RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 21, ES1003, doi:10.2205/2020ES000723, 2021 Figure 7. The calculated dependence of the solubility of methane in pore waters on the water temperature for the Sevastopol Bay (average depth 11.3 m, $S = 18$ ‰) and the Vistula Lagoon (average depth 2.7 m, $S = 3.8$ ‰) calculated by Henry's Law. Copyright 2021 by the Geophysical Center RAS. Generated from LaTeX source by ELXfinal, v.2.0 software package. |