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The entry is based on a fit of all available field free data
of the OH+ main isotopolog published
by
(1) W. G. D. P. Silva, L. Schneider, U. U. Graf, H. S. P. Müller,
P. Jusko, A. M. Jacob, D. Riechers, S. Schlemmer, and O. Asvany,
2026, Phys. Chem. Chem. Phys., accepted.
The work includes highly accurate hyperfine-resolved low-N
infrared transition frequencies along with N = 1 0 and
2 1 rotational transition frequencies obtained with microwave accuracy.
Further v = 1 0 infrared data with megahertz accuracies
were taken from
(2) C. R. Markus, J. M. Hodges, A. J. Perry, G. S. Kocheril,
H. S. P. Müller, and B. J. McCall,
2016, Astrophys. J. 817, Art. No. 138.
Particularly noteworthy are also vibration-rotation transitions up to
v = 5 4. These were published in
(3) B. D. Rehfuss, M.-F. Jagod, L.-W. Xu, and T. Oka,
1992, J. Mol. Spectrosc. 151, 59.
Also retained in the fit were the N = 1 0 rotational
transition frequencies with HFS splitting were taken from
(4) J. P. Bekooy, P. Verhoeve, W. L. Meerts, and A. Dymanus,
1985, J. Chem. Phys. 82, 3868;
as well as the N = 13 12 transition frequencies with
FS splitting were reported in
(5) D.-L. Liu, W.-C. Ho, and T. Oka,
1987, J. Chem. Phys. 87, 2442.
The calculations should be accurate enough for observational purposes;
increasing caution is advised for N > 5.
The 1H hyperfine structure splitting should be viewed
with slight caution because vibrational changes to the HFS parameters
could not be determined yet.
The electric dipole moment is from a quantum chemical calculation
by
(6) H.-J. Werner, P. Rosmus, and E.-A. Reinsch,
1983, J. Chem. Phys. 79, 905.
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