Physics – Geophysics
Scientific paper
Oct 1985
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985geosu...7..303r&link_type=abstract
Geophysical Surveys (ISSN 0046-5673), vol. 7, Oct. 1985, p. 303-384.
Physics
Geophysics
10
Geochemistry, Geodynamics, Geophysics, Soret Coefficient, Volcanoes, Atmospheric Boundary Layer, Explosions, Heat Flux, Long Term Effects, Magma, Time Response
Scientific paper
Double diffusive, or Soret convection phenomena in nature could yield isotope separations. The exotic ratios induced by Soret separations can momentarily cloud many dynamics, running from magma chambers to mantles to distributions among planets, etc., yet they may ultimately furnish explanations for odd oxygen isotope ratios and peculiar distributions in the Caledonian units. Rules attending the heat flux through layers of double diffusive convection suggest that the separation of double diffusive boundary layers in a convecting protosolar system nebula takes on the Titus-Bode law. Soret separation internal to the cloud could lead to interesting distributions in planets that might finally evolve from the boundary layers, each layer acting as a separation stage in a fractionation column.
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