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.
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