The Origin of Nitrogen on Jupiter and Saturn from the N/N Ratio
arXiv:1405.3800 · doi:10.1016/j.icarus.2014.05.007
Abstract
The Texas Echelon cross Echelle Spectrograph (TEXES), mounted on NASA's Infrared Telescope Facility (IRTF), was used to map mid-infrared ammonia absorption features on both Jupiter and Saturn in February 2013. Ammonia is the principle reservoir of nitrogen on the giant planets, and the ratio of isotopologues (N/N) can reveal insights into the molecular carrier (e.g., as N or NH) of nitrogen to the forming protoplanets, and hence the source reservoirs from which these worlds accreted. We targeted two spectral intervals (900 and 960 cm) that were relatively clear of terrestrial atmospheric contamination and contained close features of NH and NH, allowing us to derive the ratio from a single spectrum without ambiguity due to radiometric calibration (the primary source of uncertainty in this study). We present the first ground-based determination of Jupiter's N/N ratio (in the range from to ), which is consistent with both previous space-based studies and with the primordial value of the protosolar nebula. On Saturn, we present the first upper limit on the N/N ratio of no larger than for the 900-cm channel and a less stringent requirement that the ratio be no larger than for the 960-cm channel ( confidence). Specifically, the data rule out strong N-enrichments such as those observed in Titan's atmosphere and in cometary nitrogen compounds. To the extent possible with ground-based radiometric uncertainties, the saturnian and jovian N/N ratios appear indistinguishable, implying that N-enriched ammonia ices could not have been a substantial contributor to the bulk nitrogen inventory of either planet, favouring the accretion of primordial N from the gas phase or as low-temperature ices.
arXiv comment33 pages, 19 figures, manuscript accepted for publication in Icarus
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