Laboratory simulations of the Vis-NIR spectra of comet 67P using sub-{\mu}m sized cosmochemical analogues

TL;DR

This study uses laboratory simulations with cosmochemical analogues to replicate and understand the spectral properties of comet 67P's surface, revealing key mineral contributions and particle size effects.

Contribution

It introduces a novel laboratory approach with sub-micron analogues to match the comet's spectral features, highlighting the roles of coal, pyrrhotite, and silicates.

Findings

Best spectral match with coal, pyrrhotite, and silicates mixture

Grain sizes align with Rosetta dust particle measurements

Pyrrhotite influences low albedo and spectral slope

Abstract

Laboratory spectral measurements of relevant analogue materials were performed in the framework of the Rosetta mission in order to explain the surface spectral properties of comet 67P. Fine powders of coal, iron sulphides, silicates and their mixtures were prepared and their spectra measured in the Vis-IR range. These spectra are compared to a reference spectrum of 67P nucleus obtained with the VIRTIS/Rosetta instrument up to 2.7 {\mu}m, excluding the organics band centred at 3.2 {\mu}m. The species used are known to be chemical analogues for cometary materials which could be present at the surface of 67P. Grain sizes of the powders range from tens of nanometres to hundreds of micrometres. Some of the mixtures studied here actually reach the very low reflectance level observed by VIRTIS on 67P. The best match is provided by a mixture of sub-micron coal, pyrrhotite, and silicates. Grain sizes are in agreement with the sizes of the dust particles detected by the GIADA, MIDAS and COSIMA instruments on board Rosetta. The coal used in the experiment is responsible for the spectral slope in the visible and infrared ranges. Pyrrhotite, which is strongly absorbing, is responsible for the low albedo observed in the NIR. The darkest components dominate the spectra, especially within intimate mixtures. Depending on sample preparation, pyrrhotite can coat the coal and silicate aggregates. Such coating effects can affect the spectra as much as particle size. In contrast, silicates seem to play a minor role.