File:ERT-based Permafrost Island.png: Difference between revisions
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Fig. 1 ERT measurements conducted in 31/07/2015 with an electrode probe interval of 5 m. Permafrost island are roughly determined by the resistivity contour of 1010 Ω, which is the resistivity value at the interface of frozen/unfrozen. Borehole locati... |
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Latest revision as of 08:22, 30 March 2017
Fig. 1 ERT measurements conducted in 31/07/2015 with an electrode probe interval of 5 m. Permafrost island are roughly determined by the resistivity contour of 1010 Ω, which is the resistivity value at the interface of frozen/unfrozen. Borehole locations are marked by black square.
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| Date/Time | Thumbnail | Dimensions | User | Comment | ||
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| delete all | current | 08:22, 30 March 2017 |  | 1,366 × 496 (256 KB) | Bin Cao (talk | contribs) | Fig. 1 ERT measurements conducted in 31/07/2015 with an electrode probe interval of 5 m. Permafrost island are roughly determined by the resistivity contour of 1010 Ω, which is the resistivity value at the interface of frozen/unfrozen. Borehole locati... |
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