RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 18, ES5001, doi:10.2205/2018ES000628, 2018
Figure 4. Dependence of the permafrost electrical conductivity $\sigma$ and resistivity $\rho$ and pore fluid salinity $S$ on depth $H$ according to the borehole logging data from the mouth of McKenzie River (Beaufort Sea) at 10 m sea depth. Line shows the electrical resistivity log, while the points indicate the salinity values. Modified from [Osterkamp, 2001].
Citation: Piskunova E. A., N. A. Palshin, D. V. Yakovlev (2018), Electrical conductivity features of the Arctic shelf permafrost and electromagnetic technologies for their studies, Russ. J. Earth Sci., 18, ES5001, doi:10.2205/2018ES000628.
Copyright 2018 by the Geophysical Center RAS.
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