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Interplay Between Gas Hydrates and Submarine Slope Failure

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Submarine Mass Movements and Their Consequences

Part of the book series: Advances in Natural and Technological Hazards Research ((NTHR,volume 28))

Abstract

Interest in methane gas production from hydrate deposits has increased dramatically in the last decade. Gas hydrates are solid crystalline compounds that encage gas molecules inside a water molecule lattice. Gas hydrates are linked to large submarine slides, in part because hydrate dissociation results in loss of solid material, production of free gas, and increased fluid pressures; all which have the effect of reducing sediment strength. Laboratory experiments, small scale physical modeling, and theoretical slope stability analyses indicate that dissociation of even a small amount of hydrate can cause significant loss of sediment strength. Hydrate dissociation could be critical in inciting slope failures for low permeability sediments in shallower water depths. This paper presents recent results and advances on the intersection of gas hydrates and submarine slope stability, exploring the role of gas hydrates in triggering and/or propagating submarine mass movements.

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References

  • Ahlbrandt TW (2002) Future petroleum energy resources of the world. Int Geol Rev 44:1092–1104.

    Article  Google Scholar 

  • Booth JS, Winters WJ, Dillon WP (1994) Circumstantial evidence of gas hydrate and slope failure associations on the United States Atlantic continental margin. Natural Gas Hydrates. Annal New York Acad Sci 715:487–489.

    Article  Google Scholar 

  • Bouriak S, Vanneste M, Saoutkine A (2000) Inferred gas hydrates and clay diapirs near the Storegga Slide on the southern edge of the Vøring Plateau, offshore Norway. Mar Geol 163:125–148.

    Article  Google Scholar 

  • Bryant WR, Hottman W, Trabant P (1975) Permeability of unconsolidated and consolidated marine sediments, Gulf of Mexico. Mar Geores Geotech 1:1–14.

    Article  Google Scholar 

  • Bryn P, Berg K, Forsberg CF, Solheim A, Kvalstad TJ (2005) Explaining the Storegga slide. Mar Pet Geol 22:11–19.

    Article  Google Scholar 

  • Collett TS (2002) Energy resource potential of natural gas hydrates. Am Assoc Pet Geol Bull 86:1971–1992.

    Google Scholar 

  • Collett TS, Riedel M, Boswell R, Cochran JR, Kumar P, Sethi AK, Sathe AV, NGHP Expedition-01 Scientific Party (2006) International team completes landmark gas hydrate expedition in the offshore of India. Fire in the Ice, Methane hydrate newsletter, U.S. Department of Energy, Office of Fossil Energy, National Energy Technology Laboratory, Fall, pp. 1–4.

    Google Scholar 

  • Council of Canadian Academies (CCA) (2008) Energy from gas hydrates: Assessing the opportunities and challenges for Canada. Report of the Expert Panel on Gas Hydrates, J Grace (Chair).

    Google Scholar 

  • Durham WB, Stern LA, Kirby SH (2003) Ductile flow of methane hydrate. Can J Phys 81:373–380.

    Article  Google Scholar 

  • Dvorkin J, Prasad M, Sakai A, Lavoie D (1999) Elasticity of marine sediments; Rock physics modeling. Geophys Res Let 26:1781–1784.

    Article  Google Scholar 

  • Ebinuma T, Kamata Y, Minagawa H, Ohmura R, Nagao J, Narita H (2005) Mechanical properties of sandy sediments containing methane hydrate. 5th International Conference on Gas Hydrates, 12–16 June, Trondheim, Norway.

    Google Scholar 

  • Fyke JG, Weaver AJ (2006) The effect of potential future climate change on the marine methane hydrate stability zone. J Clim 19:5903–5917.

    Article  Google Scholar 

  • Gidley ID (2008) Gas hydrate dissociation structures in clay slopes. M.Sc. Thesis, University of Calgary, Calgary, Canada.

    Google Scholar 

  • Gidley ID, Grozic JLH (2008) Gas hydrate dissociation structures in submarine slopes. 4th Canadian Conference on Geohazards: From Causes to Management, 20–24 May, Laval, Canada, pp. 81–88.

    Google Scholar 

  • Grantz A, Dinter DA (1980) Constraints of geologic processes on western Beaufort Sea oil developments. Oil Gas J 78:304–319.

