Ice Lines in Circumbinary Protoplanetary Disks

preprint2013arXivOpen access

Abstract

I examine the position of the ice line in circumbinary disks heated by steady mass accretion and stellar irradiation and compare with the critical semi-major axis, interior to which planetary orbits are unstable. There is a critical binary separation, dependent on the binary parameters and disk properties, for which the ice line lies within the critical semi-major axis for a given binary system. For an equal mass binary comprised of 1 M⊙_{\odot} components, this critical separation is ≈1.04\approx 1.04 AU, and scales weakly with mass accretion rate and Rosseland mean opacity (∝[M˙κR]2/9\propto [\dot{M}κ_R]^{2/9}). Assuming a steady mass accretion rate of M˙∼10−8M⊙yr−1\dot{M} \sim 10^{-8} {\rm M_{\odot} yr^{-1}} and a Rosseland mean opacity of κR∼1cm2g−1κ_R\sim 1 {\rm cm^2 g^{-1}}, I show that ≳80\gtrsim 80% of all binary systems with total masses Mtot≲4.0M⊙M_{\rm tot} \lesssim 4.0 M_{\odot} have ice lines that lie interior to the critical semi-major axis. This suggests that rocky planets should not form in these systems, a prediction which can be tested by looking for planets around binaries with separations larger than the critical separation with \emph{Kepler} (difficult) and with microlensing.

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