Experimental complex for studying the physical properties of artificially formed gas hydrate containing sediments
DOI:
https://doi.org/10.15407/dopovidi2022.05.051Keywords:
gas hydrates, marine sediments, methane, modeling, physical propertiesAbstract
The presence of gas hydrates in marine bottom sediments significantly changes their physical properties, so they can be detected by remote geophysical observations. Physical properties of gas hydrate-containing sediments (HCS) are extremely important information for detecting the presence of these compounds, estimating the amount of captured gas hydrates by sediments, as well as developing methods for using this resource. Currently, the study of physical properties concerned mainly artificial gas hydrates in the process of formation and decomposition under various thermodynamic conditions in their pure form. Therefore, very little is known about the physical properties of HCS, which makes their detection by remote geophysical surveys too difficult. Development and creation of experimental laboratory modular complex for formation and measurement of physical properties of artificial methane gas hydrates in various lithological-granulometric matrices (sandstones, argillites, siltstones, etc. ) will increase efficiency geophysical methods of their exploration and optimize of technology of methane hydrate deposits development.
Downloads
References
Makogon, Y. F. (2010). Natural gas hydrates — a promising source of energy. J. Nat. Gas Sci. Eng., 2, pp. 49-59. https://doi.org/10.1016/j. jngse.2009.12.004
Waite, W. F., Santamarina, J. C., Cortes, D. D., Dugan, B., Espinoza, D. N., Germaine, J., Jang, J., Jung, J. W., Kneafsey, T. J., Shin, H., Soga, K., Winters, W. J. & Yun, T. -S. (2009). Physical properties of hydrate-bearing sediments. Rev. Geophys., 47 (RG4003), pp. 1-38. https://doi.org/10.1029/2008RG000279
Stern, L. A., Kirby, S. H., Durham, W. B., Circone, S. & Waite, W. F. (2000). Laboratory synthesis of pure methane hydrate suitable for measurement of physical properties and decomposition behavior. In Max, M. D. (Ed. ). Natural gas hydrate, in oceanic and permafrost environments (pp. 323-348). Dordrecht: Springer. https://doi.org/10.1007/978-94-011-4387-5_25
Sloan, E. D., Koh, C. A. & Sum, A. K. (2010). Gas hydrate stability and sampling: The future as related to the phase diagram. Energies, 3, pp. 1991-2000. https://doi.org/10.3390/en3121991
Klar, A., Deerberg, G., Janicki, G., Schicks, J., Riedel, M., Fietzek, P., Mosch, T., Tinivella, U., De La Fuente Ruiz, M., Gatt, P., Schwalenberg, K., Heeschen, K., Bialas, J., Pinkert, S., Tang, A. M., Kvamme, B., Spangenberg, E., English, N., Bertrand, C., Parlaktuna, M., Sahoo, S. K., Bouillot, B., Desmedt, A. & Wallmann, K. (2019). Marine gas hydrate technology: state of the art and future possibilities for Europe, WG2 report, COST Action ES 1405. https://doi.org/10.3289/MIGRATE_WG2.2019
Kobolev, V. P., Mikhailyuk, S. F. & Safronov, A. M. (2021). Experimental laboratory complex for studying the physical properties of artificially formed gas-hydrate-containing sediments. Geology and mineral resources of World Ocean, 17, No. 3, pp. 22-33 (in Ukrainian). https://doi.org/10.15407/gpimo2021.03.022
Duchkov, A. D., Istomin, V. E. & Sokolova, L. S. (2012). A geothermal method for detecting gas hydrates in the bottom sediments of water basins. Russ. Geol. Geophys., 53 pp. 704-711.https://doi.org/10.1016/j.rgg.2012.05.009
Von Herzen, R. P. & Maxwell, A. E. (1959). The measurement of thermal conductivity of deep-sea sediments by a needle probe method. J. Geophysics. Res., 84, pp. 1629-1634. https://doi.org/10.1029/JZ064i010p01557
Blackwell, J. H. (1954). A transient-flow method for determination of thermal constants of insulating materials in bulk. J. App. Phys., 25, No. 2, pp. 137-144. https://doi.org/10.1063/1.17215921
Du Frane, W. L., Stern, L. A., Weitemeyer, K. A., Constable, S., Pinkston, J. C. & Roberts, J. J. (2011). Electrical properties of polycrystalline methane hydrate. Geophys. Res. Lett., 38, L09313. https://doi.org/10.1029/2011GL047243
Zillmer, M. (2006). A method for determining gas-hydrate and free-gas saturation of porous media from seismic measurements. Geophysics, 71, рр. N21-N32. https://doi.org/10.1190/1.2192910
Downloads
Published
How to Cite
Issue
Section
License
Copyright (c) 2022 Reports of the National Academy of Sciences of Ukraine
This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.