Most of the moon’s permanently shadowed areas arose less than 2.2 billion years ago and some trapped ice during the recent past, according to research led by Planetary Science Institute Senior Scientist Norbert Schorghofer.
“These findings change the prediction for where we would expect to find water ice on the moon, and it dramatically changes estimates for how much water ice there is on the moon. Ancient water ice reservoirs are no longer expected,” said Schorghofer, lead author of “Past Extent of Lunar Permanently Shadowed Areas,” which appears in Science Advances.
Lunar water ice is a component integral to missions to the moon, both to maintain human life and for producing fuel for spacecraft. Permanently shadowed regions (PSRs) are thought to have trapped ices and are a main focus of lunar exploration.
The moon steadily migrates away from Earth, and it feels tidal forces from both the Earth and the sun. It was known for decades that the moon experienced a major spin axis reorientation at some point in the deep past, but there wasn’t enough data to really know when. It was only last year that a group in France came up with a coherent history for the evolution of the Earth-moon distance.
“When I heard about their result, I immediately realized it has profound implications for the search of water ice on the moon. I dropped everything I was doing and began to work out the specifics, with the help of my co-author Raluca Rufu,” Schorghofer said. “We calculated the lunar spin axis orientation and the extent of PSRs based on recent advances for the time evolution of the Earth-moon distance.”
Early in its history, the moon (which is 4.5 billion years old) was bombarded by comets and volcanism released water vapor from its interior, but continuously shadowed areas started to appear only 3.4 billion years ago. By that time these processes had started to die down, so most of the water that was delivered to the moon or outgassed from its interior could not have been trapped in the polar regions. Any ice in the polar regions today must have a more recent origin.
“We have been able to quantify how young the lunar PSRs really are,” Schorghofer said. “The average age of PSRs is 1.8 billion years, at most. There are no ancient reservoirs of water ice on the moon.”
The impact site of the Lunar Crater Observation and Sensing Satellite, a robotic spacecraft that detected water in 2009, lies within a PSR that is less than 1 billion years old, and therefore all the volatiles discovered there—which include water and carbon dioxide—must be young, he said. In a way this is very encouraging, because even the young PSRs contain ice. Older PSRs should contain even more ice.
This work might also explain why the polar regions of planet Mercury have much more ice than the moon’s. Mercury’s PSRs are much older and could have captured water early on.
More information:
Norbert Schörghofer et al, Past extent of lunar permanently shadowed areas, Science Advances (2023). DOI: 10.1126/sciadv.adh4302
Provided by
Planetary Science Institute
Citation:
Study highlights the young age of permanently shadowed lunar areas (2023, September 13)
