In the lower ionosphere of Mars, the relative density distributions of the major ions CO 2 + , O 2 + , and O + are largely determined by three reactions, including the two channels of the reaction of CO 2 + with O, which yield either O 2 + (R1) or O + (R2), and the reaction of O + with CO 2 , which yields solely O 2 + (R3). There have been only two measurements of the rate coefficients for reactions (R1) and (R2) in the last 50 years, and they are very different (Fehsenfeld et al., 1970; Tenewitz et al., 2018). Although we have carried out a fairly thorough exploration of parameter space in our quest to fit the density profiles of the major ions and O atoms as measured by instruments on the MAVEN spacecraft, we report here only a small fraction of that exploration. In this investigation, we have used the atmosphere of Mars as a laboratory to distinguish between the two sets of rate coefficients. We find that the best fits to the O 2 + , CO 2 + , and O + densities are for the three models in which the Fehsenfeld et al. rate coefficients are adopted, each of which has its advantages. We conclude that the favored O density profile is 1 . 5 ± 0 . 5 times the measured profile, and that the rate coefficients measured 50 years ago are much better than those recently measured at explaining the density profiles of O 2 + , CO 2 + , and O + in the Martian ionosphere as we know it. • There have been only two measured rate constants for the important reactions of CO 2 + + O. • We have used the thermosphere/ionosphere of Mars as a laboratory to distinguish them. • An alternative Te profile is constructed and the O density profiles are scaled by small factors. • We adopt the electron densities measured by the MAVEN LPW and binned as for the ions. • Full 1-D models show that the 50-year old rate coefficients yield better ion density distributions.
Read full abstract