Electrostatic Repulsion of Dust from Planetary Surfaces
arXiv:2301.11609 · doi:10.3847/PSJ/acad7f
Abstract
Surfaces of planetary bodies can have strong electric fields, subjecting conductive grains to repulsive electrostatic forces. This has been proposed as mechanism to eject grains from the ground. To quantify this process, we study mm-sized basalt aggregates consisting of micrometer constituents exposed to an electric field in drop tower experiments. The dust aggregates acquire high charges on sub-second timescales while sticking to the electrodes according to the field polarity. Charging at the electrodes results in a repulsive (lifting) force and continues until repulsion overcomes adhesion and particles are lifted, moving towards the opposite electrode. Some aggregates remain attached, which is consistent with a maximum charge limit being reached, providing an electrostatic force too small to counteract adhesion. All observations are in agreement with a model of moderately conductive grains with a small but varying number of adhesive contacts to the electrodes. This supports the idea that on planetary surfaces with atmospheres, electrostatic repulsion can significantly contribute to airborne dust and sand, i.e. decrease the threshold wind speed that is required for saltation and increase the particle flux as suggested before.
References in corpus (7)
- Sticking Properties of Silicates in Planetesimal Formation Revisited
- Failed Growth at the Bouncing Barrier in Planetesimal Formation
- Drifting inwards in protoplanetary discs II: The effect of water on sticking properties at increasing temperatures
- Crossing barriers in planetesimal formation: The growth of mm-dust aggregates with large constituent grains
- Observation of bottom-up formation for charged grain aggregates related to pre-planetary evolution beyond the bouncing barrier
- Electrostatic Dust Ejection From Asteroid (3200) Phaethon With the Aid of Mobile Alkali Ions at Perihelion
- Measuring Electric Dipole Moments of Trapped Sub-mm Particles