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Energies 2021, 14, 387 18 of 32 5. CO2 Sequestration and NGH Purification Storage of carbon dioxide from a power station or industrial facilities can be feasibly done as climate change mitigation options in subsurface formation within or below the ocean or under the ground. Considering the large-scale capture and storage, it is crucial to highlights the toxicity of CO2. The concentration in the atmosphere is around 0.04% but, if it increases up to 10%, the CO2 acts as an asphyxiant while, if it rises until 20%, the inhalation leads to rapid death. Therefore, once stored, the site will need to be monitored for many years to verify that CO2 can never be released to the atmosphere. The main types of underground storage site are: • Oil and gas wells. They are immediately accessible and used for EOR. During the extraction process, it is possible to achieve an oil with high viscosity (i.e., heavy oil) that it is impossible to extract with conventional methods. The injection of CO2 is one method to enhance oil recovery. The gas remains underground after pumped while the oil can be extract. The sequestered CO2 have to be monitored every days [46]. It can also be used depleted oil and gas fields, providing a storage capacity that will often have pipeline access but with limited capacity. • Coal beds too deep to be mined. These coal beds (relatively rare) usually contain methane, and therefore carbon dioxide can replace it. The recovery methane will offset the cost of carbon dioxide sequestration. • Brine aquifer. It is created when a cap of impermeable rock is formed deep un- derground and prevents water and gas seeping upwards. It can potentially be the most critical type of underground site in which CO2 can replace the brine to remain securely stored. • Sequestrating CO2 as hydrate. Potentially, the CO2 can be trapped as clathrate hy- drates into deep oceanic basins, depleted or existing natural gas hydrate reservoir, sub permafrost region with unfrozen water, and depleted oil and gas partially saturated with water. 5.1. CO2 Storage as Clathrate Hydrates Subsurface CO2 permanent sequestration through clathrate hydrates formation is a novel method to mitigate global warming. Gas hydrate are clathrate compounds in which some guest gas molecules (e.g., CO2, CH4, C2H6) are encapsulated in water molecules. The gas hydrate form under low temperature and high-pressure conditions via hydrogen bonding between water molecules. Reserves of methane in hydrate structure are abundant in geological accumulations in offshore and permafrost environments, and they exceed the all-carbon fossil fuel [47]. Three methods are used to shift the equilibrium and produce methane from oceanic sediments: (i) thermal stimulation through direct heating or injection of heated fluid; (ii) depressurization is the preferred technique for driving gas hydrate dissociation; (iii) injection of chemical inhibitors; (iv) gas swapping [48]. The thermal stimulation method requires a continuous energy source to raise the hydrate temperature above the stability point. The depressurization method decreases the hydrate pressure under the stability point, causing hydrate dissociation. Inhibitor injection involves the injection of a compound at isobaric conditions that shift the equilibrium point to the lower temperature. The injection of CO2 molecule into NGH deposits involves the replacement of CH4 into the water cages that leads to produce methane and store carbon dioxide. CO2 forms a stable hydrate structure at lower pressure conditions than CH4 hydrates at the same temperature, as it is showed in Figure 11. Therefore, CO2 hydrates are more stable than CH4 hydrates under certain conditions (i.e., CO2 and CH4 hydrates equilibrium curves intersect at around 10.5 ◦C and 75 bar), and it can displace the methane in the hydrate structure. In this way, it enables low carbon energy recovery (e.g., CH4) while offsetting capture and transportation cost. Besides, CO2 can re-occupy the pore space from methane recovery, maintaining the mechanical stability of the rock and preventing possible hazards of slope failures. Uchida et al. [49] have demonstrated via experiment andPDF Image | Energies 14
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