Evidence of N2-Ice On the Surface of the Icy Dwarf Planet 136472 (2005 FY9)
S.C. Tegler, W.M. Grundy, F. Vilas, W. Romanishin, D. Cornelison, G.J., Consolmagno

TL;DR
This study provides spectroscopic evidence of N2-ice on the surface of the icy dwarf planet 2005 FY9 by detecting characteristic blueshifts in methane ice absorption bands.
Contribution
It reports the first detection of N2-ice on 2005 FY9 through precise spectral analysis of methane ice band shifts, indicating surface composition complexity.
Findings
CH4-ice bands are blueshifted by about 4 Å, indicating N2 presence.
No significant variation in CH4/N2 ratio across different nights or depths.
Spectral features are consistent with N2-ice similar to Triton and Pluto.
Abstract
We present high signal precision optical reflectance spectra of 2005 FY9 taken with the Red Channel Spectrograph and the 6.5-m MMT telescope on 2006 March 4 UT (5000 - 9500 A; 6.33 A pixel-1) and 2007 February 12 UT (6600 - 8500 A; 1.93 A pixel-1). From cross correlation experiments between the 2006 March 4 spectrum and a pure CH4-ice Hapke model, we find the CH4-ice bands in the MMT spectrum are blueshifted by 3 +/- 4 A relative to bands in the pure CH4-ice Hapke spectrum. The higher resolution MMT spectrum of 2007 February 12 UT enabled us to measure shifts of individual CH4-ice bands. We find the 7296 A, 7862 A, and 7993 A CH4-ice bands are blueshifted by 4 +/- 2 A, 4 +/- 4 A, and 6 +/- 5 A. From four measurements we report here and one of our previously published measurements, we find the CH4-ice bands are shifted by 4 +/- 1 A. This small shift is important because it suggest the…
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