Georgia Tech scientists have built a laboratory version of solar wind, the stream of particles from the sun that constantly bombards the moon. Using this setup, they created synthetic moon rocks to study how the lunar surface changes over time. The findings, published in The Planetary Science Journal, shed light on a phenomenon called space weathering that reshapes the moon's crust through microscopic impacts and particle bombardment.

Space weathering has long puzzled researchers because it alters the moon's appearance and composition in ways that complicate data interpretation from orbiters. By replicating solar wind exposure in a controlled environment, the team can now isolate how individual factors—like particle energy or exposure duration—affect lunar minerals. This is a critical step toward deciphering remote sensing data from missions such as NASA's Lunar Reconnaissance Orbiter.

The experiments revealed that simulated solar wind causes chemical changes in the synthetic rock samples, including the potential formation of hydroxyl molecules—a precursor to water. The Georgia Tech team observed these transformations at temperatures and pressures similar to the lunar surface. The study provides the first detailed laboratory measurement of how solar wind alone alters rock chemistry without the confounding effects of micrometeorite impacts.

These results could help interpret data from current and future lunar missions, particularly regarding the presence and distribution of water on the moon. If solar wind alone can generate hydroxyl, it suggests water might be more widespread than previously thought—a key consideration for future exploration and resource utilization. The lab setup also allows researchers to test how different lunar terrains respond to space weathering.

"The moon is constantly being modified, and we're just beginning to understand the pace and mechanisms," said one of the study's co-authors. The next step involves combining solar wind simulation with micrometeorite impacts to study their synergistic effects.