Fossil DCN in Orion-KL
- Virginia Univ., Charlottesville (USA) California Univ., Berkeley (USA) National Radio Astronomy Observatory, Charlottesville, VA (USA)
The J = 1 - 0 transition of DCN was mapped toward Orion-KL with the BIMA array. With a synthesized beam width of 7.6 arcsec, emission from the hot core, compact ridge, and northern cloud regions was identified. Over half of the integrated DCN emission detected originates from the hot core component, with progressively smaller contributions from the compact ridge and northern cloud. The DCN fractional abundance is 10 to the -9th in the hot core, 4 x 10 to the -10th in the compact ridge, and 2 x 10 to the -10th in the northern cloud; it is estimated that the corresponding DCN/HCN ratios are about 0.005, 0.02, and 0.02. Chemical models suggest that such high DCN/HCN abundance ratios are produced only in clouds colder than about 20 K. Since the present temperatures near Orion-KL are 50-275 K, it is evident that most of the DCN formed before this region was heated by massive star formation. Much of the fossil DCN which is now observed may have sublimated from icy grain mantles. 32 refs.
- OSTI ID:
- 5756883
- Journal Information:
- Astrophysical Journal; (USA), Vol. 369; ISSN 0004-637X
- Country of Publication:
- United States
- Language:
- English
Similar Records
HERSCHEL FAR-INFRARED SPECTRAL-MAPPING OF ORION BN/KL OUTFLOWS: SPATIAL DISTRIBUTION OF EXCITED CO, H{sub 2}O, OH, O, AND C{sup +} IN SHOCKED GAS
COMPLEX ORGANIC MOLECULES AT HIGH SPATIAL RESOLUTION TOWARD ORION-KL. I. SPATIAL SCALES
Related Subjects
GENERAL PHYSICS
CYANIDES
COSMOCHEMISTRY
DEUTERIUM COMPOUNDS
INTERSTELLAR SPACE
CHEMICAL COMPOSITION
COSMIC GASES
DETECTION
GROUND STATES
HYDROCYANIC ACID
MATHEMATICAL MODELS
MOLECULES
NEBULAE
CHEMISTRY
ENERGY LEVELS
FLUIDS
GASES
HYDROGEN COMPOUNDS
INORGANIC ACIDS
SPACE
640105* - Astrophysics & Cosmology- Galaxies