Triple oxygen isotopic evidence for atmospheric nitrate and its application in source identification for river systems in the Qinghai-Tibetan Plateau

被引:32
|
作者
Xia, Xinghui [1 ]
Li, Siling [1 ]
Wang, Fan [2 ]
Zhang, Sibo [1 ]
Fang, Yunting [3 ]
Li, Jianghanyang [4 ]
Michalski, Greg [4 ]
Zhang, Liwei [1 ]
机构
[1] Beijing Normal Univ, Sch Environm, State Key Lab Water Environm Simulat, Beijing 100875, Peoples R China
[2] Sun Yat Sen Univ, Sch Atmospher Sci, Guangdong Prov Key Lab Climate Change & Nat Disas, Guangzhou 51027, Guangdong, Peoples R China
[3] Chinese Acad Sci, Inst Appl Ecol, 72 Wenhua Rd, Shenyang 110016, Liaoning, Peoples R China
[4] Purdue Univ, Dept Earth & Atmospher Sci, 550 Stadium Mall, W Lafayette, IN 47907 USA
基金
中国国家自然科学基金;
关键词
Nitrate source; Delta O-17; delta N-15; Atmospheric nitrate; The Qinghai-Tibetan Plateau; SIAR; SUSPENDED-SEDIMENT; YELLOW-RIVER; FORMATION PATHWAYS; ALPINE GRASSLAND; CLIMATE-CHANGE; NITROGEN; DENITRIFICATION; NITRIFICATION; PRECIPITATION; DEPOSITION;
D O I
10.1016/j.scitotenv.2019.06.204
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Nitrate source identification in river systems is important for water quality management. Recently, the oxygen isotopic anomaly of nitrate in atmospheric deposition (Delta O-17(atm)) is used to identify unprocessed atmospheric nitrate in river systems to reduce the uncertainty caused by the wide range of delta O-18. In high-elevation regions, such as the Qinghai-Tibetan Plateau (QTP) featured with lower temperature and pressure as well as strong radiation, the Delta O-17(atm) might be different from that in low-elevation regions, but no relevant studies have been reported. In this work, Delta O-17(atm), in the QTP was studied, and the fingerprints of nitrate isotopes in synthetic fertilizer, livestock manure, domestic sewage, and soil organic nitrogen (SON) were identified and used to quantify various source contributions to riverine nitrate in the Yellow River and Changjiang River source regions located in the QTP during 2016-2017. The results showed that the average of Delta O-17(atm) in the QTP was 16.4%, lower than the range (19-30%.) reported for the low-elevation regions. The possible mechanism is decreased O-3 as well as increased hydroxyl and peroxy radical levels in the troposphere caused by the climate condition and ozone valley in the QTP will affect the production pathways of atmospheric nitrate. By combining the sewage discharge data with the output results of the SIAR (stable isotope analysis in R) model based on the stable isotope data, manure was determined to be one of the major sources to riverine nitrate for both rivers. The contributions of various sources to riverine nitrate were 47 +/- 10% for manure, 30 +/- 5% for SON, 10 +/- 4% for atmospheric 9 +/- 2% for synthetic fertilizer, and 4 +/- 0% for sewage in the Yellow River source region. This study indicates that the unique atmospheric conditions in the QTP have led to a lower Delta O-17(atm) value, and atmospheric source makes a considerable contribution to riverine nitrate in the QTP. (C) 2019 Elsevier B.V. All rights reserved.
引用
收藏
页码:270 / 280
页数:11
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