收稿日期: 2004-03-17
修回日期: 2004-07-27
网络出版日期: 2004-10-20
METHANE GENERATION IN PERMAFROST SEDIMENTS
Received date: 2004-03-17
Revised date: 2004-07-27
Online published: 2004-10-20
李桂菊, 庄新国 . 多年冻土区沉积物中甲烷的生成[J]. 天然气地球科学, 2004 , 15(5) : 516 -518 . DOI: 10.11764/j.issn.1672-1926.2004.05.516
With the development of permafrost activities, it is clear that the discovery of viable microbes in permafrost raised their research status due to their peculiar physiological mechanism. Methane generation from bicarbonate and acetate showed an affected interest with microbes activities. The results of this work has great theory and economic meanings. In addition, it is also promising for the application prospects to the continual development of organisms research.
Key words: Permafrost; Methane; Microbes.
[1]Rivina E. Microbial Life in Permafrost[J]. Advances in Space Rresearch, 2004,33:1215-1221.
[2] Laurinavichus K S, Belyaev S S. Application of carbon radioa-= ctive isotopes to determine the intensity of methane oxidation by micro-organisms in natural waters[J].Mikrobiologiya,1978, 47:1115-1117.
[3] Samarkin V, Gundelwein A, Pfeiffer E M. Land-ocean syst ems in siberian arctic[M]. Berlin: Springer, 1999. 329-342.
[4] Farell J, Rose A. In thermobiology[M]. London: Academic, 1967. 147-218.
[5] Anderson D. ICE nucleation and the substrate-ice intorface[J]. Nature, 1967,216: 563-566.
[6] Tsytovich N A. Mekhanika merzlykh gruntov (Mechanics of Frozen Soils)[M]. Moscow: Vysshaya Shkola, 1973.
[7] Rivkina E, Gilichinsky D, McKay C. et al. Permafrost Resp onse on Economic Development, Environmental Security and Natural Resources, Issue of NATO Series[M]. Amsterdam: Kluwer, 2001. 487-496.
/
〈 |
|
〉 |