The DOI matches its Crossref record; 28 of the 28 references it cites were found in a registry or an index.
Potential effects of gas hydrate on human welfare
Open accessAbstract
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.
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Cites
Clathrate Hydrates of Natural Gases
Sloan Jr., E. D., Koh, C. A., & Koh, C. A. (2007) · CRC Press eBooks · doi:10.1201/9781420008494 · Cited by 9,824
Biogeochemical aspects of atmospheric methane
Cicerone, R. J., & Oremland, R. S. (1988) · Global Biogeochemical Cycles · doi:10.1029/gb002i004p00299 · Cited by 1,559
Gas hydrates—geological perspective and global change
Kvenvolden, K. A. (1993) · Reviews of Geophysics · doi:10.1029/93rg00268 · Cited by 1,533
Self-citationDickens, G. R., O'Neil, J. R., Rea, D. K., & Owen, R. M. (1995) · Paleoceanography · doi:10.1029/95pa02087 · Cited by 1,433
Climate change—The IPCC scientific assessment
(1991) · Environment International · doi:10.1016/0160-4120(91)90291-w · Cited by 1,289
Methane hydrate — A major reservoir of carbon in the shallow geosphere?
Kvenvolden, K. A. (1988) · Chemical Geology · doi:10.1016/0009-2541(88)90104-0 · Cited by 1,174
Self-citationThe Origin and Distribution of Methane in Marine Sediments
Claypool, G. E., & Kaplan, I. R. (1974) · Natural Gases in Marine Sediments · doi:10.1007/978-1-4684-2757-8_8 · Cited by 1,034
Handbook of Natural Gas Engineering
Katz, D. L. (1959) · Cited by 778
AN ASSESSMENT OF WORLD HYDROCARBON RESOURCES
Rogner, H.-H. (1997) · Annual Review of Energy and the Environment · doi:10.1146/annurev.energy.22.1.217 · Cited by 709
Makogon, I. F. (1997) · Medical Entomology and Zoology · Cited by 693
Cited by
Dickens, G. R. (2003) · Earth and Planetary Science Letters · doi:10.1016/s0012-821x(03)00325-x · Cited by 429
Life Close to the Thermodynamic Limit: How Methanogenic Archaea Conserve Energy
Deppenmeier, U., & Müller, V. (2007) · Results and Problems in Cell Differentiation · doi:10.1007/400_2006_026 · Cited by 132
Metadata
- Authors
- Kvenvolden, K. A.
- Venue
- Proceedings of the National Academy of Sciences
- Published
- 1999-03-30
- Volume
- 96
- Issue
- 7
- Pages
- 3420-3426
- ISSN
- 0027-8424 (ISSN-L)
- 1091-6490
- OpenAlex
- W2022568776
- Cited by
- 555
- References
- 28
- FWCI
- 13.39
- Type
- journal article
- Language
- en
- Open access
- green
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