Published data on the solubility of methane in water covering the range from 70 to 680°F (21 to 360°C) and from 600 to 16,000 psi (4,137 to 110,320 kPa) can be used to construct depth-versus-solubility curves for given geothermal and geopressure gradients.
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L. C. Bonham (1978) studied this question.