Forest streams are important sources for nitrous oxide emissions

被引:35
作者
Audet, Joachim [1 ,2 ]
Bastviken, David [3 ]
Bundschuh, Mirco [2 ,4 ]
Buffam, Ishi [5 ]
Feckler, Alexander [2 ]
Klemedtsson, Leif [6 ]
Laudon, Hjalmar [7 ]
Lofgren, Stefan [2 ]
Natchimuthu, Sivakiruthika [3 ]
Oquist, Mats [7 ]
Peacock, Mike [2 ]
Wallin, Marcus B. [8 ]
机构
[1] Aarhus Univ, Dept Biosci, Vejlsovej 25, DK-8600 Silkeborg, Denmark
[2] Swedish Univ Agr Sci, Dept Aquat Sci & Assessment, Uppsala, Sweden
[3] Linkoping Univ, Dept Themat Studies Environm Change, Linkoping, Sweden
[4] Univ Koblenz Landau, Inst Environm Sci, Landau, Germany
[5] Univ Cincinnati, Dept Biol Sci, Cincinnati, OH USA
[6] Univ Gothenburg, Dept Earth Sci, Gothenburg, Sweden
[7] Swedish Univ Agr Sci, Dept Forest Ecol & Management, Umea, Sweden
[8] Uppsala Univ, Dept Earth Sci Air Water & Landscape Sci, Uppsala, Sweden
关键词
agriculture; forest; greenhouse gas; nitrogen; nitrous oxide; river; stream; HEADWATER STREAMS; SURFACE WATERS; N2O EMISSIONS; BOREAL CATCHMENTS; ORGANIC-CARBON; SPRUCE FOREST; SOIL; DENITRIFICATION; METHANE; NITRATE;
D O I
10.1111/gcb.14812
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Streams and river networks are increasingly recognized as significant sources for the greenhouse gas nitrous oxide (N2O). N2O is a transformation product of nitrogenous compounds in soil, sediment and water. Agricultural areas are considered a particular hotspot for emissions because of the large input of nitrogen (N) fertilizers applied on arable land. However, there is little information on N2O emissions from forest streams although they constitute a major part of the total stream network globally. Here, we compiled N2O concentration data from low-order streams similar to 1,000 observations from 172 stream sites) covering a large geographical gradient in Sweden from the temperate to the boreal zone and representing catchments with various degrees of agriculture and forest coverage. Our results showed that agricultural and forest streams had comparable N2O concentrations of 1.6 +/- 2.1 and 1.3 +/- 1.8 mu g N/L, respectively (mean +/- SD) despite higher total N (TN) concentrations in agricultural streams (1,520 +/- 1,640 vs. 780 +/- 600 mu g N/L). Although clear patterns linking N2O concentrations and environmental variables were difficult to discern, the percent saturation of N2O in the streams was positively correlated with stream concentration of TN and negatively correlated with pH. We speculate that the apparent contradiction between lower TN concentration but similar N2O concentrations in forest streams than in agricultural streams is due to the low pH (< 6) in forest soils and streams which affects denitrification and yields higher N2O emissions. An estimate of the N2O emission from low-order streams at the national scale revealed that similar to 1.8 x 10(9) g N2O-N are emitted annually in Sweden, with forest streams contributing about 80% of the total stream emission. Hence, our results provide evidence that forest streams can act as substantial N2O sources in the landscape with 800 x 10(9) g CO2-eq emitted annually in Sweden, equivalent to 25% of the total N2O emissions from the Swedish agricultural sector.
引用
收藏
页码:629 / 641
页数:13
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