EGU26-12859, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-12859
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Monday, 04 May, 15:15–15:25 (CEST)
 
Room L1
Examining the Ballistic Transport of Sulfur-Bearing Volatile Species in the Lunar Exosphere
Diana Hayes1, Sébastien Verkercke2, Liam Morrissey3,4, and John Moores1
Diana Hayes et al.
  • 1Centre for Research in Earth and Space Science, York University, Toronto, Canada (hayes954@yorku.ca)
  • 2LATMOS/CNRS, Paris, France
  • 3Department of Engineering and Applied Science, Memorial University, St. John’s, Canada
  • 4Department of Astrophysics, American Museum of Natural History, New York, USA

Although Earth’s Moon lacks a collisional atmosphere, it is known to possess a surface-bounded collisionless exosphere populated by volatile species undergoing thermally-driven ballistic jumps across the surface. Previous models of the lunar exosphere have focused primarily on atomic species (e.g. H, Ar, etc.), with water, hydroxyl (OH), and H2 being the only molecular species that have received significant attention.

However, these are not the only volatile molecular species that exist on the Moon. The LCROSS impactor uncovered a diverse population of volatile species within one of the Moon’s polar permanently-shadowed regions, of which water was the most abundant. Here, we model the exospheric ballistic transport of two sulfur bearing species (H2S and SO2), that were measured in the LCROSS impact plume at abundances of 16.75% and 3.17% relative to water, respectively. As a key component in our model, we use molecular dynamics simulations to determine the surface binding energy distributions of these two species on lunar-like surfaces.

How to cite: Hayes, D., Verkercke, S., Morrissey, L., and Moores, J.: Examining the Ballistic Transport of Sulfur-Bearing Volatile Species in the Lunar Exosphere, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-12859, https://doi.org/10.5194/egusphere-egu26-12859, 2026.