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Little is known about the effects of X-rays in interstellar ices. To understand the sulfur depletion in dense clouds and the presence of S 2 in comets, we simulated experimentally the soft X-ray processing (0.3 keV) of H 2 S ice for the first time. Experiments were performed under ultrahigh vacuum conditions at 8 K using infrared and quadrupole mass spectrometry to monitor the solid and gas phases, respectively. A UV irradiation experiment using a similar dose was made for comparison. After X-ray irradiation, an infrared absorption appears near 4.0 μm which is attributed to H 2 S 2 formation in the ice. This identification is also supported by the desorption at 133 K of m / z 66, 65, 64, corresponding to the mass fragments of H 2 S 2 . The H 2 S 2 species is expected to be present in interstellar and cometary ices that were processed by X-rays. Further irradiation leads to dissociation of this molecule forming S 2 and larger S-molecules up to S 8 , which may explain the depletion of sulfur in dense clouds. CS 2 was so far the parent molecule proposed for S 2 formation in comets. But the abundance of H 2 S 2 , formed by irradiation of pure H 2 S or H 2 S in an H 2 O–ice matrix, should be larger than that of CS 2 in the ice, the latter requiring a carbon source for its formation. Based on our experimental results, we propose that S 2 in comets could be formed by dissociation of H 2 S 2 in the ice.
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Jiménez-Escobar et al. (2012) studied this question.
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