Isotopic constraints on the formation pathways and sources of atmospheric nitrate in the Mt. Everest region

被引:9
|
作者
Wang, Kun [1 ,2 ,4 ]
Hattori, Shohei [2 ]
Kang, Shichang [1 ,3 ,4 ]
Lin, Mang [2 ,5 ]
Yoshida, Naohiro [2 ,6 ]
机构
[1] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Cryospher Sci, Lanzhou 730000, Peoples R China
[2] Tokyo Inst Technol, Sch Mat & Chem Technol, Dept Chem Sci & Engn, Midori Ku, 4259 Nagatsuta Cho, Yokohama, Kanagawa 2268502, Japan
[3] CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
[4] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[5] Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China
[6] Tokyo Inst Technol, Earth Life Sci Inst, Meguro Ku, Tokyo 1528551, Japan
基金
中国国家自然科学基金;
关键词
Atmospheric nitrate; the Mt. Everest; Isotope; Oxidation pathways; NOx source; TIBETAN PLATEAU; TRIPLE OXYGEN; SURFACE OZONE; BLACK CARBON; THEORETICAL CALCULATION; FRACTIONATION FACTORS; NITROGEN ISOTOPES; 1ST MEASUREMENTS; DUMONT DURVILLE; GLOBAL-MODEL;
D O I
10.1016/j.envpol.2020.115274
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Inorganic particulate nitrate (p-NO3-), gaseous nitric acid (HNO3(g)) and nitrogen oxides (NOx = NO + NO2), as main atmospheric pollutants, have detrimental effects on human health and aquatic/terrestrial ecosystems. Referred to as the 'Third Pole' and the 'Water Tower of Asia', the Tibetan Plateau (TP) has attracted wide attention on its environmental changes. Here, we evaluated the oxidation processes of atmospheric nitrate as well as traced its potential sources by analyzing the isotopic compositions of nitrate (delta N-15, delta O-18, and Delta O-17) in the aerosols collected from the Mt. Everest region during April to September 2018. Over the entire sampling campaigns, the average of delta N-15(NO3-), delta O-18(NO3-), and Delta O-17(NO3-) was -5.1 +/- 2.3 parts per thousand, 66.7 +/- 10.2 parts per thousand, and 24.1 +/- 3.9 parts per thousand, respectively. The seasonal variation in Delta O-17(NO3-) indicates the relative importance of O-3 and HO2/RO2/OH in NOx oxidation processes among different seasons. A significant correlation between NO3- and Ca2+ and frequent dust storms in the Mt. Everest region indicate that initially, the atmospheric nitrate in this region might have undergone a process of settling; subsequently, it got re-suspended in the dust. Compared with the Delta O-17(NO3-) values in the northern TP, our observed significantly higher values suggest that spatial variations in atmospheric Delta O-17(NO3-) exist within the TP, and this might result from the spatial variations of the atmospheric O-3 levels, especially the stratospheric O-3, over the TP. The observed delta N-15(NO3-) values predicted remarkably low delta N-15 values in the NOx of the sources and the N isotopic fractionation plays a crucial role in the seasonal changes of delta N-15(NO3-). Combined with the results from the backward trajectory analysis of air mass, we suggest that the vehicle exhausts and agricultural activities in South Asia play a dominant role in determining the nitrate levels in the Mt. Everest region. (c) 2020 Elsevier Ltd. All rights reserved.
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页数:12
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