Applications of Planetary Electromagnetic Sounding: Microhertz to Gigahertz

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Scientific paper

EM sounding formally encompasses both propagative (high-frequency) and inductive (low-frequency) methods. Orbital, surface-penetrating radars have been shown to be effective to depths of kilometers on the Moon and in icy parts of Mars, but have been ineffective over the most of Mars' silicate surface. Fixed, surface-based radars will likely improve penetration to no more than several hundred meters. The optimum future application of surface-penetrating radar on Mars is to provide subsurface geological context for rovers. Deep sounding can be accomplished using natural-source induction, and has been used to probe the Moon and Galilean satellites. Applications include Mars groundwater, Venus geodynamics, and the interior of the Moon from crust to core. Magnetotellurics has the advantage of performing a complete sounding from a single station.

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