DOI: 10.1051/0004-6361:200811302
HD and H2 formation in low-metallicity dusty gas clouds at high redshift
S. Cazaux and M. SpaansKapteyn Astronomical Institute, PO box 800, 9700 AV Groningen, The Netherlands
e-mail: cazaux@astro.rug.nl
Received 6 November 2008 / Accepted 19 December 2008
Abstract
Context. HD and H2 molecules play important roles in the
cooling of primordial and very metal-poor gas at high redshift.
Aims. Grain
surface and gas phase formation of HD and H2 are investigated to
assess the importance of trace amounts of dust,
10-5-10-3
, in the production of HD and H2.
Methods. We
consider carbonaceous and silicate grains and include both
physisorption and chemisorption, tunneling, and realistic grain
surface barriers. We find that, for a collapsing gas cloud environment
with coupled chemical and thermal balance, dust abundances as
small as 10-5 solar lead to a strong boost in the H2 formation
rate due to surface reactions. As a result of this enhancement in
H2, HD is formed more efficiently in the gas phase through the
D+ + H2 reaction. Direct formation of HD on dust grains cannot
compete well with this gas phase process for dust temperatures below
150 K. We also derive up-to-date analytic fitting formulae for the
grain surface formation of H2 an HD, including the different
binding energies of H and D.
Results. Grain surface reactions are crucial to
the availability of H2 and HD in very metal-poor
environments. Above metallicities of 10-5 solar, the grain
surface route dominates the formation of H2, which in turn drives
the formation of HD in the gas phase. At dust temperatures above
150 K, laboratory experiments and theoretical modeling suggest that H2
formation on grains is suppressed while HD formation on grains is
not.
Key words: ISM: dust, extinction -- ISM: molecules -- galaxies: high-redshift
© ESO 2009

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