Abstract
The recent interpretation that the μ+ SR signal in crystalline nitrogen at 37 K arises from N2μ+(also written as N2μ+) is examined in the light of ab initio calculations using Hartree-Fock, second-order Møller-Plesset, quadratic configuration interaction and density functional methods. It is concluded that the intrinsic nitrogen quadrupole interaction (2·26 MHz) is too large by more than a factor of two to be assigned to the species N2Mu+. Calculations are extended to the linear complex [N2MuN2]+, which is shown to be more stable and gives a quadrupole interaction closer to the experimental value.