Inventories of N2O and NO emissions from European forest soils

被引:145
作者
Kesik, M
Ambus, P
Baritz, R
Brüggemann, NB
Butterbach-Bahl, K
Damm, M
Duyzer, J
Horváth, L
Kiese, R
Kitzler, B
Leip, A
Li, C
Pihlatie, M
Pilegaard, K
Seufert, G
Simpson, D
Skiba, U
Smiatek, G
Vesala, T
Zechmeister-Boltenstern, S
机构
[1] IFU, Karlsruhe Res Ctr, Inst Meteorol & Climate Res, IMK, D-82467 Garmisch Partenkirchen, Germany
[2] Riso Natl Lab, Dept Plant Biol & Biogeochem, Riso, Denmark
[3] Fed Inst Geosci & Nat Resources, D-3000 Hannover, Germany
[4] Netherlands Org Appl Sci Res, Apeldoorn, Netherlands
[5] Hungarian Meteorol Serv, Dept Anal Atmospher Environm, Budapest, Hungary
[6] Inst Forest Ecol & Soil, Fed Forest Res Ctr, Vienna, Austria
[7] Commiss European Communities, Joint Res Ctr, Inst Environm, I-21020 Ispra, Italy
[8] Univ New Hampshire, Inst Study Earth Oceans & Space, Durham, NH 03824 USA
[9] Univ Helsinki, Dept Phys Sci, Helsinki, Finland
[10] Norwegian Meteorol Inst, Oslo, Norway
[11] NERC, Ctr Ecol & Hydrol, Edinburgh, Midlothian, Scotland
关键词
D O I
10.5194/bg-2-353-2005
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Forest soils are a significant source for the primary and secondary greenhouse gases N2O and NO. However, current estimates are still uncertain due to the still limited number of field measurements and the herein observed pronounced variability of N trace gas fluxes in space and time, which are due to the variation of environmental factors such as soil and vegetation properties or meteorological conditions. To overcome these problems we further developed a process-oriented model, the PnET-N-DNDC model, which simulates the N trace gas exchange on the basis of the processes involved in production, consumption and emission of N trace gases. This model was validated against field observations of N trace gas fluxes from 19 sites obtained within the EU project NOFRETETE, and shown to perform well for N2O (r(2) = 0.68, slope = 0.76) and NO (r(2) = 0.78, slope = 0.73). For the calculation of a European-wide emission inventory we linked the model to a detailed, regionally and temporally resolved database, comprising climatic properties (daily resolution), and soil parameters, and information on forest areas and types for the years 1990, 1995 and 2000. Our calculations show that N trace gas fluxes from forest soils may vary substantial from year to year and that distinct regional patterns can be observed. Our central estimate of NO emissions from forest soils in the EU amounts to 98.4, 84.9 and 99.2 kt N yr(-1) 1, using meteorology from 1990, 1995 and year 2000, respectively. This is < 1.0% of pyrogenic NOx emissions. For N2O emissions the central estimates were 86.8, 77.6 and 81.6 kt N yr(-1), respectively, which is approx. 14.5% of the source strength coming from agricultural soils. An extensive sensitivity analysis was conducted which showed a range in emissions from 44.4 to 254.0 kt N yr(-1) for NO and 50.7 to 96.9 kt N yr(-1) for N2O, for year 2000 meteorology. The results show that process-oriented models coupled to a GIS are useful tools for the calculation of regional, national, or global inventories of biogenic N trace gas emissions from soils. This work represents the most comprehensive effort to date to simulate NO and N2O emissions from European forest soils.
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收藏
页码:353 / 375
页数:23
相关论文
共 90 条
[71]   Inventorying emissions from nature in Europe [J].
Simpson, D ;
Winiwarter, W ;
Börjesson, G ;
Cinderby, S ;
Ferreiro, A ;
Guenther, A ;
Hewitt, CN ;
Janson, R ;
Khalil, MAK ;
Owen, S ;
Pierce, TE ;
Puxbaum, H ;
Shearer, M ;
Skiba, U ;
Steinbrecher, R ;
Tarrasón, L ;
Öquist, MG .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D7) :8113-8152
[72]  
Simpson D., 2003, 12003 EMEP
[73]   The potential to mitigate global warming with no-tillage management is only realized when practised in the long term [J].
Six, J ;
Ogle, SM ;
Breidt, FJ ;
Conant, RT ;
Mosier, AR ;
Paustian, K .
GLOBAL CHANGE BIOLOGY, 2004, 10 (02) :155-160
[74]   Nitric oxide emissions from agricultural soils in temperate and tropical climates: sources, controls and mitigation options [J].
Skiba, U ;
Fowler, D ;
Smith, KA .
NUTRIENT CYCLING IN AGROECOSYSTEMS, 1997, 48 (1-2) :139-153
[75]   EMISSIONS OF NO AND N2O FROM SOILS [J].
SKIBA, U ;
FOWLER, D ;
SMITH, K .
ENVIRONMENTAL MONITORING AND ASSESSMENT, 1994, 31 (1-2) :153-158
[76]   Leaf uptake of nitrogen dioxide (NO2) in a tropical wet forest:: implications for tropospheric chemistry [J].
Sparks, JP ;
Monson, RK ;
Sparks, KL ;
Lerdau, M .
OECOLOGIA, 2001, 127 (02) :214-221
[77]   A process-oriented model of N2O and NO emissions from forest soils 2.: Sensitivity analysis and validation [J].
Stange, F ;
Butterbach-Bahl, K ;
Papen, H ;
Zechmeister-Boltenstern, S ;
Li, CS ;
Aber, J .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2000, 105 (D4) :4385-4398
[78]  
STANGE F, 2000, THESIS U FREIBURG FR
[79]   A European inventory of soil nitric oxide emissions and the effect of these emissions on the photochemical formation of ozone [J].
Stohl, A ;
Williams, E ;
Wotawa, G ;
KrompKolb, H .
ATMOSPHERIC ENVIRONMENT, 1996, 30 (22) :3741-3755
[80]   Initial soil pH affects the pH at which nitrification ceases due to self-induced acidification of microbial microsites [J].
Strong, DT ;
Sale, PWG ;
Helyar, KR .
AUSTRALIAN JOURNAL OF SOIL RESEARCH, 1997, 35 (03) :565-570