Thermal stability of CO2 hydrates in porous media with varying grain size in brine solution

Thermal stability of CO2 hydrates in porous media with varying grain size in brine solution

AMIRUN NISSA Rehman, CORNELIUS B. Bavoh, BHAJAN Lal

download PDF

Abstract. In the present work, the heat transfer behavior of CO2 hydrate dissociation was studied in three quartz sand particles (QS-1, QS-2 and QS-3) with varying grain sizes. The heat transfer behavior was evaluated by determining the heating rates of the porous media (quartz sand) during the CO2 hydrate dissociation process in 3.3 wt.% NaCl. The experiment was performed using sandstone hydrate reactor by first forming the CO2 hydrates at 4 MPa and 274.15 K and then dissociating the hydrates from 274.15 to 277.15 K, respectively. The results indicate that the thermal response of the porous sediment was significantly influenced by the hydrates as well as the porous sediment properties. The heating rate of the porous media increased when the grain size increased. However, the presence of CO2 hydrates reduced the heat transfer behavior of the porous sediment due to the endothermic nature of hydrate dissociation. The heating behavior of the porous media with hydrates mainly depends on the type and pattern of hydrate formed (pore-filling, load-bearing, and cementation) and the location of the hydrates within the pores of the porous sediment. The pore-filling type of hydrate formation in porous sediments provides high thermal stability for CO2 hydrate storage due to its less contact with the quartz sand particles. However, the pore-filling hydrate formation type is challenged with low or undesired CO2 hydrate storage capacity. These findings will provide meaningful insights to select favorable sediment properties/sites for CO2 storage in the hydrate form in porous sediments.

Keywords
CO2 Hydrates, Porous Media, Dissociation, Heat Transfer, Particle Size

Published online 5/20/2023, 11 pages
Copyright © 2023 by the author(s)
Published under license by Materials Research Forum LLC., Millersville PA, USA

Citation: AMIRUN NISSA Rehman, CORNELIUS B. Bavoh, BHAJAN Lal, Thermal stability of CO2 hydrates in porous media with varying grain size in brine solution, Materials Research Proceedings, Vol. 29, pp 98-108, 2023

DOI: https://doi.org/10.21741/9781644902516-13

The article was published as article 13 of the book Sustainable Processes and Clean Energy Transition

Content from this work may be used under the terms of the Creative Commons Attribution 3.0 license. Any further distribution of this work must maintain attribution to the author(s) and the title of the work, journal citation and DOI.

