Assessing Water Dynamics at Lunar Gravity

Because future plant cultivation on the Moon will require lunar-gravity specific water management, we examined the behavior of water, a glycerol and saline solution under lunar gravity conditions during a flight experiment on Blue Origin’s New Shephard 29 mission. This mission simulated lunar gravity as centrifugal force by rotating the capsule during the weightlessness phase. The menisci of the fluids were imaged, compared with ground controls, and modeled using the Young–Laplace equation. Compared with theoretical values, the estimates for surface tension and capillary length for both controls and flight data were lower than literature values but generated values for glycerol that were higher than for water. These data indicate how the effect of surface features overrides fluid behavior and the difficulty of obtaining experimental data under space flight conditions. The results suggest future studies that include water movement and wetting studies in the presence of lunar regolith as crucial factors to prepare for lunar plant cultivation.

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Publication Details

Journal
Microgravity Science and Technology
Published
2026-09-12
DOI
https://doi.org/10.1007/s12217-026-10277-w
Primary Topic
Planetary Science and Exploration
Type
article
Field-Weighted Citation Impact
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article

Assessing Water Dynamics at Lunar Gravity

Christopher P. McKay, John Z. Kiss, Karl H. Hasenstein
Microgravity Science and Technology
Planetary Science and Exploration
article

Assessing Water Dynamics at Lunar Gravity

Christopher P. McKay, John Z. Kiss, Karl H. Hasenstein
article en

Abstract

Because future plant cultivation on the Moon will require lunar-gravity specific water management, we examined the behavior of water, a glycerol and saline solution under lunar gravity conditions during a flight experiment on Blue Origin’s New Shephard 29 mission. This mission simulated lunar gravity as centrifugal force by rotating the capsule during the weightlessness phase. The menisci of the fluids were imaged, compared with ground controls, and modeled using the Young–Laplace equation. Compared with theoretical values, the estimates for surface tension and capillary length for both controls and flight data were lower than literature values but generated values for glycerol that were higher than for water. These data indicate how the effect of surface features overrides fluid behavior and the difficulty of obtaining experimental data under space flight conditions. The results suggest future studies that include water movement and wetting studies in the presence of lunar regolith as crucial factors to prepare for lunar plant cultivation.

Microgravity Science and TechnologyVol. 38(5)
Florida Institute of Technology (US), Ames Research Center (US), University of Louisiana at Lafayette (US)
Clean water and sanitation
Openalex Percentile: Top 10%
Planetary Science and Exploration
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