From: LARRY KLAES (ljk4_at_msn.com)
Date: Tue Jun 14 2005 - 12:37:34 PDT
Paper: astro-ph/0506254
Date: Sat, 11 Jun 2005 09:01:42 GMT (150kb)
Title: Deuterated H$_3^+$ in proto-planetary disks
Authors: Cecilia Ceccarelli and Carsten Dominik
Comments: accepted for publication in Astronomy & Astrophysics
\\
Probing the gas and dust in proto-planetary disks is central for
understanding the process of planet formation. In disks surrounding solar
type
protostars, the bulk of the disk mass resides in the outer midplane, which
is
cold ($\leq$20 K), dense ($\geq 10^7$ cm$^{-3}$) and depleted of CO.
Observing
the disk midplane has proved, therefore, to be a formidable challenge.
Ceccarelli et al. (2004) detected H$_2$D$^+$ emission in a proto-planetary
disk
and claimed that it probes the midplane gas. Indeed, since all
heavy-elements
bearing molecules condense out onto the grain mantles, the most abundant
ions
in the disk midplane are predicted to be H$_3^+$ and its isotopomers. In
this
article, we carry out a theoretical study of the chemical structure of the
outer midplane of proto-planetary disks. Using a self-consistent physical
model
for the flaring disk structure, we compute the abundances of H$_3^+$ and its
deuterated forms across the disk midplane. We also provide the average
column
densities across the disk of H$_3^+$, H$_2$D$^+$, HD$_2^+$ and D$_3^+$, and
line intensities of the ground transitions of the ortho and para forms of
H$_2$D$^+$ and HD$_2^+$ respectively. We discuss how the results depend on
the
cosmic ray ionization rate, dust-to-gas ratio and average grain radius, and
general stellar/disk parameters. An important factor is the poorly
understood
freeze-out of N$_2$ molecules onto grains, which we investigate in depth. We
finally summarize the diagnostic values of observations of the H$_3^+$
isotopomers.
\\ ( http://arXiv.org/abs/astro-ph/0506254 , 150kb)
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