    Google Scholar 

  • Grozic JLH, Kvalstad TJ (2007) Laboratory verification of gas hydrate-sediment response. XIII Pan-American Conference on Soil Mechanics and Geotechnical Engineering, 16–20 July, Margarita, Venezuela.

    Google Scholar 

  • Hatzikiriakos SG, Englezos P (1993) The relationship between global warming and methane gas hydrates in the earth. Chem Eng Sci 48:3963–3969.

    Article  Google Scholar 

  • Helgerud M, Waite WF, Kirby SH, Nur A (2009) Elastic wave speeds and moduli in polycrystal-line ice Ih, sI methane hydrate, and sII methane-ethane hydrate. J Geophys Res 114:B02212, doi:10.1029/2008JB006132.

    Article  Google Scholar 

  • Hovland M, Gudmestad OT (2001) Potential influence of gas hydrates on seabed installations. In: Paull CK and Dillon WP (eds.). Natural Gas Hydrates. Washington, DC: American Geophysical Union, Geophysical Monograph Series, 124, pp. 300–309.

    Google Scholar 

  • Jayasinghe AG, Grozic JLH (2007) An experimental investigation of temperature induced dissociation of methane hydrate in porous media. 60th Canadian Geotechnical Conference, 21–24 October, Ottawa, Canada, pp. 2062–2067.

    Google Scholar 

  • Jung W Y, Vogt PR (2004) Effects of bottom water warming and sea level rise on Holocene hydrate dissociation and mass wasting along the Norwegian-Barents Continental Margin. J Geophys Res 109:B06104, 18 pp.

    Article  Google Scholar 

  • Kayen RE, Lee HJ (1991) Pleistocene slope instability of gas hydrate-laden sediment on the Beaufort Sea margin. Mar Geotech 10:125–141.

    Article  Google Scholar 

  • Kvenvolden KA (1988) Methane hydrate — A major reservoir of carbon in the shallow geosphere? Chem Geol 71:41–51.

    Article  Google Scholar 

  • Kvenvolden KA (1993) Gas hydrates — Geological perspective and global climate change. Rev Geophys 31:173–187.

    Article  Google Scholar 

  • Kvenvolden KA (1999) Potential effects of gas hydrate on human welfare. Proc Natl Acad Sci USA 96:3420–3426.

    Article  Google Scholar 

  • Kvenvolden KA (2000) Natural gas hydrate: Introduction and history of discovery. In: Max MD (ed.). Natural Gas Hydrate in Oceanic and Permafrost Environments. The Netherlands: Kluwer Academic, pp. 9–16.

    Google Scholar 

  • Kvenvolden KA (2002) Methane hydrate in the global organic carbon cycle. Terra Nova 14:302–306.

    Article  Google Scholar 

  • Kvenvolden KA, Rogers BW (2005) Gaia's breath-global methane exhalations. Mar Pet Geol 22:79–590.

    Article  Google Scholar 

  • Kwon T H, Cho GC, Santamarina JC (2008) Gas hydrate dissociation in sediments: Pressure-temperature evolution. Geochem Geophys Geosys 9:Q03019, doi:10.1029/2007GC001920, 14 p.

    Article  Google Scholar 

  • Lee HJ (2009) Timing of occurrence of large submarine landslides on the Atlantic Ocean margin. Mar Geol 264:53–64.

    Article  Google Scholar 

  • Leynaud D, Mienert J, Vanneste M (2009) Submarine mass movements on glaciated and non-glaciated European continental margins: A review of triggering mechanisms and preconditions to failure. 26:618–632.

    Google Scholar 

  • Locat J, Lee HJ (2002) Submarine landslides: Advances and challenges. Can Geotech J 39:193–212.

    Article  Google Scholar 

  • Makogon YF (1997) Hydrates of Hydrocarbons. Tulsa, OK: Penn Well Publishing.

    Google Scholar 

  • Makogon YF, Holditch SA (2001) Lab work clarifies gas hydrate formation, dissociation. Oil Gas J 99:47–52.

    Google Scholar 

  • Maslin M, Owen M, Day S, Long D (2004) Linking continental-slope failures and climate change: testing the clathrate gun hypothesis. Geology 32:53–56.

