4.7 Article

The use of stable oxygen and nitrogen isotopic signatures to reveal variations in the nitrate formation pathways and sources in different seasons and regions in China

期刊

ENVIRONMENTAL RESEARCH
卷 201, 期 -, 页码 -

出版社

ACADEMIC PRESS INC ELSEVIER SCIENCE
DOI: 10.1016/j.envres.2021.111537

关键词

Nitrogen isotope; Oxygen isotope; Nitrate; Seasonal variations; Southwestern China

资金

  1. National Natural Science Foundation of China [41863002]
  2. Jiangxi Provincial Natural Science Foundation [20202BABL213034]
  3. Open Foundation of State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences [SKLLQG1705]
  4. Jiangxi Provincial Education Department Science and Technology Research Project [GJJ170468]

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The study shows that nitrate in southern China, especially during warm months, is mainly derived from the OH radical pathway, while changes in formation pathways and isotopic composition are influenced by air pollution emissions. Higher isotopic values from NOx emissions in northern areas and during cold months lead to higher nitrate isotopic compositions.
Nitrate (NO3-) is one of the most important inorganic ions in fine particulate (PM2.5) and drives regional haze formation; however, the NO3- sources and formation mechanisms in different seasons and regions are still debated. Here, PM2.5 samples were collected from Kunming and Nanning in southwestern China from September 1, 2017, to February 28, 2018 (spanning warm and cold months). We measured the daily O and N isotopic compositions of NO3-(delta O-18-NO3- and delta N-15-NO3-), estimated the delta O-18-HNO3 values produced by different oxidation pathways, and quantified the NO3- formation pathways based on the isotope mass-balance equation. Our results showed that the delta O-18-NO3- values in Kunming (65.3 +/- 7.6 parts per thousand) and Nanning (67.7 +/- 10.1 parts per thousand) are close to the delta O-18-HNO3- values arising from the OH radical pathway (POH, 54.7 +/- 1.2 parts per thousand to 61.2 +/- 1.8 parts per thousand), suggesting that the delta O-18-NO3- values are mainly influenced by POH, which showed a contribution greater than 74%. Stronger surface solar radiation and higher air temperatures in low-latitude regions and warm months increased the amount of HNO3 produced by POH and reduced the amount of HNO3 produced by PN2O5, which produced low delta O-18-NO3- values. Increased air pollution emissions decreased the contribution from POH and increased the contribution from N2O5 and NO3 pathways (PN2O5+NO3). The delta N-15-NO3- values of PM2.5 in Kunming (7.3 +/- 2.8 parts per thousand) were slightly higher than those in Nanning (2.8 +/- 2.7 parts per thousand). The increased NOx emissions with positive isotopic values led to high delta N-15-NO3- values in northern China and during cold months. A higher f(NO2) (f(NO2) = NO2/(NO + NO2), temperature, and contribution of POH produced lower N isotope fractionation between NOx and delta N-15-NO3-, which was found to further decrease the delta N-15-NO3- values in southwestern China and during warm months.

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