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Abstracts
10/18
"Exotic Earths: Forming Habitable Worlds with
Giant Planet Migration," S. Raymond, A. Mandell & S. Sigurdsson
2006 Science, 313, 1413
Close-in giant planets (e.g. "Hot Jupiters")
are thought
to form far from their host stars and migrate inward,
through the terrestrial planet zone, via torques with a
massive gas disk. Here we simulate terrestrial planet
growth during and after giant planet
migration. Several-
Earth mass planets also form interior to the migrating
Jovian planet, analogous to recently-discovered "Hot
Earths." Very water-rich, Earth-mass planets form from
surviving material outside the giant planet's orbit,
often in the Habitable Zone and with low orbital
eccentricities. More than a third of the known systems
of giant planets may harbor Earth-like planets.
11/8
Mixing: A Strict Limit on Infall in the
Chemical Evolution of Galaxies
Galactic chemical evolution models assume infalling gas
mixes instantaneously with disk gas. We investigate
whether physically-realistic models for mixing of
infalling gas are consistent with the small present-day
scatter in metallicity logZ, ~ 0.04 dex at most. The
observational limit is well-established for oxygen from
many FUSE/HST lines of sight, and iron and other
elements in star clusters. Unlike previous work, we
solve a kinetic equation for the evolution of the Z
probability distribution. Mixing only occurs in nature
by microscopic diffusion, which must be amplified by a
complex velocity field to bring Z gradients to very
small scales. The two mixing models are instabilities
in ISM-sweeping supernova shells, and interstellar
turbulence. Both processes have time scales that are
well-constrained, and we show that either can account
for the observed scatter in the absence of infall. With
infall, mixing is constantly counteracted by the
addition of gas with Z much different than the disk
mean, and the resulting Z scatter is a factor
of 5 to 10
larger than observed. Infall will not resolve the
so-called G-dwarf problem, the original motivation for
its suggested existence. Our results are the first
quantitative support for qualitative arguments by
Larson (1998) and Haywood (2006) that infall is not
required to account for any major chemical evolution
constraint, and in fact contradicts them.
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