Peer-reviewed articles 17,970 +



Title: PHASE BOUNDARY EQUILIBRIUM CONDITIONS FOR CH4, C2H6 AND C3H8 IN MARINE QUARTZ-BASED POROUS SAND: THERMODYNAMIC EVOLUTION OF THE SYSTEM AND DEVIATION FROM THE IDEAL TREND

PHASE BOUNDARY EQUILIBRIUM CONDITIONS FOR CH4, C2H6 AND C3H8 IN MARINE QUARTZ-BASED POROUS SAND: THERMODYNAMIC EVOLUTION OF THE SYSTEM AND DEVIATION FROM THE IDEAL TREND
Alberto Maria Gambelli; Jessica Di Mario; Giovanni Gigliotti
10.5593/sgem2024v/3.2
1314-2704
English
24
3.2
•    Prof. DSc. Oleksandr Trofymchuk, UKRAINE •    Prof. Dr. hab. oec. Baiba Rivza, LATVIA
Natural gas hydrate reservoirs often consist of a mixture of various gaseous species: small-chain hydrocarbons, as methane, ethane, propane and butane, and other species, as carbon dioxide, nitrogen, oxygen, hydrogen sulfide and others. Every species shows different forming conditions. Moreover, those conditions may change as a function of the mixture composition and the properties of the surrounding environment. The present study deals the production of hydrates with small-chain hydrocarbons, within a silica-based porous marine sediment. Hydrates were formed and melted, the experimental phase boundary equilibrium conditions were then compared with the ideal ones, obtained from literature. Such a comparison allowed to characterize how the sediment acted during the process. In presence of methane and ethane, It was found capable to promote the process, while It acted as inhibitor for propane hydrates. The difference observed between the various species, were finally explained in terms of typology of hydrate structure formed and molecular diameter of the guest species.
[1] Sloan E.D., Koh C.A., Clathrate hydrates of natural gases, 3rd Ed, CRC Press, 2008.
[2] Ndlovu P., Babaee S., Naidoo P., Experimental study of CH4-CO2 replacement in gas hydrates in the presence of nitrogen and graphene nanoparticles. J. Mol. Liq. 371, 121109, 2023.
[3] Yan P., Luan H., Jiang Y., Liang W., Liu M., Chen H., Influence of depressurization mode on natural gas hydrate production characteristics: One-dimensional experimental study. Geoen. Sci. Eng. 234, 212671, 2024.
[4] Giovannetti R., Gambelli A.M., Castellani B., Rossi A., Minicucci M., Zannotti M., Li Y., Rossi F., May sediments affect the inhibiting properties of NaCl on CH4 and CO2 hydrates formation? An experimental report. J. Mol. Liq. 359 119300, 2022.
[5] Sun Y., Li B., Guo W., Lu X., Zhang Y., Li K., Wang P., Jin G., Ji R., Qu L., Comparative analysis of the production trial and numerical simulations of gas production from multiplayer hydrate deposits in the Qilian Mountain Permafrost. J. Nat. Gas Sci. Eng. 21, 456 – 466, 2014.
[6] Li X.S., Xu C.G., Zhang Y., Ruan X.K., Li G., Wang Y., Investigation into gas production from natural gas hydrate: a review. Appl. Energy 172, 286 – 322, 2016.
[7] Moridis G.J., Sloan E.D., Gas production potential of disperse low-saturation hydrate accumulation in oceanic sediments. Energy Convers. Manag. 48, 1834 – 1849, 2007.
[8] Ohmura R., Uchida T., Takeya S., Nagao J., Minagawa H., Ebinuma T., Narita H., Clathrate hydrate formation in (methane+water+methylcyclohexanone) systems: the first phase equilibrium data. J. Chem Thermodyn. 35, 2045 – 2054, 2003.
[9] Semenov A.P., Medvedev V.I., Guschin P.A., Yakushev V., Effect of heating rate on the accuracy of measuring equilibrium conditions for methane and argon hydrates. Chem. Eng. Sci. 137, 161 – 169, 2015.
[10] Sundramoorthy J.D., Hammonds P., Lal B., Philips G., Gas hydrate equilibrium measurement and observation of gas hydrate dissociation with/without a KHI. Procedia Eng. 148, 870 – 877, 2016.
[11] Li Y., Gambelli A.M., Chen J., Yin Z., Rossi F., Tronconi E., Mei S., Experimental study on the competition between carbon dioxide hydrate and ice below the freezing point. Chem. Eng. Sci. 268, 118426, 2023.
[12] Kaschiev D., Verdoes D., van Rosmalen G.M., Induction time and metastability limit in new phase formation. J. Cryst. Growth 110, 373 – 380, 1991.
[13] Englezos P., Kalogerakis N., Dholabai P.D., Bishnoi P.R., Kinetics of formation of methane and ethane gas hydrate. Chem. Eng. Sci. 42, 2647 – 2658, 1987.
[14] Winters J.W., Waite W.F., Mason D.H., Gilbert L.Y., Pecher I.A., Methane gas hydrate effect on sediments acoustic and strength properties. J. Pet. Sci. Eng. 56, 127 – 135, 2017.
[15] Oshima M., Suzuki K., Yoneda J., Kato A., Kida M., Konno Y., Muraoka M., Jin Y., Nagao J., Tenma N. Lithological properties of natural gas hydrate-bearing sediments in pressure-cores recovered from the Krishna-Godavari Basin. Mar. Pet. Geol. 108, 439 – 470, 2019.
[16] Gambelli A.M., Rossi F., Experimental characterization of the difference in induction period between CH4 and CO2 hydrates: Motivations and possible consequences on the replacement process. J. Nat. Gas Sci. Eng. 108, 104848, 2022.
[17] Bavoh C.B., Partoon B., Lal B., Keong L.K., Methane hydrate-liquid-vapor-equilibrium phase condition measurements in the presence of natural amino acids. J. Nat. Gas Sci. Eng. 37, 425 – 434, 2017.
[18] Subramanian S., Kini R.A., Dec S.F., Sloan E.D., Evidence of structure II hydrate formation from methane + ethane mixtures. Chem. Eng. Sci. 55, 1981 – 1999, 2000.
[19] Moojer-van der Heuvel M.M., Peters C.J., Aron J.S., Gas hydrate phase equilibria for propane in the presence of additive components. Fluid Phase Equilibr. 193, 245 – 249, 2002.

