May 2, 2024

Researchers Uncover Origin and Abundance of Lunar Surface Water

A schematic representation of high-speed hydrogen ions injected from the solar surface into the lunar surface and enhanced on the surface area of lunar soil particles Credit: Prof. Lin Yangtings group
Recently, there has actually been a great deal of focus on the abundance, distribution, and origin of lunar surface area water due to its essential role in future space expedition.
A research study team composed of members from the National Space Science Center and the Institute of Geology and Geophysics, both part of the Chinese Academy of Sciences, discovered that the grain rims of the soil samples gathered by the Chang e-5 objective have high levels of hydrogen and a low ratio of deuterium to hydrogen, constant with the theory that lunar water stems from the solar wind.
The findings were released in the Proceedings of the National Academy of Sciences..

The scientists conducted simulations on the preservation of hydrogen in lunar soils at various temperature levels. They discovered that SW-originated water could be well preserved in the middle and high-latitude regions of the lunar surface area. “The polar lunar soils could consist of more water than Chang e-5 samples,” said Professor Lin Yangting from IGG, matching author of the research study.
Previous research studies have actually shown that water (OH/H2O) on the lunar surface area differs with latitude and time of day (as much as 200 ppm). Such an obvious change indicates a quick desorption rate from the lunar surface area.
In contrast to the 6 Apollo and 3 Luna missions, which all landed at low latitudes (8.97 ° S– 26.13 ° N), the Chang e-5 mission returned soil samples from a middle latitude location (43.06 ° N). In addition, the Chang e-5 samples were collected from the youngest recognized lunar basalts (2.0 Ga) and the driest basaltic basement. Chang e-5 samples are key to attending to the spatial-temporal circulation and retention of SW-derived water in the lunar regolith.
On 17 lunar soil grains returned by the Chang e-5 objective, the researchers took NanoSIMS depth-profiling measurements of hydrogen abundance and calculated deuterium/hydrogen ratios.
Results revealed that the majority of the grain rims (upper ~ 100 nm) exhibited high concentrations of hydrogen (1,116– 2,516 ppm) with extremely low δD values (-908 ‰ to -992 ‰), implying an SW origin. Based upon the grain size circulation of the lunar soils and their hydrogen content, the bulk SW-derived water content was approximated to be 46 ppm for the Chang e-5 lunar soils, consistent with the remote sensing result.
Heating experiments on a subset of the grains demonstrated that the SW-implanted hydrogen might be maintained after burial. Utilizing this information in addition to previous information, the scientists established a design of the dynamic stability between the implantation and outgassing of SW-hydrogen in soil grains on the moon, exposing that temperature level (latitude) plays a key role in the implantation and migration of hydrogen in lunar soils.
Using this model, they predicted an even greater abundance of hydrogen in the grain rims in the lunar polar areas. “This discovery is of excellent significance for the future utilization of water resources on the moon,” said Professor Lin. “Also, through particle sorting and heating, it is relatively simple to exploit and use the water included in the lunar soil.”.
Referral: “High abundance of solar wind-derived water in lunar soils from the middle latitude” by Yuchen Xu, Heng-Ci Tian, Chi Zhang, Marc Chaussidon, Yangting Lin, Jialong Hao, Ruiying Li, Lixin Gu, Wei Yang, Liying Huang, Jun Du, Yazhou Yang, Yang Liu, Huaiyu He, Yongliao Zou, Xianhua Li and Fuyuan Wu, 12 December 2022, Proceedings of the National Academy of Sciences.DOI: 10.1073/ pnas.2214395119.

The researchers conducted simulations on the preservation of hydrogen in lunar soils at various temperatures. They found that SW-originated water might be well protected in the high-latitude and middle areas of the lunar surface. “The polar lunar soils could include more water than Chang e-5 samples,” said Professor Lin Yangting from IGG, corresponding author of the research study.
“Also, through particle sorting and heating, it is reasonably easy to exploit and utilize the water included in the lunar soil.”.