Global Boundary Lines of N2O and CH4 Emission in Peatlands

被引:3
作者
Parn, Jaan [1 ]
Aasa, Anto [1 ]
Egorov, Sergey [1 ]
Filippov, Ilya [2 ]
Gabiri, Geofrey [3 ,4 ]
Gheorghe, Iuliana [5 ]
Jarveoja, Jarvi [1 ]
Kasak, Kuno [1 ]
Laggoun-Defarge, Fatima [6 ]
Luswata, Charles Kizza [4 ]
Maddison, Martin [1 ]
Mitsch, William J. [7 ]
Oskarsson, Hlynur [8 ]
Pellerin, Stephanie [9 ]
Salm, Juri-Ott [1 ,10 ]
Sohar, Kristina [1 ]
Soosaar, Kaido [1 ]
Teemusk, Alar [1 ]
Tenywa, Moses M. [4 ]
Villa, Jorge A. [6 ]
Vohla, Christina [1 ]
Mander, Ulo [1 ,11 ]
机构
[1] Univ Tartu, Inst Ecol & Earth Sci, Vanemuise St 46, EE-51014 Tartu, Estonia
[2] Yugra State Univ, UNESCO Chair Environm Dynam & Climate Change, Khanty Mansiysk 628012, Russia
[3] Kenyatta Univ, Dept Geog, Nairobi, Kenya
[4] Makerere Univ, Coll Agr & Environm Sci, Dept Agr Prod, Kampala, Uganda
[5] Ecol Univ Bucharest, Fac Ecol & Environm Protect, Bucharest, Romania
[6] Univ Orleans, CNRS, Inst Sci Terre Orleans, Orleans, France
[7] Florida Gulf Coast Univ, Kapnick Ctr, Ft Myers, FL 33965 USA
[8] Agr Univ Iceland, Fac Environm Sci, IS-311 Hvanneyri, Borgarnes, Iceland
[9] Univ Montreal, Inst Rech Biol Vegetale, Jardin Bot Montreal, Montreal, PQ H1X 2B2, Canada
[10] Estonian Fund Nat, Dept Geog, EE-51014 Tartu, Estonia
[11] Natl Res Inst Sci & Technol Environm & Agr Irstea, Hydrosystems & Bioproc Res Unit, F-92761 Antony, France
来源
ROLE OF NATURAL AND CONSTRUCTED WETLANDS IN NUTRIENT CYCLING AND RETENTION ON THE LANDSCAPE | 2015年
关键词
Bog; Ecosystem; Fen; Histosol; Hydromorphic; Landscape; Methane; Microbiology; Mire; Nitrous oxide; Organic soil; NITROUS-OXIDE; METHANE EMISSION; WATER-TABLE; SOIL; FLUXES; N-2; DENITRIFICATION; COMPLEX; CARBON; MODEL;
D O I
10.1007/978-3-319-08177-9_7
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Predicting N2O (nitrous oxide) and CH4 (methane) emissions from peatlands is challenging because of the complex coaction of biogeochemical factors. This study uses data from a global soil and gas sampling campaign. The objective is to analyse N2O and CH4 emissions in terms of peat physical and chemical conditions. Our study areas were evenly distributed across the A, C and D climates of the Koppen classification. Gas measurements using static chambers, groundwater analysis and gas and peat sampling for further laboratory analysis have been conducted in 13 regions evenly distributed across the globe. In each study area at least two study sites were established. Each site featured at least three sampling plots, three replicate chambers and corresponding soil pits and one observation well per plot. Gas emissions were measured during 2-3 days in at least three sessions. A log-log linear function limits N2O emissions in relation to soil TIN (total inorganic nitrogen). The boundary line of N2O in terms of soil temperature is semilog linear. The closest representation of the relationship between N2O and soil moisture is a local regression curve with its optimum at 60-70 %. Semilog linear upper boundaries describe the effects of soil moisture and soil temperature to CH4 best. The global N2O boundary lines revealed a striking similarity with the Southern German N2O boundary lines, as well as with analogous scattergrams for Europe (Couwenberg et al. 2011) and Southern Queensland (Wang and Dalal 2010). This suggests that local rather than global conditions determine land-use-based greenhouse gas emissions. Further work will analyse relationships between the environmental factors and the spatial distribution of the main functional genes nirS, nirK and nosZ regulating the denitrification process in the soil samples currently stored in fridge at -18 degrees. An additional analysis will study the relationships between the intensity of CH4 emissions and methanogenesis-regulating functional genes mcrA, pmoA and dsrAB.
引用
收藏
页码:87 / 102
页数:16
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