Although the 2165 cm(-1) (4.62 mum) "XCN" IR absorption in interstellar ice
s was first detected over 20 years ago, its assignment has remained controv
ersial, and its mode of formation has seldom been studied. Here we report a
n extensive laboratory investigation of this band's formation in interstell
ar ice analogs. Ices with known or suspected interstellar molecules were pr
oton-irradiated at 15-25 K to simulate interstellar energetic processing, a
nd their IR spectra were recorded. Reactions for irradiated mixtures showin
g an XCN spectral band have been developed based on results with chemically
related systems and with over 60 ices examined here. Combined with previou
s work, our new results leave no doubt that the band produced in the labora
tory is due to OCN-, the cyanate anion. Tests of the reactions leading to O
CN- are described, and independent methods of producing OCN- are reported.
The results of all of these new experiments help reveal the chemistry under
lying this ion's formation and establish some of the conditions under which
OCN- might be found in interstellar ices. They also show that energetic pr
ocessing is an efficient way to produce OCN- in interstellar ices and that
temperature increases to promote acid-base chemistry are unnecessary.