Methane emission from bogs in the subtaiga of Western Siberia: The development of standard model

被引:21
作者
Glagolev, M. V. [1 ,2 ,4 ,5 ]
Sabrekov, A. F. [1 ]
Kleptsova, I. E. [2 ]
Filippov, I. V. [2 ]
Lapshina, E. D. [2 ]
Machida, T. [3 ]
Maksyutov, Sh. Sh. [3 ]
机构
[1] Moscow MV Lomonosov State Univ, Fac Soil Sci, Moscow 119991, Russia
[2] Yugorskii State Univ, Khanty Mansiisk 628012, Russia
[3] Natl Inst Environm Studies, Tsukuba, Ibaraki 3058506, Japan
[4] Tomsk State Pedag Univ, Tomsk 634041, Russia
[5] Moscow MV Lomonosov State Univ, Inst Ecol Soil Sci, Moscow 119991, Russia
关键词
EURASIAN Soil Science; Methane Emission; Forest Steppe; Methane Flux; Water Table Level;
D O I
10.1134/S106422931210002X
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The methane emission from typical bog landscapes of the West Siberian subtaiga was studied in the summer-autumn of 2007-2010. The lowest specific fluxes (the median value is 0.08 mg C-CH4/m(2) per h) were recorded from ryams (raised bogs with dwarf shrub-sphagnum associations). From the ridges of the ridge-pool complexes, the fluxes were estimated at 0.49 mg C-CH4/m(2) per h; from the oligotrophic hollows, eutrophic bogs, floating lake mats, and mesotrophic quaking bogs, they were estimated at 2.68, 3.36, 4.53, and 4.98 mg C-CH4/m(2) per h, respectively. The maximal flux was determined from the lakes (the median is 17.98 mg C-CH4/m(2) per h). The regional assessment of the methane flux from the bogs of Western Siberia (2.93 Tg C-CH4/yr) was obtained on the basis of the authors' and literature data.
引用
收藏
页码:947 / 957
页数:11
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