr....98.2075h&link_type=abstract
Journal of Geophysical Research (ISSN 0148-0227), vol. 98, no. B2, p. 2075-2089.
Physics
22
Earth Core, Earth Planetary Structure, Mathematical Models, Precambrian Period, Geophysical Fluids, Planetary Evolution
Scientific paper
Formation process of earth's core is studied by numerical simulations of flow field in a self-gravitating fluid sphere. The proto-earth was assumed to have gravitationally unstable three-layered structure initially, which consists of the uppermost silicate melt layer, the middle iron layer, and the central undifferentiated silicate-rich protocore. This structure of the heavy iron layer overlying the light protocore leads to Rayleigh-Taylor instability. The numerical simulation supports that the fastest mode of the instability is the translation of the protocore relative to the iron layer, as pointed out by previous studies. Furthermore, the present calculation shows that the translational mode is followed by growth of a gigantic iron drop and intrusion of the iron drop into the protocore. This late stage process is found to be the controlling process of earth's core formation.
Honda Rie
Mizutani Hitoshi
Yamamoto Tetsuo
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