    Article  Google Scholar 

  • Masui A, Haneda H, Ogata Y, Aoki K (2005) The effect of saturation degree of methane hydrate on the shear strength of synthetic methane hydrate sediments. 5th International Conference on Gas Hydrates, 12–16 June, Trondheim, Norway.

    Google Scholar 

  • Masui A, Miyazaki K, Haneda H, Ogata Y, Aoki K (2008) Mechanical characteristics of natural and artificial gas hydrate bearing sediments. 6th International Conference on Gas Hydrates, 6–10 July, Vancouver, Canada.

    Google Scholar 

  • Max M, Dillon W (2000) Natural gas hydrate: A frozen asset? Chem Ind 10:16–18.

    Google Scholar 

  • McIver RD (1982) Role of naturally occurring gas hydrates in sediment transport. Am Assoc Pet Geol Bull 66:789–792.

    Google Scholar 

  • Mienert J, Berndt C, Laberg JS, Vorren TO (2002) Slope instability of continental margins. In: Wefer G, Billett D, Hebbeln D, Jørgensen BB., Schluter M, VanWeering T. (eds.). Ocean Margin Systems. Heidelberg: Springer, pp. 179–193.

    Google Scholar 

  • Mienert J, Vanneste M, Bunz, S, Andreassen K, Haflidason H, Sejrup HP (2005) Ocean warming and gas hydrate stability on the mid-Norwegian margin at the Storegga Slide. Mar Pet Geol 22:233–244.

    Article  Google Scholar 

  • Milkov AV, Claypool GE, Lee Y-J, Xu W, Dickens GR, Borowski WS, The Ocean Drilling Program Leg 204 Scientific Party (2003) In situ methane concentrations at Hydrate Ridge, offshore Oregon: New constrains on the global gas hydrate inventory from active margins. Geology 31:833–836.

    Google Scholar 

  • Nimblett JN, Shipp RC, Strijbos F (2005) Gas hydrate as a drilling hazard: Examples from global deepwater settings. Offshore Technology Conference, Houston, Texas, OTC Paper 17476.

    Google Scholar 

  • Nixon MF (2005) Influence of gas hydrates on submarine slope stability. M.Sc. Thesis, Department of Civil Engineering, University of Calgary, Calgary, AB.

    Google Scholar 

  • Nixon MF, Grozic JLH (2006) A simple model for submarine slope stability analysis with gas hydrates. Nor J Geol 86:309–316.

    Google Scholar 

  • Nixon MF, Grozic JLH (2007) Submarine slope failure due to gas hydrate dissociation: A preliminary quantification. Can Geotech J 44:314–325.

    Article  Google Scholar 

  • Park KP, Bahk JJ, Kwon Y, Kim GY, Riedel M, Hollsand M, Schultheiss P, Rose K, The UBGH-1 Scientific Party (2008) Korean National Program Expedition confirms rich gas hydrate deposit in the Ulleung Basin, East Sea. Fire in the Ice, Methane hydrate newsletter, U.S. Department of Energy, Office of Fossil Energy, National Energy Technology Laboratory, Spring, pp. 6–9.

    Google Scholar 

  • Paull CK, Buelow WJ, Ussler III W, Borowski WS (1996) Increased continental margin slumping frequency during sea-level lowstands above gas hydrate-bearing sediments. Geology 24:143–146.

    Article  Google Scholar 

  • Paull CK, Ussler III W, Dillon WP (2000) Potential role of gas hydrate decomposition in generation submarine slope failures. In: Max M (ed.). Natural Gas Hydrate in Marine and Permafrost Environments. Dordrecht: Kluwer Academic, pp. 149–156.

    Google Scholar 

  • Pentland W (2008) Methane hydrates: Energy's most dangerous game. Forbes Magazine, www.forbes.com, 2 September 2008. Reprinted by www.cbc.ca, 14 October 2008.

  • Piper DJW, Pirmez C, Manley PL, Long D, Flood RD, Normark WR, Showers W (1997) Mass-transport deposits of the Amazon Fan. In: Flood RD, Piper DJW, Klaus A, Peterson (eds.). Proceedings of the Ocean Drilling Program. Scientific Results, 155, pp. 109–146.

    Google Scholar 

  • Popenoe P, Schmuck EA, Dillon WP (1993) The Cape Fear landslide: slope failure associated with salt diapirism and gas hydrate decomposition. In: Schwab WC, Lee HJ, Twichell DC (eds.). Submarine Landslides: Selected Studies in the U.S. EEZ: USGS Bulletin 2002, pp. 40–53.