References
[1] R. P. Singh, K. S. Shekhawat, M. K. Das, and K. Muralidhar, “Geological sequestration of CO 2 in a water-bearing reservoir in hydrate-forming conditions,” Oil Gas Sci. Technol. – Rev. IFP Energies Nouv., vol. 75, no. 51, pp. 1–19, 2020.
[2] B. K. Sahu, P. Pati, and R. C. Panigrahy, “Impact of climate change on marine plankton with special reference to Indian seas,” Indian J. Geo-Marine Sci., vol. 47, no. 2, pp. 259–268, 2018.
[3] B. Lal and O. Nashed, Chemical Additives for Gas Hydrates. Cham: Springer International Publishing, 2020.
[4] A. Hosseini Zadeh, I. Kim, and S. Kim, “Experimental study on the characteristics of formation and dissociation of CO2hydrates in porous media,” in E3S Web of Conferences, 2020, vol. 205, https://doi.org/10.1051/e3sconf/202020502004
[5] D. D. Cortes, A. I. Martin, T. S. Yun, F. M. Francisca, J. C. Santamarina, and C. Ruppel, “Thermal conductivity of hydrate-bearing sediments,” J. Geophys. Res. Solid Earth, vol. 114, no. 11, pp. 1–10, 2009, https://doi.org/10.1029/2008JB006235
[6] S. H. B. Yang, P. Babu, S. F. S. Chua, and P. Linga, “Carbon dioxide hydrate kinetics in porous media with and without salts,” Appl. Energy, vol. 162, pp. 1131–1140, Jan. 2016, https://doi.org/10.1016/j.apenergy.2014.11.052
[7] J. Zhao et al., “Heat transfer analysis of methane hydrate sediment dissociation in a closed reactor by a thermal method,” Energies, vol. 5, no. 5, pp. 1292–1308, 2012, https://doi.org/10.3390/en5051292
[8] X. Y. Li, Y. Wang, X. Sen Li, Y. Zhang, and Z. Y. Chen, “Experimental study of methane hydrate dissociation in porous media with different thermal conductivities,” Int. J. Heat Mass Transf., vol. 144, p. 118528, 2019, https://doi.org/10.1016/j.ijheatmasstransfer.2019.118528
[9] J. Zhao, D. Liu, M. Yang, and Y. Song, “Analysis of heat transfer effects on gas production from methane hydrate by depressurization,” Int. J. Heat Mass Transf., vol. 77, pp. 529–541, 2014, https://doi.org/10.1016/j.ijheatmasstransfer.2014.05.034
[10] X. Guo et al., “Effect of thermal properties on the production behavior from water-saturated methane hydrate-bearing sediments using depressurization,” in Energy Procedia, 2019, vol. 158, no. 2018, pp. 5453–5458, https://doi.org/10.1016/j.egypro.2019.01.602
[11] Q. C. Wan, H. Si, B. Li, and G. Li, “Heat transfer analysis of methane hydrate dissociation by depressurization and thermal stimulation,” Int. J. Heat Mass Transf., vol. 127, pp. 206–217, 2018, https://doi.org/10.1016/j.ijheatmasstransfer.2018.07.016
[12] Z. Yin, G. Moridis, Z. R. Chong, H. K. Tan, and P. Linga, “Numerical Analysis of Experiments on Thermally Induced Dissociation of Methane Hydrates in Porous Media,” Ind. Eng. Chem. Res., vol. 57, no. 17, pp. 5776–5791, 2018, https://doi.org/10.1021/acs.iecr.7b03256
[13] X. Guo et al., “Analytical Investigation of Gas and Water Production from Aqueous-Rich Hydrate-Bearing Sediments by Depressurization,” Energy and Fuels, 2021, https://doi.org/10.1021/acs.energyfuels.0c04060
[14] M. Roostaie and Y. Leonenko, “Gas production from methane hydrates upon thermal stimulation; an analytical study employing radial coordinates,” Energy, vol. 194, p. 116815, 2020, https://doi.org/10.1016/j.energy.2019.116815
[15] Q. C. Wan, L. L. Chen, B. Li, K. Peng, and Y. Q. Wu, “Insights into the Control Mechanism of Heat Transfer on Methane Hydrate Dissociation via Depressurization and Wellbore Heating,” Ind. Eng. Chem. Res., vol. 59, no. 22, pp. 10651–10663, 2020, https://doi.org/10.1021/acs.iecr.0c00705
[16] E. Chuvilin and B. Bukhanov, “Thermal conductivity of frozen sediments containing self-preserved pore gas hydrates at atmospheric pressure: An experimental study,” Geosci., vol. 9, no. 2, 2019, https://doi.org/10.3390/geosciences9020065
[17] P. Wang and Y. Teng, “Numerical and Experimental Research on Gas Production from Methane Hydrate under Water–Excess Conditions,” Energy & Fuels, vol. 35, no. 6, pp. 4848–4857, 2021, https://doi.org/10.1021/acs.energyfuels.0c04106
[18] C. B. Bavoh, M. S. Khan, B. Lal, N. I. Bt Abdul Ghaniri, and K. M. Sabil, “New methane hydrate phase boundary data in the presence of aqueous amino acids,” Fluid Phase Equilib., vol. 478, pp. 129–133, 2018, https://doi.org/10.1016/j.fluid.2018.09.011
[19] C. B. Bavoh, O. Nashed, M. S. Khan, B. Partoon, B. Lal, and A. M. Sharif, “The impact of amino acids on methane hydrate phase boundary and formation kinetics,” J. Chem. Thermodyn., vol. 117, pp. 48–53, 2018, https://doi.org/10.1016/j.jct.2017.09.001
