

Discrete mesh for the 3-D model with a heterogeneous ice shell thickness. The ice shell surface and base are constrained by models depicted in Figure 1 and described in Table 1. The yellow circle depicts the ice base of the mean ice shell, corresponding to the 1-D model. Three colors denote ice, ocean, and core regions. Each region is assigned a homogeneous electrical conductivity according to Table 2. The total number of cells in the mesh is 126976. — astro-ph.EP
Electromagnetic (EM) sounding can constrain the electrical structure of Enceladus and, in turn, the salinity of its ocean and the porosity, fluid content, and thermal state of its hydrothermally active core.
Here, we assess the feasibility of EM sounding at Enceladus using both global (orbiter) and local (lander) EM induction transfer functions. We provide a physical framework for modeling EM induction for 1-D and 3-D subsurface conductivity models and discuss how transfer functions can be estimated from global or local measurements of the magnetic and electric fields.
We simulate 3-D induction effects arising from variations in ice-shell thickness. The magnitude of these effects in the magnetic field correlates with the ice-shell thickness at the surface and is strongly dependent on the ocean’s conductivity. These magnetic variations, if observed, would favor a moderately to highly conductive ocean, providing lower bounds on salinity and volatile content. The absence of these effects indicates a thicker, more homogeneous ice shell and/or a lower-conductivity ocean. Given plausible magnitudes, a polar-orbiting mission with low-altitude measurements will be required to detect these effects.
In summary, an orbiter will constrain global ocean conductivity using long-period induction and possibly map the ice thickness variations. The detailed EM sounding of both the hydrosphere and the core can be achieved by a lander-based broadband EM sounding at periods ≈101−105 s to probe ocean salinity and thickness, as well as core properties including porosity, fluid content, and temperature.
Alexander Grayver, Joachim Saur
Subjects: Earth and Planetary Astrophysics (astro-ph.EP); Geophysics (physics.geo-ph); Space Physics (physics.space-ph)
Cite as: arXiv:2605.09052 [astro-ph.EP] (or arXiv:2605.09052v1 [astro-ph.EP] for this version)
https://doi.org/10.48550/arXiv.2605.09052
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Submission history
From: Alexander Grayver
[v1] Sat, 9 May 2026 16:55:24 UTC (6,815 KB)
https://arxiv.org/abs/2605.09052
Astrobiology, Astrogeology,






