http://arxiv.org/abs/2305.01462
Constraints on the interior structure of the Moon have been derived from its inductive response, principally as measured by the magnetic transfer function (TF) between the distantly orbiting Explorer 35 satellite and the Apollo 12 surface station. The most successful prior studies used a dataset 0.01-1 mHz, so the lunar response could be modeled as a simple dipole. However, earlier efforts also produced transfer functions up to 40 mHz. The smaller electromagnetic skin depth at higher frequency would better resolve the uppermost mantle – where key information about primitive lunar evolution may still be preserved – but requires a multipole treatment.
I compute new profiles of electrical conductivity vs depth using both the low-frequency and the full-bandwidth ranges of published Apollo-Explorer TFs. I derive temperature profiles at depths >400 km (<1 mHz) consistent with conductive heat loss and expectations of the iron (and possibly water) content of the mantle. The near-constant iron fraction (Mg# 81 +/- 7) implies either efficient mixing, due to now-defunct convection or perhaps incomplete overturn of gravitationally unstable cumulates following crystallization of the magma ocean.
In contrast, the full-bandwidth analysis produced a different conductivity profile that could not be realistically matched by conduction, convection, partial melting, or simple considerations of lateral heterogeneity. I conclude that the TF method at the Moon is unreliable >>1 mHz. Future EM sounding using the magnetotelluric method can operate up to 100s Hz and is largely insensitive to multipole effects, resolving structure to 100 km or less.
R. Grimm
Wed, 3 May 23
57/67
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