Laboratory identification of the 4.62mu M solid state absorption band in the ISO-SWS spectrum of RAFGL 7009S

Details Laboratory identification of the 4.62mu M solid state absorption band in the ISO-SWS spectrum of RAFGL 7009S Laboratory identification of the 4.62mu M solid state absorption band in the ISO-SWS spectrum of RAFGL 7009S

Nov 1998

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1998a%26a...339..553d&link_type=abstract

Astronomy and Astrophysics, v.339, p.553-560 (1998)

Astronomy and Astrophysics

Astrophysics

69

Ism: Individual Objects: Rafgl 7009S, Ism: Molecules, Ism: Abundances, Molecular Processes, Dust, Exctinction

Scientific paper

We focus on the problem of the assignment of the ``XCN'' solid state feature observed in the spectra of numerous protostellar objects. This feature, located at 4.62μm has been tentatively identified with the molecular ion OCN(-) . New laboratory experiments have been performed in order to confirm this identification. OCN(-) is produced by UV photolysis of mixtures of CO:NH_3 (1:1) deposited on a cold substrate. Simultaneously, the counterion NH(+_4) is also produced to balance the charge in the matrix. The use of electron donor and acceptor dopants incorporated in the mixtures allows us to reduce or enhance the production of the OCN(-) and NH(+_4) features, thus establishing their ionic character. The production of HNCO when an electron acceptor is used, and the formation of the OCN(-) band during thermal annealing, constitute convincing arguments in favour of the formation of OCN(-) and NH(+_4) by acid-base reactions where the acid HNCO transfers a proton to the base NH_3. We consider the astrophysical implications for the interpretation of the ISO-SWS spectrum of the protostellar source RAFGL 7009S. In this source, the 4.62μm band is deep and large, although the derived abundance of this ion, relative to H_2O ice, is on the order of 4%. Identification of OCN(-) is considered in several other sources. The contribution of NH(+_4) to the unidentified 6.85μm feature is discussed. Based on observations with ISO, an ESA project with instruments funded by ESA Member States (especially the PI countries: France, Germany, the Netherlands and the United Kingdom) and with the participation of ISAS and NASA.

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