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    Ar+-C2 Cl4 Reactions and Their Role in the Collection of Ar+37 Produced by Solar Neutrinos

    J. J. Leventhal* and L. Friedman

    • Chemistry Department, Brookhaven National Laboratory, Upton, New York 11973

    • *Permanent address: Department of Physics, University of Missouri-St. Louis, St. Louis, Mo. 63121.

    Phys. Rev. D 6, 3338 – Published 1 December, 1972

    DOI: https://doi.org/10.1103/PhysRevD.6.3338

    Abstract

    A high-pressure gas phase study of the Ar+-C2Cl4 ion-molecule system has been made to determine relative rates of charge transfer and ion-molecule reaction. This study was initiated to investigate assumptions made concerning the collection of Ar+37 produced by the reaction Cl37(ν,e−)Ar37 in the Brookhaven solar neutrino experiment. Charge transfer was found to proceed at high pressures in the gas with a rate more than two orders of magnitude greater than other possible Ar+-C2Cl4 ion-molecule reactions. These results support the argument that Ar+ is not converted into stable charged species which might be missed with techniques used in the solar neutrino experiment.

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