Affordable relaxed eddy accumulation system to measure fluxes of H2O, CO2, CH4 and N2O from ecosystems

被引:7
作者
Grelle, Achim [1 ]
Keck, Hannes [1 ]
机构
[1] Swedish Univ Agr Sci, Dept Ecol, Uppsala, Sweden
关键词
REA; Micrometeorology; Conditional sampling; Greenhouse gas fluxes; Turbulent fluxes; Nitrous oxide; EMISSIONS; EXCHANGE; COEFFICIENT;
D O I
10.1016/j.agrformet.2021.108514
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
The relaxed eddy accumulation (REA) technique is frequently applied to measure fluxes of a large variety of atmospheric tracers above ecosystems. It is often the method of choice since the eddy covariance (EC) technique is limited to a few tracers due to the lack of fast response analysers, high financial costs and in some cases high power consumption. REA avoids the need for a fast response analyser by collecting air from up-drafts and downdrafts into separate reservoirs. After collecting the air over a predefined time period, trace gas concentrations in the reservoirs are analysed by a slow response analyser and the average fluxes can be calculated. We developed and tested a REA system that is capable of measuring CO2, CH4, N2O and H2O fluxes simultaneously with only one gas analyser (Picarro G2805). This system is compatible with virtually any gas analyser and thus supports the flux analysis of a wide range of other air constituents such as isotopes, aerosols and volatile organic compounds. Furthermore, the modular design and rugged casing makes the sampling system robust and portable, and with its 12 V DC operation it is suitable for a wide range of field campaigns. The performance of the REA system was tested during the growing seasons of 2018 and 2020 on a grassland on organic soil in central Sweden. The system has worked reliably during several months in the Nordic climate, covering ambient temperatures between -20 degrees C and +30 degrees C. Measured fluxes of CO2 and H2O agree well with fluxes measured independently by an EC system. The similarity in the technology and the determined detection limits made us confident that the REA system even captures fluxes of CH4 and N2O well.
引用
收藏
页数:9
相关论文
共 29 条
[1]   Stability dependence of the relaxed eddy accumulation coefficient for various scalar quantities [J].
Ammann, C ;
Meixner, FX .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2002, 107 (D7-8)
[2]  
Aubinet M, 2000, ADV ECOL RES, V30, P113, DOI 10.1016/S0065-2504(08)60018-5
[3]   Design, construction and operation of flux measurement systems using the conditional sampling technique [J].
Beverland, IJ ;
Oneill, DH ;
Scott, SL ;
Moncrieff, JB .
ATMOSPHERIC ENVIRONMENT, 1996, 30 (18) :3209-3220
[4]   Modification of the relaxed eddy accumulation technique to maximize measured scalar mixing ratio differences in updrafts and downdrafts [J].
Bowling, DR ;
Delany, AC ;
Turnipseed, AA ;
Baldocchi, DD ;
Monson, RK .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D8) :9121-9133
[5]   The use of relaxed eddy accumulation to measure biosphere-atmosphere exchange of isoprene and of her biological trace gases [J].
Bowling, DR ;
Turnipseed, AA ;
Delany, AC ;
Baldocchi, DD ;
Greenberg, JP ;
Monson, RK .
OECOLOGIA, 1998, 116 (03) :306-315
[6]  
Brutsaert W., 2013, Evaporation into the Atmosphere: Theory, History and Applications
[7]  
BUSINGER JA, 1990, J ATMOS OCEAN TECH, V7, P349, DOI 10.1175/1520-0426(1990)007<0349:FMWCS>2.0.CO
[8]  
2
[9]   Multiscale estimates of N2O emissions from agricultural lands [J].
Desjardins, R. L. ;
Pattey, E. ;
Smith, W. N. ;
Worth, D. ;
Grant, B. ;
Srinivasan, R. ;
MacPherson, J. I. ;
Mauder, M. .
AGRICULTURAL AND FOREST METEOROLOGY, 2010, 150 (06) :817-824
[10]  
DESJARDINS RL, 1972, THESIS CORNELL U, P119