资源环境科技发展态势分析平台

The charge state of dust particles on regolith surfaces exposed to ultraviolet radiation or plasma is investigated for understanding the role of electrostatic dust transport in the surface evolution of airless planetary bodies. Our charge measurement shows that the regolith dust that can be electrostatically transported or lofted carries large negative charges. This result is consistent with our patched charge model, which predicts that dust particles forming microcavities in the regolith surfaces can attain large negative charges by collecting photoelectrons and/or secondary electrons emitted from neighboring particles and the resulting repulsive forces between these negatively charged particles lead to their mobilization. The observed negative charge polarity is contrary to the generally expected positive charges on the regolith dust emitting photoelectrons. The measured negative charges are orders of magnitude larger than the prediction by classical charging models. Our laboratory measurements provide critical initial charging conditions for regolith dust dynamics studies.