TY - JOUR
T1 - Assessment and quantification of NOx sources at a regional background site in North China
T2 - Comparative results from a Bayesian isotopic mixing model and a positive matrix factorization model
AU - Zong, Zheng
AU - Tan, Yang
AU - Wang, Xiaoping
AU - Tian, Chongguo
AU - Fang, Yunting
AU - Chen, Yingjun
AU - Fang, Yin
AU - Han, Guangxuan
AU - Li, Jun
AU - Zhang, Gan
N1 - Publisher Copyright:
© 2018 Elsevier Ltd
PY - 2018/11
Y1 - 2018/11
N2 - Regional sources of nitrogen oxides (NOx) in North China during summer were explored using both a Bayesian isotopic mixing model and a positive matrix factorization (PMF) model. Results showed that the nitrogen isotope (δ15N) composition of particulate nitrate (NO3 −) varied between −8.9‰ and +14.1‰ while the oxygen isotope (δ18O) composition ranged from +57.4‰ to +93.8‰. Based on results from the Bayesian isotopic mixing model, the contribution of the hydroxyl radical (•OH) NOx conversion pathway showed clear diurnal fluctuation; values were higher during the day (0.53 ± 0.16) and lower overnight (0.42 ± 0.17). Values peaked at 06:00–12:00 and then decreased gradually until 00:00–06:00 the next day. Coal combustion (31.34 ± 9.04%) was the most significant source of NOx followed by biomass burning (25.74 ± 2.58%), mobile sources (23.83 ± 3.66%), and microbial processes (19.09 ± 5.21%). PMF results indicated that the contribution from mobile sources was 19.83%, slightly lower as compared to the Bayesian model (23.83%). The PMF model also reported a lower contribution from coal combustion (28.65%) as compared to the Bayesian model (31.34%); however, the sum of biomass burning and microbial processes in the Bayesian model (44.83%) was lower than the aggregate of secondary inorganic aerosol, sea salt, and soil dust in PMF model (51.52%). Overall, differences between the two models were minor, suggesting that this study provided a reasonable source quantification for NOx in North China during summer. Resulting NOx source difference from Bayesian isotopic mixing model and PMF model in North China was minor with the largest discrepancy of 6.69%.
AB - Regional sources of nitrogen oxides (NOx) in North China during summer were explored using both a Bayesian isotopic mixing model and a positive matrix factorization (PMF) model. Results showed that the nitrogen isotope (δ15N) composition of particulate nitrate (NO3 −) varied between −8.9‰ and +14.1‰ while the oxygen isotope (δ18O) composition ranged from +57.4‰ to +93.8‰. Based on results from the Bayesian isotopic mixing model, the contribution of the hydroxyl radical (•OH) NOx conversion pathway showed clear diurnal fluctuation; values were higher during the day (0.53 ± 0.16) and lower overnight (0.42 ± 0.17). Values peaked at 06:00–12:00 and then decreased gradually until 00:00–06:00 the next day. Coal combustion (31.34 ± 9.04%) was the most significant source of NOx followed by biomass burning (25.74 ± 2.58%), mobile sources (23.83 ± 3.66%), and microbial processes (19.09 ± 5.21%). PMF results indicated that the contribution from mobile sources was 19.83%, slightly lower as compared to the Bayesian model (23.83%). The PMF model also reported a lower contribution from coal combustion (28.65%) as compared to the Bayesian model (31.34%); however, the sum of biomass burning and microbial processes in the Bayesian model (44.83%) was lower than the aggregate of secondary inorganic aerosol, sea salt, and soil dust in PMF model (51.52%). Overall, differences between the two models were minor, suggesting that this study provided a reasonable source quantification for NOx in North China during summer. Resulting NOx source difference from Bayesian isotopic mixing model and PMF model in North China was minor with the largest discrepancy of 6.69%.
KW - Bayesian isotopic mixing model
KW - NO sources
KW - Nitrogen/oxygen isotope
KW - PMF model
UR - https://www.scopus.com/pages/publications/85053030584
U2 - 10.1016/j.envpol.2018.08.026
DO - 10.1016/j.envpol.2018.08.026
M3 - 文章
C2 - 30138830
AN - SCOPUS:85053030584
SN - 0269-7491
VL - 242
SP - 1379
EP - 1386
JO - Environmental Pollution
JF - Environmental Pollution
ER -