H3+
Spectra of three interstellar clouds showing absorption lines due to the R(1,1)u and R(1,0) transitions of H3+. Arrows indicate the expected positions of the absorption features from previous measurements of the interstellar gas velocity.
Observations
H3+ is extremely important to the chemistry of interstellar clouds. This is because H3+ willingly donates its extra proton to a variety of collision partners, thus laying the foundation for a large network of ion-molecule reactions.
The reactions surrounding the formation and destruction of H3+ are relatively simple. It is generally assumed that a cosmic ray first ionizes H2, which then collides with another H2 molecule to form H3+ and H. In diffuse clouds H3+ is destroyed via electron recombination, while in dense clouds destruction primarily occurs by charge tranfer with CO. This overall simplicity allows observations of H3+ to be used in estimating the ionization rate of H2 due to cosmic rays.
The cosmic-ray ionization rate in the ISM has previously been estimated using various molecular tracers such as OH, HD, HCO+, and H3O+. While these studies have found an average value of about 10-17 s-1, individual results have varied over a few orders of magnitude. Using the United Kingdom Infrared Telescope, we have observed H3+ absorption in several diffuse molecular cloud sight lines and inferred an average ionization rate of 4x10-16 s-1. Because the chemistry behind H3+ is so much simpler than for the other tracers, we believe that this is the most accurate determination of the cosmic-ray ionization rate to date.
Theoretical Calculations
In addition to ionizing H and H2, cosmic rays can also spall atomic nuclei and excite atomic nuclear states. Spallation of C, N, and O will produce the light element isotopes 6Li, 7Li, 9Be, 10B, and 11B, while nuclear excitation of 12C and 16O will emit 4.4 MeV and 6.1 MeV gamma rays, respectively. Exactly how much these processes occur depends on the energy spectrum of cosmic rays in the 1 MeV - 10 GeV range. Unfortunately, cosmic rays in this energy range are unobservable at the Earth due to the solar wind. As a result, we have tested multiple low energy spectra in an attempt to reproduce light element, gamma ray, and ionization observations.

Three theoretical distributions of the differential cosmic-ray flux at low energies. These cosmic-ray spectra were used with various cross sections to predict the ionization rate of atomic hydrogen, light element isotope production rates, and gamma-ray line fluxes.
Related Content
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| 16 | N. Indriolo "Astrochemical Constraints on the Cosmic-Ray Ionization Rate" Research Prospectus for Preliminary Examination, Department of Astronomy, University of Illinois, 2008. |