The authors would acknowledge the Department of Civil and Environmental Engineering of the University of Perugia.
conference
Proceedings of 24th International Multidisciplinary Scientific GeoConference SGEM 2024
24th International Multidisciplinary Scientific GeoConference SGEM 2024, 27 - 30 November, 2024
Proceedings Paper
STEF92 Technology
International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM
SWS Scholarly Society; Acad Sci Czech Republ; Latvian Acad Sci; Polish Acad Sci; Russian Acad Sci; Serbian Acad Sci and Arts; Natl Acad Sci Ukraine; Natl Acad Sci Armenia; Sci Council Japan; European Acad Sci, Arts and Letters; Acad Fine Arts Zagreb Croatia; Croatian Acad Sci and Arts; Acad Sci Moldova; Montenegrin Acad Sci and Arts; Georgian Acad Sci; Acad Fine Arts and Design Bratislava; Russian Acad Arts; Turkish Acad Sci.
367-374
27 - 30 November, 2024
website
10089
natural gas hydrates; phase boundary equilibrium conditions; marine porous sediments; cage occupancy; small-chain hydrocarbons.

25th SGEM International Conference on Earth & Planetary Sciences


International GeoConference SGEM2025
27 June - 6 July, 2025 / Albena, Bulgaria

Read More
   

SGEM Vienna GREEN "Green Science for Green Life"


Extended Scientific Sessions SGEM Vienna GREEN
3 -6 December, 2025 / Vienna, Austria

Read More
   

A scientific platform for Art-Inspired Scientists!


The Magical World Where Science meets Art
Vienna, Austria

Read More