Carbon capture and storage [CCS] is crucial for mitigating
CO2 emissions. One of the potential CCS concepts is to
compress
and store the captured CO2 into deep oceanic sediments
as gas hydrates. However, seawater is highly saline [brine], which
may impair the formation/dissociation kinetics and storage of CO2 hydrates. Therefore, it is essential to understand the liquid
CO2 [LCO2] hydrate formation and dissociation
kinetics in static brine systems. In this experimental study, we have
examined the formation/dissociation kinetics and morphology of high-pressure
LCO2 hydrates in brine using a static [unstirred] high-pressure
crystallizer at deep oceanic [1 km] thermodynamic conditions [10 MPa,
1–2 °C]. The results are compared with [unstirred/stirred]
freshwater systems with/without hydrate promoters. Three key stages
have been identified in the experiments: nucleation [stage 1], LCO2-hydrate-brine film formation [stage 2], and LCO2-hydrate-brine film breakage [stage 3]. In the absence of stirring, the formation of the LCO2-hydrate-brine film resists the mass transfer of LCO2 into
the brine, and most likely, the volume expansion during hydrate formation
causes the LCO2-hydrate-brine film to break. New hydrate
morphological growth patterns have been identified. It was estimated
that the hydrate conversion in the freshwater system was higher [27.5%
(±3.04%) in 21.1 (±1.26) h] compared to the brine system
[25.0% in 24.2 (±0.58) h]. LCO2 hydrates dissociate
faster in brine [1.7 (±0.14) h] compared to the freshwater system
[5.7 (±1.77) h]. Finally, the presence of the eco-friendly hydrate
promoter 500 ppm l-tryptophan can delay the dissociation
process.