The Chemistry of Interstellar OH+, H2O+, and H3O+: Inferring the Cosmic Ray Ionization Rates from Observations of Molecular Ions
David Hollenbach, M. J. Kaufman, D. Neufeld, M. Wolfire, and J. R., Goicoechea

TL;DR
This study models the chemistry of interstellar ions OH+, H2O+, and H3O+ to infer cosmic ray ionization rates from observations, considering effects of PAHs, grain chemistry, and UV flux in different cloud environments.
Contribution
It introduces a comprehensive chemical model including PAHs and grain processes to relate molecular ion observations to cosmic ray ionization rates in interstellar clouds.
Findings
Ion column densities scale with cosmic ray ionization rate and density.
Presence of PAHs affects H3O+ abundance and its independence from ionization rate.
Estimated cosmic ray ionization rate towards W49N is 4-6 x 10^-16 s^-1.
Abstract
We model the production of OH+, H2O+, and H3O+ in interstellar clouds, using a steady state photodissociation region code that treats the freeze-out of gas species, grain surface chemistry, and desorption of ices from grains. The code includes PAHs, which have important effects on the chemistry. All three ions generally have two peaks in abundance as a function of depth into the cloud, one at A_V<~1 and one at A_V~3-8, the exact values depending on the ratio of incident ultraviolet flux to gas density. For relatively low values of the incident far ultraviolet flux on the cloud ({\chi}<~ 1000; {\chi}= 1= local interstellar value), the columns of OH+ and H2O+ scale roughly as the cosmic ray primary ionization rate {\zeta}(crp) divided by the hydrogen nucleus density n. The H3O+ column is dominated by the second peak, and we show that if PAHs are present, N(H3O+) ~ 4x10^{13} cm^{-2}…
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