Let and denote the measured fundamental and first-overtone wavenumbers, and put . Differences of the Morse oscillator levels giveConsequently , and . Substituting the two pairs of measured bands gives the following derived quantities:The conversion is , after multiplication by and consistent length units. Therefore the requested ground-state dissociation energies are and . The corresponding potential-well depths are and . These are extrapolations under the stipulated Morse oscillator model; two low-lying bands do not establish the accuracy of the real potential near dissociation.
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