[20] K. M. Sabil, O. Nashed, B. Lal, L. Ismail, and A. Japper-Jaafar, “Experimental investigation on the dissociation conditions of methane hydrate in the presence of imidazolium-based ionic liquids,” J. Chem. Thermodyn., vol. 84, pp. 7–13, 2015, https://doi.org/10.1016/j.jct.2014.12.017
[21] M. Idress, M. Jasamai, I. M. Saaid, B. Lal, B. Partoon, and K. M. Sabil, “Effect of Porosity to Methane Hydrate Formation in Quartz Sand,” in ICIPEG 2016, 2017, pp. 231–240, https://doi.org/10.1007/978-981-10-3650-7_19
[22] C. B. Bavoh, B. Partoon, B. Lal, and L. Kok Keong, “Methane hydrate-liquid-vapour-equilibrium phase condition measurements in the presence of natural amino acids,” J. Nat. Gas Sci. Eng., vol. 37, pp. 425–434, 2017, https://doi.org/10.1016/j.jngse.2016.11.061
[23] Y. Song, J. Wang, Y. Liu, and J. Zhao, “Analysis of heat transfer influences on gas production from methane hydrates using a combined method,” Int. J. Heat Mass Transf., vol. 92, pp. 766–773, 2016, https://doi.org/10.1016/j.ijheatmasstransfer.2015.08.102.
[24] J. Ahn and J. Jung, “Effects of fine particles on thermal conductivity ofmixed silica sands,” Appl. Sci., vol. 7, no. 7, 2017, https://doi.org/10.3390/app7070650
[25] A. N. Rehman et al., “Kinetic insight on CO2 hydrate formation and dissociation in quartz sand in presence of brine,” Int. J. Greenh. Gas Control, vol. 114, no. February 2021, p. 103582, Feb. 2022, https://doi.org/10.1016/j.ijggc.2022.103582
[26] A. N. Rehman, R. Pendyala, and B. Lal, “Effect of brine on the kinetics of Carbon dioxide hydrate formation and dissociation in porous media,” Mater. Today Proc., vol. 47, pp. 1366–1370, 2021, https://doi.org/10.1016/j.matpr.2021.04.024
[27] G. T. Sudha, B. Stalin, and M. Ravichandran, “Optimization of powder metallurgy parameters to obtain low corrosion rate and high compressive strength in Al-MoO3 composites using SN ratio and ANOVA analysis,” Mater. Res. Express, vol. 6, no. 9, 2019, https://doi.org/10.1088/2053-1591/ab2cef
[28] M. Vasheghani Farahani et al., “Effect of thermal formation/dissociation cycles on the kinetics of formation and pore-scale distribution of methane hydrates in porous media: a magnetic resonance imaging study,” Sustain. Energy Fuels, vol. 5, no. 5, pp. 1567–1583, 2021, https://doi.org/10.1039/d0se01705a
[29] X.-Y. Li et al., “Influence of Particle Size on the Heat and Mass Transfer Characteristics of Methane Hydrate Formation and Decomposition in Porous Media,” Energy & Fuels, 2021, https://doi.org/10.1021/acs.energyfuels.0c03812
[30] S. Choi, J. Park, and Y. T. Kang, “Experimental investigation on CO2 hydrate formation/dissociation for cold thermal energy harvest and transportation applications,” Appl. Energy, vol. 242, no. March, pp. 1358–1368, 2019, https://doi.org/10.1016/j.apenergy.2019.03.141
[31] Y. Wang, J. C. Feng, X. Sen Li, Y. Zhang, and Z. Y. Chen, “Fluid flow mechanisms and heat transfer characteristics of gas recovery from gas-saturated and water-saturated hydrate reservoirs,” Int. J. Heat Mass Transf., vol. 118, pp. 1115–1127, 2018, https://doi.org/10.1016/j.ijheatmasstransfer.2017.11.081
[32] S. Liu, Y. Liang, B. Li, Q. Wan, and X. Han, “Interaction relationship analysis between heat transfer and hydrate decomposition for optimization exploitation,” Fuel, vol. 256, no. May, 2019, https://doi.org/10.1016/j.fuel.2019.115742
[33] Z. A. Jarrar, K. A. Alshibli, R. I. Al-Raoush, and J. Jung, “3D measurements of hydrate surface area during hydrate dissociation in porous media using dynamic 3D imaging,” Fuel, vol. 265, no. December 2019, p. 116978, 2020, https://doi.org/10.1016/j.fuel.2019.116978.
[34] W. F. Waite et al., “PHYSICAL PROPERTIES OF HYDRATE-BEARING SEDIMENTS,” no. 2008, pp. 1–38, 2009, https://doi.org/10.1029/2008RG000279.Table.
[35] L. Zhan, Y. Wang, and X.-S. Li, “Experimental study on characteristics of methane hydrate formation and dissociation in porous medium with different particle sizes using depressurization,” Fuel, vol. 230, no. May, pp. 37–44, Oct. 2018, https://doi.org/10.1016/j.fuel.2018.05.008
[36] M. Muraoka, M. Ohtake, N. Susuki, H. Morita, M. Oshima, and Y. Yamamoto, “Thermal properties of highly saturated methane hydrate-bearing sediments recovered from the Krishna–Godavari Basin,” Mar. Pet. Geol., vol. 108, no. October 2018, pp. 321–331, 2019, https://doi.org/10.1016/j.marpetgeo.2018.10.037
[37] P. Guo, Y. K. Pan, L. L. Li, and B. Tang, “Molecular dynamics simulation of decomposition and thermal conductivity of methane hydrate in porous media,” Chinese Phys. B, vol. 26, no. 7, 2017, https://doi.org/10.1088/1674-1056/26/7/073101