[Baps] Elkins-Tanton seminar, Tue March 28, 2pm, CfA
Sarah Stewart-Mukhopadhyay
sstewart at eps.harvard.edu
Sun Mar 26 11:18:03 EST 2006
Harvard Department of Astronomy
Special Seminar
TUESDAY, MARCH 28
2:00 pm, Phillips Auditorium, 60 Garden St.
Magma Oceans, Early Atmospheres, and Mantle Evolution in Young Terrestrial
Planets
Dr. Linda T. Elkins-Tanton
Brown University
Abstract: Significant and perhaps complete melting of the young
terrestrial planets is expected from radiogenic heating, heat of
accretion, and the potential energy release of core formation. The
rate of subsequent magma ocean solidification is tempered by volatiles
that are degassed to the atmosphere, where they decrease atmospheric
transmission, reduce heat flux from the planets surface, and slow
solidification. I will present results from a new model that
integrates silicate mantle solidification with atmospheric formation,
linking heat flux, convective velocity, and cooling rates with
resulting mantle and atmospheric compositions. Magma ocean processes
may be responsible for initial atmospheric mass and composition,
initial mantle heterogeneity and compositional stability, and
formation of both an early crust and planetary magnetic field.
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