Seasonal trends of the stable nitrogen isotope ratio in particulate nitrogen compounds and their gaseous precursors in Akita, Japan

Particulate matter (PM) can have adverse effects on human health. Moreover, because the mechanisms of PM formation and behavior in the atmosphere are notably complicated, to reduce PM concentrations effectively and meet environmental standards, source–receptor relationships must be clearly understoo...

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Main Author: Hiroto Kawashima
Format: Article
Language:English
Published: Stockholm University Press 2019-01-01
Series:Tellus: Series B, Chemical and Physical Meteorology
Subjects:
Online Access:http://dx.doi.org/10.1080/16000889.2019.1627846
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author Hiroto Kawashima
author_facet Hiroto Kawashima
author_sort Hiroto Kawashima
collection DOAJ
description Particulate matter (PM) can have adverse effects on human health. Moreover, because the mechanisms of PM formation and behavior in the atmosphere are notably complicated, to reduce PM concentrations effectively and meet environmental standards, source–receptor relationships must be clearly understood. Stable isotope ratios can be used to detect chemical processes and distinguish sources. In environmental science, especially in research on aerosols, stable isotope ratios have proven to constitute a powerful tool for source identification. However, there are few long-term studies of isotope fractionation during secondary aerosol formation. In this study, stable nitrogen isotope ratios (δ15N) of ammonia gas (NH3), nitrogen dioxide gas (NO2), nitric acid vapor (HNO3), particulate nitrate (NO3−), and ammonium (NH4+) in suspended PM (SPM) were analyzed to investigate seasonal trends and isotope fractionation during aerosol formation for long term sampling in Akita, Japan. The results indicated that δ15N-NH4+ in SPM and δ15N-NH3 gas ranged from 1.3‰ to 38.5‰ (mean 16.1‰) and from −33.6‰ to −0.0‰ (−16.9‰), respectively. Furthermore, δ15N-NO3− (SPM) and δ15N-NO2 and δ15N-HNO3 (gaseous) ranged from −4.6‰ to 4.8‰ (mean −0.5‰), from −8.2‰ to −3.1‰ (−5.4‰), and from −7.5‰ to 2.7‰ (−5.0‰), respectively. The mean annual isotope fractionation factors for transformations from gaseous NH3 to NH4+ in SPM, from gaseous NO2 to gaseous HNO3, and from HNO3 gas to NO3– in SPM in the atmospheric environment were +33.3‰, +0.5‰, and +4.9‰, respectively. Isotope fractionation of NH4+ in SPM was much higher than that of NO3– in SPM. As the chemical reaction from gaseous precursors progressed, δ15N-NO3– in SPM became steadily heavier.
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spelling doaj.art-2af383ccbad94c6da334c66bf012bbb42022-12-22T02:57:02ZengStockholm University PressTellus: Series B, Chemical and Physical Meteorology1600-08892019-01-0171110.1080/16000889.2019.16278461627846Seasonal trends of the stable nitrogen isotope ratio in particulate nitrogen compounds and their gaseous precursors in Akita, JapanHiroto Kawashima0Akita Prefectural UniversityParticulate matter (PM) can have adverse effects on human health. Moreover, because the mechanisms of PM formation and behavior in the atmosphere are notably complicated, to reduce PM concentrations effectively and meet environmental standards, source–receptor relationships must be clearly understood. Stable isotope ratios can be used to detect chemical processes and distinguish sources. In environmental science, especially in research on aerosols, stable isotope ratios have proven to constitute a powerful tool for source identification. However, there are few long-term studies of isotope fractionation during secondary aerosol formation. In this study, stable nitrogen isotope ratios (δ15N) of ammonia gas (NH3), nitrogen dioxide gas (NO2), nitric acid vapor (HNO3), particulate nitrate (NO3−), and ammonium (NH4+) in suspended PM (SPM) were analyzed to investigate seasonal trends and isotope fractionation during aerosol formation for long term sampling in Akita, Japan. The results indicated that δ15N-NH4+ in SPM and δ15N-NH3 gas ranged from 1.3‰ to 38.5‰ (mean 16.1‰) and from −33.6‰ to −0.0‰ (−16.9‰), respectively. Furthermore, δ15N-NO3− (SPM) and δ15N-NO2 and δ15N-HNO3 (gaseous) ranged from −4.6‰ to 4.8‰ (mean −0.5‰), from −8.2‰ to −3.1‰ (−5.4‰), and from −7.5‰ to 2.7‰ (−5.0‰), respectively. The mean annual isotope fractionation factors for transformations from gaseous NH3 to NH4+ in SPM, from gaseous NO2 to gaseous HNO3, and from HNO3 gas to NO3– in SPM in the atmospheric environment were +33.3‰, +0.5‰, and +4.9‰, respectively. Isotope fractionation of NH4+ in SPM was much higher than that of NO3– in SPM. As the chemical reaction from gaseous precursors progressed, δ15N-NO3– in SPM became steadily heavier.http://dx.doi.org/10.1080/16000889.2019.1627846stable nitrogen isotope rationh3no2hno3
spellingShingle Hiroto Kawashima
Seasonal trends of the stable nitrogen isotope ratio in particulate nitrogen compounds and their gaseous precursors in Akita, Japan
Tellus: Series B, Chemical and Physical Meteorology
stable nitrogen isotope ratio
nh3
no2
hno3
title Seasonal trends of the stable nitrogen isotope ratio in particulate nitrogen compounds and their gaseous precursors in Akita, Japan
title_full Seasonal trends of the stable nitrogen isotope ratio in particulate nitrogen compounds and their gaseous precursors in Akita, Japan
title_fullStr Seasonal trends of the stable nitrogen isotope ratio in particulate nitrogen compounds and their gaseous precursors in Akita, Japan
title_full_unstemmed Seasonal trends of the stable nitrogen isotope ratio in particulate nitrogen compounds and their gaseous precursors in Akita, Japan
title_short Seasonal trends of the stable nitrogen isotope ratio in particulate nitrogen compounds and their gaseous precursors in Akita, Japan
title_sort seasonal trends of the stable nitrogen isotope ratio in particulate nitrogen compounds and their gaseous precursors in akita japan
topic stable nitrogen isotope ratio
nh3
no2
hno3
url http://dx.doi.org/10.1080/16000889.2019.1627846
work_keys_str_mv AT hirotokawashima seasonaltrendsofthestablenitrogenisotoperatioinparticulatenitrogencompoundsandtheirgaseousprecursorsinakitajapan