Potential effects of gas hydrate on human welfare.

For almost 30 years. serious interest has been directed toward natural gas hydrate, a crystalline solid composed of water and methane, as a potential (i) energy resource, (ii) factor in global climate change, and (iii) submarine geohazard. Although each of these issues can affect human welfare, only (iii) is considered to be of immediate importance. Assessments of gas hydrate as an energy resource have often been overly optimistic, based in part on its very high methane content and on its worldwide occurrence in continental margins. Although these attributes are attractive, geologic settings, reservoir properties, and phase-equilibria considerations diminish the energy resource potential of natural gas hydrate. The possible role of gas hydrate in global climate change has been often overstated. Although methane is a "greenhouse" gas in the atmosphere, much methane from dissociated gas hydrate may never reach the atmosphere, but rather may be converted to carbon dioxide and sequestered by the hydrosphere/biosphere before reaching the atmosphere. Thus, methane from gas hydrate may have little opportunity to affect global climate change. However, submarine geohazards (such as sediment instabilities and slope failures on local and regional scales, leading to debris flows, slumps, slides, and possible tsunamis) caused by gas-hydrate dissociation are of immediate and increasing importance as humankind moves to exploit seabed resources in ever-deepening waters of coastal oceans. The vulnerability of gas hydrate to temperature and sea level changes enhances the instability of deep-water oceanic sediments, and thus human activities and installations in this setting can be affected.

[1]  R. F. Meyer,et al.  Long-term energy resources , 1981 .

[2]  J. Chappellaz,et al.  Variations in atmospheric methane concentration during the Holocene epoch , 1995, Nature.

[3]  K. Kvenvolden,et al.  Natural Gas Hydrate Occurrence and Issues , 1994 .

[4]  G. MacDonald Role of methane clathrates in past and future climates , 1990 .

[5]  Gerald D. Holder,et al.  The Potential of Natural Gas Hydrates as an Energy Resource , 1984 .

[6]  P. M. Lang,et al.  Slowing down of the global accumulation of atmospheric methane during the 1980s , 1992, Nature.

[7]  Isaac R. Kaplan,et al.  Natural Gases in Marine Sediments , 1974, Marine Science.

[8]  R. Cicerone,et al.  Biogeochemical aspects of atmospheric methane , 1988 .

[9]  E. Hammerschmidt Formation of Gas Hydrates in Natural Gas Transmission Lines , 1934 .

[10]  L. Harvey,et al.  Evaluation of the potential impact of methane clathrate destabilization on future global warming , 1995 .

[11]  A. J. Crawford,et al.  The global distribution of methane in the troposphere , 1987 .

[12]  H. Sejrup,et al.  Large submarine slides on the Norwegian continental margin: Sediments, transport and timing , 1987 .

[13]  E. Nisbet The end of the ice age , 1990 .

[14]  G. Dickens,et al.  A blast of gas in the latest Paleocene: simulating first-order effects of massive dissociation of oceanic methane hydrate. , 1997, Geology.

[15]  R. McIver Role of Naturally Occurring Gas Hydrates in Sediment Transport , 1982 .

[16]  C. Lorius,et al.  Ice-core record of atmospheric methane over the past 160,000 years , 1990, Nature.

[17]  G. MacDonald The Future of Methane as an Energy Resource , 1990 .

[18]  R. M. Owen,et al.  Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene , 1995 .

[19]  Carolyn A. Koh,et al.  Clathrate hydrates of natural gases , 1990 .

[20]  K. Kvenvolden Methane hydrate — A major reservoir of carbon in the shallow geosphere? , 1988 .

[21]  C. Summerhayes,et al.  Surficial slides and slumps on the continental slope and rise of South West Africa: A reconnaissance study , 1979 .

[22]  J. Brooks,et al.  Gas hydrate that breaches the sea floor on the continental slope of the Gulf of Mexico , 1994 .

[23]  K. Kvenvolden Methane hydrates and global climate , 1988 .

[24]  A. I. Levorsen Geology of Petroleum , 2001 .

[25]  Vello A. Kuuskraa,et al.  Hydrates contain vast store of world gas resources , 1998 .

[26]  R. Kayen,et al.  Pleistocene slope instability of gas hydrate‐laden sediment on the Beaufort sea margin , 1991 .

[27]  Thomas H. Shipley,et al.  Seismic Evidence for Widespread Possible Gas Hydrate Horizons on Continental Slopes and Rises , 1979 .

[28]  H. Rogner AN ASSESSMENT OF WORLD HYDROCARBON RESOURCES , 1997 .

[29]  M. Lilley,et al.  The Beaufort Sea continental shelf as a seasonal source of atmospheric methane , 1993 .

[30]  Jürgen Mienert,et al.  Gas hydrates: relevance to world margin stability and climate change , 1998 .

[31]  G. Brasseur,et al.  Stratospheric Response to Trace Gas Perturbations: Changes in Ozone and Temperature Distributions , 1988, Science.

[32]  Warren T. Wood,et al.  Methane Hydrate and Free Gas on the Blake Ridge from Vertical Seismic Profiling , 1996, Science.

[33]  Gerald R. Dickens,et al.  Direct measurement of in situ methane quantities in a large gas-hydrate reservoir , 1997, Nature.

[34]  W. Dillon,et al.  Is the extent of glaciation limited by marine gas-hydrates , 1991 .

[35]  K. Kvenvolden Gas hydrates—geological perspective and global change , 1993 .

[36]  Robert D. Stoll,et al.  Anomalous wave velocities in sediments containing gas hydrates , 1971 .

[37]  I. Fung,et al.  Potential distribution of methane hydrates in the world's oceans , 1994 .