4.7 Article

Sources of ammonium in seasonal wet deposition at a coastal New England city

Journal

ATMOSPHERIC ENVIRONMENT
Volume 260, Issue -, Pages -

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.atmosenv.2021.118557

Keywords

Stable isotope; Ammonium; Wet scavenging; Precipitation; Deposition; Long-range transport

Funding

  1. Institute at Brown for Environment and Society through the Voss Fellowship for Environmental Science and Communication
  2. IBES Equipment Award
  3. National Science Foundation [1624618, 1351932]
  4. International Atomic Energy Agency (IAEA) [F32008]
  5. Directorate For Geosciences
  6. Div Atmospheric & Geospace Sciences [1624618] Funding Source: National Science Foundation
  7. Div Atmospheric & Geospace Sciences
  8. Directorate For Geosciences [1351932] Funding Source: National Science Foundation

Ask authors/readers for more resources

National monitoring networks have reported an increase in ammonium (NH4+) deposition, dominating inorganic nitrogen deposition across most of the United States. Atmospheric deposition of fixed nitrogen has significant environmental consequences, including acidification and eutrophication. In the study site, long-range transport via in-cloud scavenging tended to play a stronger role in shaping w-NH4+ patterns.
National monitoring networks have reported an increase in ammonium (NH4+) deposition, such that NH4+ now dominates inorganic nitrogen deposition across most of the United States. Atmospheric deposition of fixed nitrogen has significant environmental consequences, including acidification and eutrophication. Thus, understanding source contributions is critical for formulating policies to mitigate the effects of excess nitrogen in sensitive ecosystems. Here, we investigated sources of wet-deposited NH4+ (w-NH4+) in Providence, RI, U.S.A., a mid-sized coastal city at the head of Narragansett Bay. We utilized concentration measurements, nitrogen stable isotopes (815N), and air mass back trajectory analysis for precipitation events and intra-event samples collected between January-November 2018. There was a general lack of seasonality in 815N(w-NH4+). Air mass origin had a strong influence on [w-NH4+], but [w-NH4+] was not related to 815N(w-NH4+), suggesting the potential dominance of a single NH3 emission source type. An average 815N(w-NH4+) of -3.7 +/- 3.5 parts per thousand (n = 42) was measured for daily-based precipitation. This value is consistent with previous measurements in the U.S. over the past 40 years, indicating a similar source of NH3 across the U.S. likely derived from agricultural activities. Intra-event analysis from precipitation events collected throughout the year found frequent mid- and end-event [w-NH4+] peaks that were suggested to be related to in-cloud [w-NH4+] changes rather than changes in below-cloud scavenging due to a consistent corresponding shift in precipitation intensity. Large intra-event 815N(w-NH4+) variations as high as 15.9 parts per thousand were also observed. However, the cumulative mass-weighted 815N(w-NH4+) of the intra-event series tended to converge to a similar value (-4.8 +/- 1.3 parts per thousand; n = 6). Overall, our results indicate that long-range transport via in-cloud scavenging tended to play a stronger role in shaping w-NH4+ patterns compared to local emissions at our study site.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available