Application of a GC-ECD for measurements of biosphere-atmosphere exchange fluxes of peroxyacetyl nitrate using the relaxed eddy accumulation and gradient method

被引:12
|
作者
Moravek, A. [1 ]
Foken, T. [2 ,3 ]
Trebs, I. [1 ]
机构
[1] Max Planck Inst Chem, Biogeochem Dept, D-55020 Mainz, Germany
[2] Univ Bayreuth, Dept Micrometeorol, D-95447 Bayreuth, Germany
[3] Univ Bayreuth, Bayreuth Ctr Ecol & Environm Res BayCEER, D-95447 Bayreuth, Germany
关键词
VOLATILE ORGANIC-COMPOUNDS; ELECTRON-CAPTURE DETECTION; DRY DEPOSITION; SURFACE-LAYER; MICROMETEOROLOGICAL TECHNIQUES; COVARIANCE MEASUREMENTS; CARBON-TETRACHLORIDE; GAS-CHROMATOGRAPHY; QUALITY ASSESSMENT; SCALAR SIMILARITY;
D O I
10.5194/amt-7-2097-2014
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Peroxyacetyl nitrate (PAN) may constitute a significant fraction of reactive nitrogen in the atmosphere. Current knowledge about the biosphere-atmosphere exchange of PAN is limited, and only few studies have investigated the deposition of PAN to terrestrial ecosystems. We developed a flux measurement system for the determination of biosphere-atmosphere exchange fluxes of PAN using both the hyperbolic relaxed eddy accumulation (HREA) method and the modified Bowen ratio (MBR) method. The system consists of a modified, commercially available gas chromatograph with electron capture detection (GC-ECD, Meteorologie Consult GmbH, Germany). Sampling was performed by trapping PAN onto two pre-concentration columns; during HREA operation one was used for updraft and one for down-draft events, and during MBR operation the two columns allowed simultaneous sampling at two measurement heights. The performance of the PAN flux measurement system was tested at a natural grassland site, using fast-response ozone (O-3) measurements as a proxy for both methods. The measured PAN fluxes were comparatively small (daytime PAN deposition was on average -0.07 nmolm(-2) s(-1)) and, thus, prone to significant uncertainties. A major challenge in the design of the system was the resolution of the small PAN mixing ratio differences. Consequently, the study focuses on the performance of the analytical unit and a detailed analysis of errors contributing to the overall uncertainty. The error of the PAN mixing ratio differences ranged from 4 to 15 ppt during the MBR and between 18 and 26 ppt during the HREA operation, while during daytime measured PAN mixing ratios were of similar magnitude. Choosing optimal settings for both the MBR and HREA method, the study shows that the HREA method did not have a significant advantage towards the MBR method under well-mixed conditions as was expected.
引用
收藏
页码:2097 / 2119
页数:23
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