Ar-37 and Ar-39 in meteorites and the spatial cosmic ray gradient

Computer Science

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Argon Isotopes, Cosmic Rays, Meteoritic Composition, Stony Meteorites, Abundance, Histograms, Iron, Nickel, Pribram Meteorite

Scientific paper

Cosmic-ray-produced Ar-37 and Ar-39 in the Fe-Ni phase of meteorites are studied in connection with their implications for the radial gradient of cosmic-ray particles. For the Canon City chondrite, about 20.1 dpm/kg FeNi of Ar-37 and about 22.5 dpm/kg FeNi of Ar-39 are found. Although the Ar-37/Ar-39 ratio is usually employed to deduce a spatial gradient, previously reported Ar-37 data are inconsistent because they fluctuate much more than could be accounted for by different orbits and because the anticipated correlation with cosmic-ray neutron detections is quite weak. As a result, the Ar-37/Ar-39-derived gradient has a low confidence level, but Ar-39 activities group close to a mean value of 22.5 dpm/kg FeNi and appear to be almost independent of the different meteoroid orbits. A comparison of Ar-39 activities in meteorites with those calculated for orbits obtained from fireball data shows that a gradient of 10% per AU or less can be reconciled with the experimental findings.

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