Articles

THE STUDY OF GAS HYDRATES AND ITS RELATION WITH GLOBAL CHANGES

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  • South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou 510301

Received date: 1996-05-06

  Revised date: 1996-06-25

  Online published: 1997-02-01

Abstract

Gas hydrates contains a large quantity of organic carbon which exceeds the total organic carbon from other sources. It is an important carbon reservoir in shallow geosphere. A slight variation of temperature/pressure would cause the formation/decomposition of gas hydrates,and subsequent consumption/release of methane. This exerts significant influence on global carbon cycle and greenhouse effect. The Polar regions differ from the mediate low latitudes on the feedback of gas hydrates to global climate change and galcial/interglacial alternation. Even in mediate low latitudes there exist two processes of opposite directions. The total effect of gas hydrates on global changes needs to be estimated in further researches. In China seas, there exist T P conditions suitable for the occurrence of gas hydrates. The BSR as an indication of gas hydrates has been reported in southern South China Sea. The total reserves of gas hydrates and their feedback to sea level changes in China seas may be assessed based on careful re interpretation of seismic profiles and computer simulations. This may provide an example for the marginal seas.

Cite this article

CHEN Hanzong, ZHOU Di . THE STUDY OF GAS HYDRATES AND ITS RELATION WITH GLOBAL CHANGES[J]. Advances in Earth Science, 1997 , 12(1) : 37 -42 . DOI: 10.11867/j.issn.1001-8166.1997.01.0037

References

1 Katz D L, Cornell D, Kobayashi R, et al. Handbook of Natural Gas Engineering. New York: McGraw-Hill, 1959.802.
2 Kvenvolden K A, Cooper A K. Natural gas hydrates of the offshore circum-Pacificmargin—a future energy resource?In: Trans 4th Circum-Pacific Energy and Mineral Resources Conference (Horn M K ed.). Circum-Pacific Council for Energy and Resources, 1987.285-297.
3 Kvenvolden K A. Gas hydrates-geological perspective and global change. Rev Geophys,1993,31(2) : 173-187.
4 Collett T S. Potential of gas hydrates outlined. Oil Gas J, 1992, 78(1), 124-130.
5 Kvenvolden K A, Ginsburg G D, Solovyev V A. Worldwide distribution of subaquatic gas hydrates. Geo Mar Lett,1993, 13: 32-40.
6 Potential Gas Committee. Potential supply of natural gas in the United States(as of December 31, 1980). Potential Gas Agency, Colorado School of Mines, Golden, 1981.119.
7 Kvenvolden K A. Methane hydrates—a major reservoir of carbon in shallow geosphere.Chem Geol, 1988, 71: 41-51.
8 McDonald I R, Guinasso JR N L, Brooks J M, et al. Seafloor gas-hydrates: a video documenting oceanographic in fluences on their formation and dissolution(abstr). AAPG Bull, 1995, 79(6): 910.
9 Lashof D A, Ahuja R.Relative contributions of greenhouse gas emissions to global warming.Nature, 1990, 344(5):529-531.
10 Haq B U. Deep-sea response to eustatic chang and significance of gas hydrates forcontinental margin stratigraphy.Spec Publs Int Ass Sed 1993,18: 93-106.
11 Paull C K, UsslerⅢW, Dillon P D. Is the extent of glaciation limited by marinegas-hydrates?. Geophys Res Lett,1991, 18: 432-434.
12 Nisbet E G. The end of ice age. Can J Earth Sci, 1990, 27: 148-157.
13 Dillon W P, Paull C K. Marine gas hydrates II: geophysical evidence. In: Cox L L ed. Natural GasHydrates, Properties, Occurrence, Recovery . Butterworth, Woburn, MA, 1983.73-90.
14 Berner U, Faber E. Hydrocarbon gases in surface sediments of the South China Sea.In: Jin et al eds. Marine Geology and Geophysics of the South China Sea. China Ocean Press,1990.199-211.
15 Yamano M S, Uyeda Y A, Shipley T H.Estimates of heat flow derived from gas hydrates.Geology, 1982, 10: 339-343.

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