THE NATURE OF CARBON DIOXIDE BEARING ICES IN QUIESCENT MOLECULAR CLOUDS
Creators
- 1. Department of Physics, Applied Physics and Astronomy, Rensselaer Polytechnic Institute, 110 Eighth Street, Troy, NY 12180 (United States)
- 2. SETI Institute, 515 N. Whisman Road, Mountain View, CA 94043 (United States)
- 3. NASA Ames Research Center, Mail Stop 245-1, Moffett Field, CA 94035 (United States)
- 4. Spitzer Science Center, Mail Code 220-6, California Institute of Technology, Pasadena, CA 91125 (United States)
- 5. Department of Physics, University of Alabama at Birmingham, 310 Campbell Hall, 1300 University Blvd., Birmingham, AL 35294 (United States)
Description
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 CO2 near 15 μm 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 ∼85% of the CO2 in the line of sight. We compare for the first time 15 μm 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 CO2/H2O ratio in the three clouds have little or no effect on the 15 μm profile. The abundance of elemental oxygen in the ices 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 (H2O, CO2, and CO) in the ices.
Availability note (English)
Available from http://dx.doi.org/10.1088/0004-637X/695/1/94Additional details
Identifiers
Publishing Information
- Journal Title
- Astrophysical Journal
- Journal Volume
- 695
- Journal Issue
- 1
- Journal Page Range
- p. 94-100
- ISSN
- 0004-637X
- CODEN
- ASJOAB
INIS
- Country of Publication
- United States
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 41042548
- Subject category
- S79: ASTROPHYSICS, COSMOLOGY AND ASTRONOMY;
- Descriptors DEI
- ABSORPTION; ABUNDANCE; CARBON DIOXIDE; CARBON MONOXIDE; CLOUDS; DUSTS; ICE; INTERPLANETARY SPACE; INTERSTELLAR GRAINS; MATTER; NEBULAE; OXYGEN; STARS; WATER
- Descriptors DEC
- CARBON COMPOUNDS; CARBON OXIDES; CHALCOGENIDES; ELEMENTS; HYDROGEN COMPOUNDS; NONMETALS; OXIDES; OXYGEN COMPOUNDS; PARTICLES; SORPTION; SPACE