Surface-atmosphere exchange of ammonia over peatland using QCL-based eddy-covariance measurements and inferential modeling

被引:35
作者
Zoell, Undine [1 ]
Bruemmer, Christian [1 ]
Schrader, Frederik [1 ]
Ammann, Christof [2 ]
Ibrom, Andreas [3 ]
Flechard, Christophe R. [4 ]
Nelson, David D. [5 ]
Zahniser, Mark [5 ]
Kutsch, Werner L. [6 ]
机构
[1] Thunen Inst Climate Smart Agr, D-38116 Braunschweig, Germany
[2] Swiss Fed Res Stn Agroscope ART, CH-8046 Zurich, Switzerland
[3] Tech Univ Denmark, Dept Environm Engn, DK-2800 Lyngby, Denmark
[4] Agrocampus Ouest, INRA, SAS UMR1069, F-35042 Rennes, France
[5] Aerodyne Res Inc, Billerica, MA USA
[6] Univ Helsinki, Head Off, ICOS, FIN-00014 Helsinki, Finland
关键词
FLUX MEASUREMENTS; DRY DEPOSITION; WATER-VAPOR; NITROGEN DEPOSITION; REACTIVE NITROGEN; TRACE GASES; GRASSLAND; VEGETATION; FIELD; SITE;
D O I
10.5194/acp-16-11283-2016
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Recent advances in laser spectrometry offer new opportunities to investigate ecosystem-atmosphere exchange of environmentally relevant trace gases. In this study, we demonstrate the applicability of a quantum cascade laser (QCL) absorption spectrometer to continuously measure ammonia concentrations at high time resolution and thus to quantify the net exchange between a seminatural peatland ecosystem and the atmosphere based on the eddy-covariance approach. Changing diurnal patterns of both ammonia concentration and fluxes were found during different periods of the campaign. We observed a clear tipping point in early spring with decreasing ammonia deposition velocities and increasingly bidirectional fluxes that occurred after the switch from dormant vegetation to CO2 uptake but was triggered by a significant weather change. While several biophysical parameters such as temperature, radiation, and surface wetness were identified to partially regulate ammonia exchange at the site, the seasonal concentration pattern was clearly dominated by agricultural practices in the surrounding area. Comparing the results of a compensation point model with our measurement-based flux estimates showed considerable differences in some periods of the campaign due to overestimation of non-stomatal resistances caused by low acid ratios. The total cumulative campaign exchange of ammonia after 9 weeks, however, differed only in a 6% deviation with 911 and 857 gNH(3)-N ha(-1) deposition being found by measurements and modeling, respectively. Extrapolating our findings to an entire year, ammonia deposition was lower than reported by Hurkuck et al. (2014) for the same site in previous years using denuder systems. This was likely due to a better representation of the emission component in the net signal of eddy-covariance fluxes as well as better adapted site-specific parameters in the model. Our study not only stresses the importance of high-quality measurements for studying and assessing land surface-atmosphere interactions but also demonstrates the potential of QCL spectrometers for continuous observation of reactive nitrogen species as important additional instruments within long-term monitoring research infrastructures such as ICOS or NEON at sites with strong nearby ammonia sources leading to relatively high mean background concentrations and fluxes.
引用
收藏
页码:11283 / 11299
页数:17
相关论文
共 76 条
[1]   Technical note: Water vapour concentration and flux measurements with PTR-MS [J].
Ammann, C. ;
Brunner, A. ;
Spirig, C. ;
Neftel, A. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2006, 6 :4643-4651
[2]  
[Anonymous], 2012, R LANG ENV STAT COMP
[3]  
[Anonymous], 2011, EUROPEAN NITROGEN AS
[4]   Ammonia: emission, atmospheric transport and deposition [J].
Asman, WAH ;
Sutton, MA ;
Schjorring, JK .
NEW PHYTOLOGIST, 1998, 139 (01) :27-48
[5]   Global assessment of nitrogen deposition effects on terrestrial plant diversity: a synthesis [J].
Bobbink, R. ;
Hicks, K. ;
Galloway, J. ;
Spranger, T. ;
Alkemade, R. ;
Ashmore, M. ;
Bustamante, M. ;
Cinderby, S. ;
Davidson, E. ;
Dentener, F. ;
Emmett, B. ;
Erisman, J. -W. ;
Fenn, M. ;
Gilliam, F. ;
Nordin, A. ;
Pardo, L. ;
De Vries, W. .
ECOLOGICAL APPLICATIONS, 2010, 20 (01) :30-59
[6]   Fluxes of total reactive atmospheric nitrogen (ΣNr) using eddy covariance above arable land [J].
Bruemmer, Christian ;
Marx, Oliver ;
Kutsch, Werner ;
Ammann, Christof ;
Wolff, Veronika ;
Flechard, Christophe R. ;
Freibauer, Annette .
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2013, 65
[7]   Modelling the dynamic chemical interactions of atmospheric ammonia with leaf surface wetness in a managed grassland canopy [J].
Burkhardt, J. ;
Flechard, C. R. ;
Gresens, F. ;
Mattsson, M. ;
Jongejan, P. A. C. ;
Erisman, J. W. ;
Weidinger, T. ;
Meszaros, R. ;
Nemitz, E. ;
Sutton, M. A. .
BIOGEOSCIENCES, 2009, 6 (01) :67-84
[8]  
Dämmgen U, 2010, GEFAHRST REINHALT L, V70, P367
[9]  
Dämmgen U, 2002, J APPL BOT-ANGEW BOT, V76, P190
[10]   Emissions of methane and nitrous oxide from Australian sugarcane soils [J].
Denmead, O. T. ;
Macdonald, B. C. T. ;
Bryant, G. ;
Naylor, T. ;
Wilson, S. ;
Griffith, D. W. T. ;
Wang, W. J. ;
Salter, B. ;
White, I. ;
Moody, P. W. .
AGRICULTURAL AND FOREST METEOROLOGY, 2010, 150 (06) :748-756