- #1
MarkBurg
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Hi,
In an enclosed system - of say Methane & water - in which the water column is sufficiently large to have significant pressure and some modest temperature difference due to gravity and geothermal effects, how would one calculate / predict the changing methane concentration (or partial pressure) down the column from a reference point (known concentration, pressure and temperature), assuming no/limited convection?
I've seen a few papers and procedures for calculating maximum (saturated) solubilities as a function of pressure, temperature and salinity, but haven't figured out how to estimate how the concentration profile might change down a static, contigous, undersaturated water column.
Can anyone provide some pointers?
Would concentrations remain constant due to diffusion?
Would the system tend to maintain uniform fugacity of the dissolved gas?
Thanks,
Mark
In an enclosed system - of say Methane & water - in which the water column is sufficiently large to have significant pressure and some modest temperature difference due to gravity and geothermal effects, how would one calculate / predict the changing methane concentration (or partial pressure) down the column from a reference point (known concentration, pressure and temperature), assuming no/limited convection?
I've seen a few papers and procedures for calculating maximum (saturated) solubilities as a function of pressure, temperature and salinity, but haven't figured out how to estimate how the concentration profile might change down a static, contigous, undersaturated water column.
Can anyone provide some pointers?
Would concentrations remain constant due to diffusion?
Would the system tend to maintain uniform fugacity of the dissolved gas?
Thanks,
Mark
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