    Google Scholar 

  • Puzrin AM, Germanovich LN (2005) The growth of shear bands in the catastrophic failure of soils. Proc R Soc Math Phys Eng Sci 461:1199–1228.

    Article  Google Scholar 

  • Riedel M, Collett TS, Malone MJ and the Expedition 311 Scientists (2006) Proceedings of the Integrated Ocean Drilling Program. Washington, DC: Integrated Ocean Drilling Program.

    Google Scholar 

  • Ruppel C, Driscoll N, Jones E, Collett T (2008) Initial science results of the March 2005 Gas Hydrate Field Program. U.S. DOE/Chevron Gulf of Mexico Joint Industry Projects. Mar Pet Geol 25:819–829.

    Article  Google Scholar 

  • Schmuck EA, Paull CK (1993) Evidence for gas accumulation associated with diapirism and gas hydrates at the head of the Cape Fear Slide. Geo-Mar Let 13:145–152.

    Article  Google Scholar 

  • Sultan N (2007) Comment on “Excess pore pressure resulting from methane hydrate dissociation in marine sediments: A theoretical approach” by Wenyue Xu and Leonid N. Germanovich. J Geophys Res 112:B02103, doi:10.1029/2006JB004527.

    Article  Google Scholar 

  • Sultan N, Cochonat P, Foucher JP, Mienert J (2004) Effect of gas hydrate melting on seafloor slope stability. Mar Geol 231:379–401.

    Article  Google Scholar 

  • Tréhu AM, Bohrmann G, Rack FR, Torres ME, et al. (2003) Proceedings of the Ocean Drilling Program Initial Reports, Volume 204.

    Google Scholar 

  • Vogt P V, Jung WY (2002) Holocene mass wasting on upper non-Polar continental slopes due to post-Glacial ocean warming and hydrate dissociation? Geophys Res Let 29:55-1–55-4.

    Article  Google Scholar 

  • Waite WF, Osegovic JP, Winters WJ, Max MD, Mason DH (2008) Seeding hydrate formation in water-saturated sand with dissolved-phase methane obtained from hydrate dissolution: A progress report. 6th International Conference on Gas Hydrates, 6–10 July, Vancouver, Canada, 9 p.

    Google Scholar 

  • Waite WF, Santamarina JC, Cortes DD, Dugan B, Espinoza DN, Germaine J, Jang J, Jung J, Kneafsey T, Shin HS, Soga K, Winters W, Yun TS (2009) Physical properties of hydrate bearing sediments. Rev Geophys, In Review.

    Google Scholar 

  • Winters WJ, Pecher IA, Waite WF, Mason DH (2004) Physical properties and rock physics models of sediment containing natural and laboratory-formed methane gas hydrate. Am Mineral 89:1221–1227.

    Google Scholar 

  • Wu L, Grozic JLH (2008) Laboratory analysis of carbon dioxide hydrate-bearing sands. ASCE J Geotech Geoenviron Eng 134:547–550.

    Article  Google Scholar 

  • Xu W, Germanovich LN (2006) Excess pore pressure resulting from methane hydrate dissociation in marine sediments: A theoretical approach. J Geophys Res 111:B01104, doi:10.1029/2004JB003600.

    Article  Google Scholar 

  • Zhang H, Yang S, Wu N, Su X, Holland M, Schultheiss P, Rose K, Butler H, Humphrey G, GMGS-1 Science Team (2007) Successful and surprising results for China's first gas hydrate drilling expedition. Fire in the Ice, Methane hydrate newsletter, U.S. Department of Energy, Office of Fossil Energy, National Energy Technology Laboratory, Fall, pp. 6–9.

    Google Scholar 

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Acknowledgments

The author gratefully acknowledges Natural Sciences and Engineering Research Council of Canada for funding this project. I also thank the reviewers Drs. N. Sultan and W. Waite for their critique and valuable input into this manuscript.

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Grozic, J.L.H. (2010). Interplay Between Gas Hydrates and Submarine Slope Failure. In: Mosher, D.C., et al. Submarine Mass Movements and Their Consequences. Advances in Natural and Technological Hazards Research, vol 28. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-3071-9_2

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