The Nature of Carbon Dioxide Bearing Ices in Quiescent Molecular Clouds
| Autor: | D. C. B. Whittet, Yvonne J. Pendleton, Perry A. Gerakines, S. S. Shenoy, A. M. Cook, Jean Chiar |
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| Jazyk: | angličtina |
| Rok vydání: | 2009 |
| Předmět: |
Earth and Planetary Astrophysics (astro-ph.EP)
Physics Nebula Serpens Molecular cloud Extinction (astronomy) FOS: Physical sciences Astronomy and Astrophysics Astrophysics Spectral line Stars Astrophysics - Solar and Stellar Astrophysics Space and Planetary Science Polar Absorption (logic) Astrophysics::Earth and Planetary Astrophysics Solar and Stellar Astrophysics (astro-ph.SR) Astrophysics::Galaxy Astrophysics Astrophysics - Earth and Planetary Astrophysics |
| Popis: | The properties of the ices that form in dense molecular clouds represent an important set of initial conditions in the evolution of interstellar and preplanetary matter in regions of active star formation. Of the various spectral features available for study, the bending mode of solid CO{sub 2} near 15 {mu}m has proven to be a particularly sensitive probe of physical conditions, especially temperature. We present new observations of this absorption feature in the spectrum of Q21-1, a background field star located behind a dark filament in the Cocoon Nebula (IC 5146). We show the profile of the feature to be consistent with a two-component (polar + nonpolar) model for the ices, based on spectra of laboratory analogs with temperatures in the range 10-20 K. The polar component accounts for {approx}85% of the CO{sub 2} in the line of sight. We compare for the first time 15 {mu}m profiles in three widely separated dark clouds (Taurus, Serpens, and IC 5146), and show that they are indistinguishable to within observational scatter. Systematic differences in the observed CO{sub 2}/H{sub 2}O ratio in the three clouds have little or no effect on the 15 {mu}m profile. The abundance of elemental oxygen in the icesmore » appears to be a unifying factor, displaying consistent behavior in the three clouds. We conclude that the ice formation process is robust and uniformly efficient, notwithstanding compositional variations arising from differences in how the O is distributed between the primary species (H{sub 2}O, CO{sub 2}, and CO) in the ices.« less |
| Databáze: | OpenAIRE |
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