Processing of analogues of plume fallout in cold regions of Enceladus by energetic electrons
A. Bergantini, S. Pilling, B. G. Nair, N. J.Mason, and H. J. Fraser

TL;DR
This study investigates how energetic electrons process ice analogues of Enceladus's plume fallout, identifying new molecules and quantifying chemical reaction parameters relevant to the moon's surface chemistry.
Contribution
It provides the first detailed analysis of electron-induced chemistry on Enceladus-like ice mixtures, including detection of new molecules and measurement of reaction cross-sections.
Findings
Detection of molecules like CO, cyanate, formamide, and formaldehyde.
Determination of destruction and formation cross-sections.
Estimation of molecules' half-lives under irradiation.
Abstract
Enceladus, a small icy moon of Saturn, is one of the most remarkable bodies in the solar system. This moon is a geologically active object, and despite the lower temperatures on most of its surface, the geothermally heated south polar region presents geysers that spouts a plume made of water (approximately ninety percent), carbon dioxide, methane, ammonia, and methanol, among other molecules. Most of the upward-moving particles do not have the velocity to escape from the gravitational influence of the moon and fall back to the surface. The molecules in the ice are continuously exposed to ionizing radiation, such as UV and X-rays photons, cosmic rays, and electrons. Over time, the ionizing radiation promotes molecular bond rupture, destroying and also forming molecules, radicals, and fragments. We analyse the processing of an ice mixture analogue to the Enceladus fallout ice in cold…
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