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Simulations Show Lander Exhaust Could Cloud Studies of Lunar Ices

Simulation showing how water vapor from a lander鈥檚 exhaust spreads throughout the Moon鈥檚 atmosphere (shades of blue and red, with warmer tones being denser) and across its surface (shades of purple, with lighter tones being denser) in 24 hours. The exhaust from a landing site near the Moon鈥檚 south pole takes only a few hours to spread to the other pole.  Credit: 秘密直播 APL
Simulation showing how water vapor from a lander鈥檚 exhaust spreads throughout the Moon鈥檚 atmosphere (shades of blue and red, with warmer tones being denser) and across its surface (shades of purple, with lighter tones being denser) in 24 hours. The exhaust from a landing site near the Moon鈥檚 south pole takes only a few hours to spread to the other pole.

Credit: 秘密直播 APL

A new study led by scientists at the 秘密直播 Applied Physics Laboratory (APL) in Laurel, Maryland, shows that exhaust from a mid-sized lunar lander can quickly spread around the Moon and potentially contaminate scientifically vital ices at the lunar poles.

Computer simulations of water vapor emitted by a 2,650-pound (1,200-kilogram) lander 鈥 about a quarter of the dry mass of the Apollo Lunar Module 鈥 touching down near the Moon鈥檚 south pole showed . From 30% to 40% of the vapor persisted in the lunar atmosphere and surface two months later, and roughly 20% would ultimately freeze out near the poles a few months after that.

Those results, published online Aug. 11 in the Journal of Geophysical Research: Planets, show that researchers鈥 interest in studying the native ices in the Moon鈥檚 poleward craters 鈥 ices that may date back several billion years 鈥 will need to be carefully considered during increased efforts to return humans to the Moon.

Dealing with spacecraft exhaust on the Moon isn鈥檛 a new problem. Researchers appreciated this issue during NASA鈥檚 Apollo missions in the 鈥60s and 鈥70s, when they developed early models to predict the spread of exhaust throughout the lunar atmosphere and contamination of the surface.

鈥淓xhaust during the Apollo mission didn鈥檛 complicate measurements in the same ways that it might now,鈥 said Parvathy Prem, a researcher at APL and the lead author on the study.

During the Apollo era, most of the interest was in collecting lunar samples. While that鈥檚 still true today, the more recent discovery of ices preserved in permanently shadowed craters near the lunar poles has shifted scientific interest to understanding the origin and dispersion of water and other volatile molecules on the Moon鈥檚 surface and in its thin atmosphere.

鈥淭hese are some of the only places where we can find traces of the origin of water in the inner solar system,鈥 Prem said. Reading that record requires measuring the composition of those ices as well as their various isotopes to deduce where they likely came from and how they may have gotten there. Frozen-out exhaust gases from robotic or human exploration that collect on those ices could confound those measurements, even if the lander touches down hundreds of miles away.

鈥淭he interesting thing about Parvathy鈥檚 work is that it shows very well that the effect, while small and temporary, is global,鈥 said Dana Hurley, a planetary scientist at APL and coauthor on the study.

Space organizations can expect volatile gases to significantly coat the lunar surface at well over 60 miles (100 kilometers) from the landing site.

Image showing the distribution of surface ices (depicted as blue dots) at the Moon鈥檚 south pole (left) and north pole (right), detected by NASA鈥檚 Moon Mineralogy Mapper instrument. The grayscale in this image depicts temperature, with darker being colder, showing the ices are concentrated in the darkest and coldest locations, the crater shadows.  Credit: NASA
Image showing the distribution of surface ices (depicted as blue dots) at the Moon鈥檚 south pole (left) and north pole (right), detected by NASA鈥檚 Moon Mineralogy Mapper instrument. The grayscale in this image depicts temperature, with darker being colder, showing the ices are concentrated in the darkest and coldest locations, the crater shadows.

Credit: NASA

The residue exhaust does eventually fade away, but Hurley points out that current plans for human lunar exploration mean it will happen more frequently and with much heavier landers.

鈥淭he results of this study drive the critical need to conduct the research we want to do about the lunar atmosphere and volatile deposits while they are relatively pristine,鈥 Hurley said.

Prem cautions that the model isn鈥檛 foolproof. Among its most salient limitations are that it assumes the degree to which water interacts and 鈥渟ticks鈥 to the lunar surface, which is still uncertain but of great interest for understanding how easily water is transported around the Moon. The model also tracks only water vapor, which comprises about a third of the composition of most landers鈥 exhaust. Other exhaust molecules, such as hydrogen, ammonia and carbon monoxide, may behave differently and perhaps persist even longer.

Follow-up work should include measuring the amount of exhaust that鈥檚 around the Moon during and after future landings, Prem said, which would help narrow in on an answer to how much these exhaust gases 鈥渟tick鈥 to the surface. 鈥淏ut I would also suggest that modeling and monitoring the fate of exhaust gases should be a routine part of lunar mission development and planning.鈥

Conversations about mitigating exhaust gases have only just started, Prem explained.

In January, NASA finalized 16 science and technology demonstration payloads that it had selected to be delivered to the Moon through the Artemis program, including , an instrument that will investigate the chemical response of the lunar surface during a landing as well as any contaminants that may have been injected.

鈥淲hether we intend to or not, we鈥檙e going to do this experiment of bringing exhaust gases with us,鈥 Prem said. It鈥檚 now a matter of deciding how we deal with them.