Dichlorodifluoromethane (R-12), monochlorodifluoromethane (R-22), and dichloromonofluoromethane (R-21) were all able to form hydrate compounds under profitable conditions. As a part of basic experiments for the hydrate process, we measured their solubilities for water and NaCl solutions, taking pressures, temperatures, and salt concentrations as experimental factors. The results obtained from those experiments were as follows.
1) At 20°C, 1 atm., solubilities for pure water were R-12:0.03%, R-21:1.2%, and R-22:0.38%, and increased linearly with pressures.
2) On the salt concentrations of solutions N, we obtained the following equation. KN=log S/S
o(K: const., S, S
o: solubilities for NaCl solutions and pure water, respectively)
3) The thermal coefficient of solubilities was negative, and when pressures and salt concentrations were kept constant, the following relations were recognized. ΔH/R=-dlog S/d (1/T)
By these relations, heats of dissolution ΔH were calculated (R-12:5.9, R-21:10.1, R-22:7.3kcal/g mol), and moreover with those values, it was possible to correct the heats of hydrate formation.
4) Activity coefficients γ amounted to several thousands for R-12 and several hundreds for R-21. When only salt concentrations were kept constant, γ decreased with the increases of solubilities and could be drawn on a curved line.
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