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Manned exploration missions to Mars will need dependable in situ resource utilization (ISRU) for oxygen production. The Martian atmosphere is composed of 95.3% CO2, other gases, and 0.13% O2 at ~ 9 mbar (1% of the Earth's pressure). However, it also contains 2-10- μm dust uploaded by dust devils and high winds. Oxygen extraction requires removal of the dust with little pressure drop (Δp). An electrostatic precipitator (ESP) has lower Δp than a filter, but the low pressure causes an electrical breakdown at electric fields ( ~ 1 kV/cm) ~ 30× lower than on Earth, making implementation challenging. Molecular mean free paths (λ = 4 μm) and ion mobility values (b = 0.008 m2/V·s) are ~ 100× larger than at Earth's pressure (λ = 44 nm) and (b = 8.4 ×10-5). The large λ lowers Stokes drag, particularly for smaller particles. Pauthenier field charging dominates for particles with and diffusion charging for d2/5% humid air at 9 mbar. Paschen curves were measured, and I- V curves ( I ~ 5 - 300 μA for V ~ 1.3 - 2.3 kV) were obtained for 5-10-cm-diameter wire/rod-cylinder ESPs. Only positive polarity yielded stable uniform corona. Charging of 0.5-1.3-cm-diameter spheres agreed with the Pauthenier theory. A Martian dust simulant collection efficiency test is in progress.
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Clements et al. (2013) studied this question.
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