Laboratory experiments on the sublimation of methane through ice dust layers and applications to cometary activity

TL;DR

This study uses laboratory experiments to analyze methane sublimation through ice dust layers, revealing how structural water changes and crust thickness influence volatile release, providing insights into cometary activity.

Contribution

It presents new experimental data on methane sublimation through amorphous water ice with layered crusts, simulating cometary conditions and revealing effects of structural changes and crust thickness.

Findings

Methane sublimation varies with heating rate and deposition method.

Thicker indene layers delay methane desorption.

Water ice structural changes drive volatile release.

Abstract

Context. Comets are small celestial bodies made of ice, dust, and rock that orbit the Sun. Understanding their behavior as they warm up at perihelion unveils many pieces of information about the interior and general morphology of the ices hidden under the dust. Aims. The goal of this research is to study the sublimation of CH4 through amorphous solid water (ASW), with a focus on the structural changes in water and the influence of a layer of indene (as a proxy of the crust) during a period of thermal processing, which we use in a controlled laboratory setting to simulate cometary environments. Methods. Ices at a CH4 to H2O abundance ratio of about 0.01 are deposited and layered, or co-deposited, at 30 K and are heated until 200 K (or 140 K) with a ramp of either 1 or 5 K per min. We use mass spectrometry and infrared spectroscopy to analyze the results. Results. Depending on the heating ramp and type of deposition, the sublimation of methane through ASW varies, being lower in intensity and higher in temperature when the co-deposited structure is considered. When two temperature cycles are applied, the second one sees less intense CH4 desorptions. When indene is placed above the ice mixtures, we find that the thicker its layer, the later the methane desorption. Conclusions. The structural changes of water ice drive volatile and hyper-volatile desorption because of the transition from high to low intrinsic density and transformation from amorphous to crystalline. This desorption indicates that such material has been deposited at low temperatures in agreement with previous theories on cometary ices formed in the pre-stellar cloud.