Oxidation of atmospheric methane in Northern European soils, comparison with other ecosystems, and uncertainties in the global terrestrial sink

被引:361
作者
Smith, KA
Dobbie, KE
Ball, BC
Bakken, LR
Sitaula, BK
Hansen, S
Brumme, R
Borken, W
Christensen, S
Priemé, A
Fowler, D
Macdonald, JA
Skiba, U
Klemedtsson, L
Kasimir-Klemedtsson, A
Degórska, A
Orlanski, P
机构
[1] Univ Edinburgh, Inst Ecol & Resource Management, Edinburgh EH9 3JG, Midlothian, Scotland
[2] Scottish Agr Coll, Edinburgh, Midlothian, Scotland
[3] Agr Univ Norway, Dept Soil & Water Sci, N-1432 As, Norway
[4] Norwegian Ctr Ecol Agr, Tingvoll, Norway
[5] Univ Gottingen, Inst Soil Sci & Forest Nutr, D-3400 Gottingen, Germany
[6] Univ Copenhagen, Dept Populat Biol, DK-1168 Copenhagen, Denmark
[7] Inst Terr Ecol, Edinburgh, Midlothian, Scotland
[8] Environm Res Inst, Gothenburg, Sweden
[9] Inst Environm Protect, Warsaw, Poland
关键词
ecosystem; global terrestrial sink; land-use change; methane oxidation; soil;
D O I
10.1046/j.1365-2486.2000.00356.x
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
This paper reports the range and statistical distribution of oxidation rates of atmospheric CH(4) in soils found in Northern Europe in an international study, and compares them with published data for various other ecosystems. It reassesses the size, and the uncertainty in, the global terrestrial CH(4) sink, and examines the effect of land-use change and other factors on the oxidation rate. Only soils with a very high water table were sources of CH(4); all others were sinks. Oxidation rates varied from 1 to nearly 200 mu g CH(4) m(-2) h(-1); annual rates for sites measured for greater than or equal to 1 y were 0.1-9.1 kg CH(4) ha(-1) y(-1), with a log-normal distribution (log-mean approximate to 1.6 kg CH(4) ha(-1) y(-1)). Conversion of natural soils to agriculture reduced oxidation rates by two-thirds - closely similar to results reported for other regions. N inputs also decreased oxidation rates. Full recovery of rates after these disturbances takes > 100 y. Soil bulk density, water content and gas diffusivity had major impacts on oxidation rates. Trends were similar to those derived from other published work. Increasing acidity reduced oxidation, partially but not wholly explained by poor diffusion through litter layers which did not themselves contribute to the oxidation. The effect of temperature was small, attributed to substrate limitation and low atmospheric concentration. Analysis of all available data for CH(4) oxidation rates in situ showed similar log-normal distributions to those obtained for our results, with generally little difference between different natural ecosystems, or between short-and longer-term studies. The overall global terrestrial sink was estimated at 29 Tg CH(4) y(-1), close to the current IPCC assessment, but with a much wider uncertainty range (7 to > 100 Tg CH(4) y(-1)). Little or no information is available for many major ecosystems; these should receive high priority in future research.
引用
收藏
页码:791 / 803
页数:13
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