Benjamin J. McCall | |||||||
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Our discovery of H3+ in diffuse clouds (more details), where CO is not the dominant reservoir of carbon, has suggested that the models of H3+ chemistry are using an incorrect value for one of three key parameters: the dissociative recombination rate constant, the electron fraction, or the cosmic-ray ionization rate. To make sense of the observed H3+ column densities, one or more of these values must be changed by almost two orders of magnitude! Our recent storage-ring measurements of H3+ dissociative recombination (more details) suggest that this value is not the source of the problem. This leaves the next most likely suspect as the electron fraction: until recently, we had not been able to detect H3+ in a sightline with sufficient UV flux to enable spectroscopy of H2 and C+ (the source of the electrons).
The combination of these results appears to leave the cosmic-ray ionization rate as the culprit: we suggest that, at least in the cloud towards zeta Persei, the cosmic-ray ionization rate must be a factor of 40 times higher than the canonical value in dense clouds. The fact that we have observed H3+ in many diffuse cloud sightlines suggests that zeta Persei is unlikely to be an unusual case, and that there may be a significant flux of low-energy cosmic rays that have sufficient energy to permeate diffuse, but not dense, clouds. Searches for H3+ in more UV-accessible sightlines continue using CGS4 at UKIRT and NIRSPEC at Keck.
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