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Surface-based Geophysical Monitoring of Conductive Planetary Environments: Integrated Electrical-resistivity-imaging–Electromagnetic-induction Approach

  • Authors: Liam Nell, Joshua Thompson, Dani Storms, Katherine Sluder, Brittany Moehnke, Itunu Apalara, Megan Elwood Madden, Andrew Elwood Madden, Caitlin Hodges, Sina Saneiyan

Liam Nell et al 2026 The Planetary Science Journal 7 .

  • Provider: AAS Journals

Caption: Figure 7.

Relationship between calibrated EMI σ values and various TDR measurements at 0.15, 0.5, and 1.2 m depth. (a) Scatter plots of EMI σ versus TDR measurements. T0–T3 markers represent the four EMI surveys: T0, 2025 March (spring); T1, 2025 June (summer); T2, 2025 September (fall); and T3, 2026 February (winter). Black lines are ordinary least-squares linear fits; R2- and p-values are calculated from four surveys and are exploratory. (b) Temporal relationships are displayed as a function of depth, with EMI σ (black, left axis) and TDR measurements scaled between 0 and 1 (colored, right axis) to represent the relative strength of relationships.

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