To enhance the progress of hydrate-based technologies,
obtaining
accurate and comprehensive data on hydrate equilibria is vital. The
presence of mineral salts in water necessitates an examination of
their impact on the phase behavior of gas hydrates. This research
aims to explore the influence of NaCl and MgCl2, the primary
dissolved salts in natural water, on the tetrahydrofuran (THF)–CH4 hydrate system. Experiments are conducted using the isochoric
pressure search method with a step-heating technique, covering a range
of pressures (1–55 MPa), temperatures (283–300 K), and
THF mass fractions (0.05–0.19). The Chen and Guo theory is
utilized to extend a thermodynamic model that predicts the behavior
of the THF–CH4 hydrate system in the absence or
presence of mineral salts. The model demonstrates a satisfactory level
of consistency with the generated hydrate data, with an average absolute
relative deviation of only 6.05%. Methane’s properties in the
gas phase are derived using the Soave–Redlich–Kwong
equation of state (SRK EoS). Additionally, the e-UNIQUAC model is
employed to calculate the activity of water and the activity coefficient
of THF in the electrolyte aqueous phase. The experimental results
indicate that THF effectively addresses the challenges associated
with methane hydrate formation in saline water, making it a promising
promoter. Furthermore, the study reveals that the inhibitory effect
of salts is more pronounced in concentrated THF solutions, and increasing
the pressure for hydrate formation enhances the inhibitory effect
of salts.