Atmospheric concentrations of ammonia and ammonium at an agricultural site in the southeast United States
In this study, we present ∼1 yr (October 1998–September 1999) of 12-hour mean ammonia (NH 3), ammonium (NH 4 +), hydrochloric acid (HCl), chloride (Cl −), nitrate (NO 3 −), nitric acid (HNO 3), nitrous acid (HONO), sulfate (SO 4 2−), and sulfur dioxide (SO 2) concentrations measured at an agricultur...
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Veröffentlicht in: | Atmospheric environment (1994) 2002-04, Vol.36 (10), p.1661-1674 |
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Sprache: | eng |
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Zusammenfassung: | In this study, we present ∼1
yr (October 1998–September 1999) of 12-hour mean ammonia (NH
3), ammonium (NH
4
+), hydrochloric acid (HCl), chloride (Cl
−), nitrate (NO
3
−), nitric acid (HNO
3), nitrous acid (HONO), sulfate (SO
4
2−), and sulfur dioxide (SO
2) concentrations measured at an agricultural site in North Carolina's Coastal Plain region. Mean gas concentrations were 0.46, 1.21, 0.54, 5.55, and 4.15
μg
m
−3 for HCl, HNO
3, HONO, NH
3, and SO
2, respectively. Mean aerosol concentrations were 1.44, 1.23, 0.08, and 3.37
μg
m
−3 for NH
4
+, NO
3
−, Cl
−, and SO
4
2−, respectively. Ammonia, NH
4
+, HNO
3, and SO
4
2− exhibit higher concentrations during the summer, while higher SO
2 concentrations occur during winter. A meteorology-based multivariate regression model using temperature, wind speed, and wind direction explains 76% of the variation in 12-hour mean NH
3 concentrations (
n=601). Ammonia concentration increases exponentially with temperature, which explains the majority of variation (54%) in 12-hour mean NH
3 concentrations. Dependence of NH
3 concentration on wind direction suggests a local source influence. Ammonia accounts for >70% of NH
x
(NH
x
=NH
3+NH
4
+) during all seasons. Ammonium nitrate and sulfate aerosol formation does not appear to be NH
3 limited. Sulfate is primarily associated ammonium sulfate, rather than bisulfate, except during the winter when the ratio of NO
3
−–NH
4
+ is ∼0.66. The annual average NO
3
−–NH
4
+ ratio is ∼0.25. |
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ISSN: | 1352-2310 1873-2844 |
DOI: | 10.1016/S1352-2310(02)00171-1 |