2022
DOI: 10.1016/j.cej.2021.134290
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Laboratory demonstration of the stability of CO2 hydrates in deep-oceanic sediments

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Cited by 63 publications
(34 citation statements)
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“…A promising method for sequestration is CO 2 storage in deep-oceanic sediments as gas hydrates. Gas hydrates are crystalline compounds made up of water and one or more hydrate-forming compound, such as CO 2 , methane, and other hydrocarbons. The hydrate-forming molecules are maintained in a metastable crystal lattice formed of water molecules by van der Waals forces within the hydrates , and offer high storage capacity (ideally 184 volumes of gas/volume of water) . Under sufficient depth from the surface, CO 2 hydrates could be formed on the seafloor or within the sediments. , Natural gas hydrates are stable and naturally found in oceanic sediments and permafrost locations, with traces of other gases, such as ethane, CO 2 , and H 2 S. Gas hydrates are stable in nature as a result of the prevalent high-pressure and low-temperature conditions in oceanic sediments and permafrost locations. CO 2 forms hydrate structure I (sI), and a unit cell is made up of 46 hydrogen-bonded water molecules with two dodecahedral cages and six tetrakaidekahedral cages, each of which may theoretically store one CO 2 molecule. , In a large mass of hydrates, some cages may be empty. Gas hydrates can act as a geological reservoir for CO 2 sequestration while also remaining stable as non-destructive structures, which might help to avoid problems, like seabed instability …”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…A promising method for sequestration is CO 2 storage in deep-oceanic sediments as gas hydrates. Gas hydrates are crystalline compounds made up of water and one or more hydrate-forming compound, such as CO 2 , methane, and other hydrocarbons. The hydrate-forming molecules are maintained in a metastable crystal lattice formed of water molecules by van der Waals forces within the hydrates , and offer high storage capacity (ideally 184 volumes of gas/volume of water) . Under sufficient depth from the surface, CO 2 hydrates could be formed on the seafloor or within the sediments. , Natural gas hydrates are stable and naturally found in oceanic sediments and permafrost locations, with traces of other gases, such as ethane, CO 2 , and H 2 S. Gas hydrates are stable in nature as a result of the prevalent high-pressure and low-temperature conditions in oceanic sediments and permafrost locations. CO 2 forms hydrate structure I (sI), and a unit cell is made up of 46 hydrogen-bonded water molecules with two dodecahedral cages and six tetrakaidekahedral cages, each of which may theoretically store one CO 2 molecule. , In a large mass of hydrates, some cages may be empty. Gas hydrates can act as a geological reservoir for CO 2 sequestration while also remaining stable as non-destructive structures, which might help to avoid problems, like seabed instability …”
Section: Introductionmentioning
confidence: 99%
“…24 Under sufficient depth from the surface, CO 2 hydrates could be formed on the seafloor or within the sediments. 25,26 Natural gas hydrates are stable and naturally found in oceanic sediments and permafrost locations, with traces of other gases, such as ethane, CO 2 , and H 2 S. 27−29 Gas hydrates are stable in nature as a result of the prevalent highpressure and low-temperature conditions in oceanic sediments and permafrost locations. 30−32 CO 2 forms hydrate structure I (sI), and a unit cell is made up of 46 hydrogen-bonded water molecules with two dodecahedral cages and six tetrakaidekahedral cages, each of which may theoretically store one CO 2 molecule.…”
Section: Introductionmentioning
confidence: 99%
“…HBS in sub-seafloor sediments has been demonstrated at the lab-scale/theoretical simulations by many researchers worldwide. ,, Still, no field trial has been reported so far. In a lab-scale study, Sun and Peter achieved 39–55% water-to-CO 2 hydrate conversion in 24 h, and Linga et al reported ∼63% conversion in 48 h, which may differ in various sediments depending on the porosity, permeability, particle size, geochemistry, and so forth .…”
Section: Introductionmentioning
confidence: 99%
“…The stability of CO 2 hydrates at conditions mimicking deep oceanic sediments has been recently demonstrated in the laboratory, 96 and progress has been made in the quantification of the fundamental properties of CO 2 hydrate formation and morphology. 97 Although these studies, and upcoming field tests, are related to sequestration, a recent techno-economic analysis suggests that using hydrates for CO 2 capture could be attractive commercially.…”
Section: State Of the Art And Fundamental Challengesmentioning
confidence: 99%