Abstract
Abstract. Dry deposition of peroxyacetyl nitrate (PAN) is known to have a phytotoxic impact on plants under photochemical smog conditions, but it may also lead to higher productivity and threaten species richness of vulnerable ecosystems in remote regions. However, underlying mechanisms or controlling factors for PAN deposition are not well understood and studies on dry deposition of PAN are limited. In this study, we investigate the impact of PAN deposition on a nutrient-poor natural grassland ecosystem situated at the edge of an urban and industrialized region in Germany. PAN mixing ratios were measured within a 3.5 months summer to early autumn period. In addition, PAN fluxes were determined with the modified Bowen ratio technique for a selected period. The evaluation of both stomatal and non-stomatal deposition pathways was used to model PAN deposition over the entire summer–autumn period. We found that air masses at the site were influenced by two contrasting pollution regimes, which led to median diurnal PAN mixing ratios ranging between 50 and 300 ppt during unpolluted and between 200 and 600 ppt during polluted episodes. The measured PAN fluxes showed a clear diurnal cycle with maximal deposition fluxes of ~−0.1 nmol m−2 s−1 (corresponding to a deposition velocity of 0.3 cm s−1) during daytime and a significant non-stomatal contribution was found. The ratio of PAN to ozone deposition velocities was found to be ~0.1, which is much larger than assumed by current deposition models. The modelled PAN flux over the entire period revealed that PAN deposition over an entire day was 333 μg m−2 d−1 under unpolluted and 518 μg m−2 d−1 under polluted episodes. Additionally, thermochemical decomposition PAN deposition accounted for 32% under unpolluted episodes and 22% under polluted episodes of the total atmospheric PAN loss. However, the impact of PAN deposition as a nitrogen source to the nutrient-poor grassland was estimated to be only minor, under both unpolluted and polluted episodes.
Highlights
Originating from both anthropogenic and natural sources, peroxyacetyl nitrate (CH3C(O)O2NO2, PAN) is primarily known as an atmospheric pollutant
Based on the modified Bowen ratio (MBR) method, we find a considerable non-stomatal uptake of PAN
1.8 × 10−4 5.1 × 10−4 3.3 × 10−4 0.21 × 10−4 likely suggesting an underestimation of PAN deposition by current models
Summary
Originating from both anthropogenic and natural sources, peroxyacetyl nitrate (CH3C(O)O2NO2, PAN) is primarily known as an atmospheric pollutant. Both the peroxyacetyl radical (CH3C(O)O2, PA) and nitrogen dioxide (NO2), which form PAN via k1. CH3C(O)O2 + NO2 + M CH3C(O)O2NO2 + M, (R1). Due to its thermal instability via the back-reaction of R1 and subsequent reaction of PA with nitric oxide (NO), CH3C(O)O2 + NO k2 −→ CH3C(O)O NO2, (R2). Long-range transport of PAN in cold layers of the upper troposphere may constitute a significant source of reactive ni-
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