Laboratory spectra of N2 and CH4 mixtures: Applications to Observations of TNOs

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CH4-ice has multiple low temperature phases that have distinct spectra [1]. In the laboratory, infrared spectra CH4-ice diluted in N2 have absorptions that are different in shape, location, and strength compared to those of pure CH4-ice [2]. However, the full range of dilutions and changes with temperature have not been consistently explored for α-N2-ices. Although, β-N2 ices are common throughout the outer solar system, there are also surfaces where the temperatures are low enough for α-N2 to survive. Recent observations of Eris [3] demonstrate that the surfaces of TNOs may consists of a complex mixture of ices of different phases and dilutions.

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