47th Lunar and Planetary Science Conference (2016) 1177.pdf NITROGEN CONTENT OF VENUS’ UPPER ATMOSPHERE FROM THE MESSENGER NEUTRON SPECTROMETER. Patrick N. Peplowski1*, David J. Lawrence1, 1Johns Hopkins University Applied Physics La- boratory, Laurel, MD 20723 (*
[email protected]) Introduction: Nitrogen, in the form of N2, is the atmosphere – C and O. As a consequence small chang- second-most abundant compound in the Venusian at- es in the N content of the atmosphere result in large mosphere. Despite being a principle component of the changes to the magnitude of the neutron flux. A similar atmosphere, its concentration is surprisingly uncertain. principle led to a derivation of Ar concentrations with- The most recent (and robust) N2 measurements were in the CO2-dominated Martian atmosphere using Mars made in December 1978, when the Pioneer Venus and Odyssey Neutron Spectrometer measurements [3]. Venera atmosphere entry probes sampled the atmos- Lingenfelter, Hess, and Canfield [2] suggested phere via mass spectroscopy and gas chromatography. placing a lightweight neutron spectrometer in close A review of these measurements led von Zahn et al. [1] proximity to Venus as a means of deriving the N2 con- to adopt a reference value of 3.5±1.8 v% N2 for the tent of the atmosphere. Although no such dedicated Venusian atmosphere. Note that the full, one-standard- experiment was conducted, 54 years after their sugges- deviation range of this value is 46%. Furthermore, this tion the MESSENGER NS fortuitously made this value is for altitudes <45 km only [1], a point that is measurement during the V2 flyby.