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      An Experimental Investigation on the Kinetics of Integrated Methane Recovery and CO 2 Sequestration by Injection of Flue Gas into Permafrost Methane Hydrate Reservoirs

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          Abstract

          Large hydrate reservoirs in the Arctic regions could provide great potentials for recovery of methane and geological storage of CO 2. In this study, injection of flue gas into permafrost gas hydrates reservoirs has been studied in order to evaluate its use in energy recovery and CO 2 sequestration based on the premise that it could significantly lower costs relative to other technologies available today. We have carried out a series of real-time scale experiments under realistic conditions at temperatures between 261.2 and 284.2 K and at optimum pressures defined in our previous work, in order to characterize the kinetics of the process and evaluate efficiency. Results show that the kinetics of methane release from methane hydrate and CO 2 extracted from flue gas strongly depend on hydrate reservoir temperatures. The experiment at 261.2 K yielded a capture of 81.9% CO 2 present in the injected flue gas, and an increase in the CH 4 concentration in the gas phase up to 60.7 mol%, 93.3 mol%, and 98.2 mol% at optimum pressures, after depressurizing the system to dissociate CH 4 hydrate and after depressurizing the system to CO 2 hydrate dissociation point, respectively. This is significantly better than the maximum efficiency reported in the literature for both CO 2 sequestration and methane recovery using flue gas injection, demonstrating the economic feasibility of direct injection flue gas into hydrate reservoirs in permafrost for methane recovery and geological capture and storage of CO 2. Finally, the thermal stability of stored CO 2 was investigated by heating the system and it is concluded that presence of N 2 in the injection gas provides another safety factor for the stored CO 2 in case of temperature change.

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          Fundamental principles and applications of natural gas hydrates.

          E Sloan (2003)
          Natural gas hydrates are solid, non-stoichiometric compounds of small gas molecules and water. They form when the constituents come into contact at low temperature and high pressure. The physical properties of these compounds, most notably that they are non-flowing crystalline solids that are denser than typical fluid hydrocarbons and that the gas molecules they contain are effectively compressed, give rise to numerous applications in the broad areas of energy and climate effects. In particular, they have an important bearing on flow assurance and safety issues in oil and gas pipelines, they offer a largely unexploited means of energy recovery and transportation, and they could play a significant role in past and future climate change.
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            Power plant post-combustion carbon dioxide capture: An opportunity for membranes

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              Permanent carbon dioxide storage in deep-sea sediments.

              Stabilizing the concentration of atmospheric CO(2) may require storing enormous quantities of captured anthropogenic CO(2) in near-permanent geologic reservoirs. Because of the subsurface temperature profile of terrestrial storage sites, CO(2) stored in these reservoirs is buoyant. As a result, a portion of the injected CO(2) can escape if the reservoir is not appropriately sealed. We show that injecting CO(2) into deep-sea sediments below [corrected] 3,000-m water depth and a few hundred meters of sediment provides permanent geologic storage even with large geomechanical perturbations. At the high pressures and low temperatures common in deep-sea sediments, CO(2) resides in its liquid phase and can be denser than the overlying pore fluid, causing the injected CO(2) to be gravitationally stable. Additionally, CO(2) hydrate formation will impede the flow of CO(2)(l) and serve as a second cap on the system. The evolution of the CO(2) plume is described qualitatively from the injection to the formation of CO(2) hydrates and finally to the dilution of the CO(2)(aq) solution by diffusion. If calcareous sediments are chosen, then the dissolution of carbonate host rock by the CO(2)(aq) solution will slightly increase porosity, which may cause large increases in permeability. Karst formation, however, is unlikely because total dissolution is limited to only a few percent of the rock volume. The total CO(2) storage capacity within the 200-mile economic zone of the U.S. coastline is enormous, capable of storing thousands of years of current U.S. CO(2) emissions.
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                Author and article information

                Contributors
                petjy@hw.ac.uk
                Journal
                Sci Rep
                Sci Rep
                Scientific Reports
                Nature Publishing Group UK (London )
                2045-2322
                7 November 2019
                7 November 2019
                2019
                : 9
                : 16206
                Affiliations
                [1 ]ISNI 0000000106567444, GRID grid.9531.e, Hydrates, Flow Assurance & Phase Equilibria Research Group, Institute of Petroleum Engineering, School of Energy, Geoscience, Infrastructure and Society, , Heriot-Watt University, ; Riccarton, Edinburgh EH14 4AS UK
                [2 ]ISNI 0000 0004 1936 7988, GRID grid.4305.2, School of Geosciences, , University of Edinburgh, Grant Institute, ; West Main Road, Edinburgh, EH9 3JW UK
                [3 ]ISNI 0000 0004 0555 3608, GRID grid.454320.4, Skolkovo Institute of Science and Technology (Skoltech), ; 3 Nobel Street, Skolkovo Innovation Center, 10, Moscow, 143026 Russia
                Article
                52745
                10.1038/s41598-019-52745-x
                6838119
                31700072
                9ac6c91d-4705-42f9-a8ab-e10dfedbe04f
                © The Author(s) 2019

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 14 May 2019
                : 22 October 2019
                Categories
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                © The Author(s) 2019

                Uncategorized
                climate-change mitigation,marine chemistry
                Uncategorized
                climate-change mitigation, marine chemistry

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