Geology

Soil water

Organic chemistry

Lunar soil

Plagioclase

Olivine

Maturity (psychological)

Developmental psychology

Geochemistry

Paleontology

Psychology

Soil science

Mineralogy

Chemistry

Geotechnical engineering

Mineral

Water content

Pyroxene

Quartz

Environmental science

Nature Communications

The formation and distribution of lunar surficial water remains ambiguous. Here, we show the prominence of water (OH/H2O) attributed to solar wind implantation on the uppermost surface of olivine, plagioclase, and pyroxene grains from Chang'E-5 samples. The results of spectral and microstructural analyses indicate that solar wind-derived water is affected by exposure time, crystal structure, and mineral composition. Our estimate of a minimum of 170 ppm water content in lunar soils in the Chang'E-5 region is consistent with that reported by the Moon Minerology Mapper and Chang'E-5 lander. By comparing with remote sensing data and through lunar soil maturity analysis, the amount of water in Chang'E-5 provides a reference for the distribution of surficial water in middle latitude of the Moon. We conclude that minerals in lunar soils are important reservoirs of water, and formation and retention of water originating from solar wind occurs on airless bodies.

Chang’E-5 samples reveal high water content in lunar minerals