Due to decarbonization issues, there is growing concern about greenhouse gases, especially carbon dioxide (CO 2 ). Gas hydrate research is a potential solution to energy needs and CO 2 storage tasks. Naturally occurring methane hydrates provide natural gas availability, while CO 2 hydrates are also receiving widespread attention for carbon capture, storage, and pipeline flow assurance. This study measured the thermodynamic equilibrium temperatures and pressures at the dissociation points for CO 2 hydrate mixtures containing various additives. These results provide fundamental data on the thermodynamic phase boundaries of CO 2 hydrate mixtures where three phases of hydrate (H), liquid water (L w ), and vapor (V) coexisted. The equilibrium conditions for CO 2 with pure water and various additives including 2-methoxyethyl ether (0.20 and 0.30 mass fractions), 1,1,3,3-tetramethylguanidine (0.20 and 0.30 mass fractions), 4methylmorpholine (0.10 and 0.20 mass fractions), 1-ethyl-3-methylimidazolium chloride (0.10, 0.20, and 0.30 mass fractions), urea (0.10, 0.20, and 0.30 mass fractions), and 1,3-cyclohexanebis(methylamine) (0.10 and 0.20 mass fractions) were experimentally measured in the pressure range of 1.54−3.58 MPa using the isochoric and temperature cycling method. These additives all had an inhibition effect on the formation of CO 2 hydrates, and the maximum average inhibition effect of each additive on the equilibrium temperature ranged from 5 to 11 K. To simulate seawater conditions, equilibrium conditions for CO 2 hydrate mixtures with three of these additives are also reported. The Clausius−Clapeyron equation was used to estimate possible hydrate structures. The results show that the CO 2 hydrate mixtures exhibited possible sI structures after adding each additive in this study.