Ambient mixing ratios of ammonia during pre and post harvest paddy season in Punjab
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IISERM
Abstract
Ammonia gas plays a key role in atmospheric chemistry as it partitions actively
between gas and aerosol phase. The sources and ambient mixing ratios of ammonia
are poorly known over the North West- Indo Gangetic Plain. Potentially the region is
thought to be a hotspot for ammonia emissions because agriculture and biomass
burning. The residue burning practice, is functional at NW- IGP after the harvesting
of paddy, in October to November. This anthropogenic contamination has significant
impacts on the formation of secondary inorganic aerosol particles and ill-effects on
humans including irritation to the eyes, skin, nose and the respiratory system. No
studies have been done yet to investigate changes in ambient ammonia mixing ratios
due to paddy residue burning in the region. Other harmful gases are also emitted from
the paddy residue burning such as carbon monoxide, acetonitrile, benzene and
benzenoids. This study reports the measured enhancements seen in ambient ammonia
in the post paddy harvest season (October 05,2015 to November 26,2015). Ammonia
was quantified using the cavity ring down spectroscopy technique. Enhancements in
the 4 minute averaged data were observed to be: for PM 2.5 (97.2±62.1 vs 23.1±51.5 μg
m -3 ) , CO (658.9±442.7 vs 369.4±151.9 ppb), acetonitrile (1.3±1.2 vs 0.5±0.3 ppb),
benzene (2.7±2.5 vs 1.4±1.1 ppb), toluene (4.2±4.9 vs 2.1±2.2 ppb), sum of C8
aromatics ;sum of ethyl benzene and xylenes (2.8±3.1 vs 1.7 ± 1.3 ppb) and ammonia
(31.2±13.9.vs 25.0±9.1 ppb) were by a factor of 1.9, 1.8, 2.3, 1.9, 1.9, 1.6 and 1.2
respectively as compared to the pre harvest season (September 06,2015- October
04,2015). For ammonia during 09:00-12:00 hours of the day, a peak in mixing ratio is
observed and it is 1.6 times than that observed in pre harvest season, clearly
signifying influence of paddy residue burning emissions. The enhancement in gas
phase ammonia scales with temperature and low relative humidity consistent with
aerosol phase conversion of ammonium nitrate and ammonium chloride salts to gas
phase ammonia. Results show active chemical processing of reactive atmospheric
nitrogen which requires further investigations.