Abstract

Under the influence of human activities and the rapid development of industry and agriculture, atmospheric nitrate (NO − 3 ) pollution is becoming increasingly serious and has become an environmental problem worldwide. The stable isotopic composition of atmospheric NO − 3 (δ 15 N, δ 18 O, and Δ 17 O) can provide a strong basis for understanding the atmospheric nitrogen cycle to effectively control atmospheric NO x pollution. In this work, the δ 15 N values associated with different sources of atmospheric NO − 3 , the seasonal variation characteristics of δ 15 N-NO − 3 , and the main influencing factors are reviewed. The δ 18 O and Δ 17 O values of different oxidants in the atmosphere and the spatiotemporal distribution characteristics and possible influencing factors of the δ 18 O and Δ 17 O values ​​of atmospheric NO − 3 are summarised. In addition, key advances in NO − 3 isotopic analysis technique is reviewed. Based on previous work, it is suggested that more attention should be given to the oxidative formation mechanism of NO − 3 (spatio-temporal differences in the isotopic compositions of different types of oxidants), the δ 15 N composition of different NO x sources, and the processes of formation, transport, depositional/chemical loss ofatmospheric NO − 3 with the help of observation and chemical models.

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