Nitrate runoff loss and source apportionment in a typical subtropical agricultural watershed

被引:12
|
作者
Dong, Yue [1 ,2 ,3 ]
Yang, Jin-Ling [1 ,2 ]
Zhao, Xiao-Rui [1 ]
Yang, Shun-Hua [1 ]
Mulder, Jan [3 ]
Dorsch, Peter [3 ]
Zhang, Gan-Lin [1 ,2 ,4 ]
机构
[1] Chinese Acad Sci, State Key Lab Soil & Sustainable Agr, Inst Soil Sci, Nanjing 210008, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100081, Peoples R China
[3] Norwegian Univ Life Sci, Fac Environm Sci & Nat Resource Management, N-1432 As, Norway
[4] Chinese Acad Sci, Key Lab Watershed Geog Sci, Nanjing Inst Geog & Limnol, Nanjing 210008, Peoples R China
基金
中国国家自然科学基金;
关键词
Nitrogen isotopes; Oxygen isotopes; Source identification; Bayesian isotope mixing model; Nitrogen fertilization; Agricultural watershed; LAND-USE; CROPPING SYSTEMS; ISOTOPE FRACTIONATION; N-15-LABELED NITROGEN; SOURCE IDENTIFICATION; GROUND-WATER; DUAL-ISOTOPE; RIVER; SOIL; CHINA;
D O I
10.1007/s11356-021-16935-3
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Nitrate (NO3-) loss and enrichment in water bodies caused by fertilization are a major environmental problem in agricultural areas. However, the quantitative contribution of different NO3- sources, especially chemical fertilizers (CF) and soil organic nitrogen (SON), to NO3- runoff loss remains unclear. In this study, a systematic investigation of NO3- runoff and its sources was conducted in a subtropical agricultural watershed located in Yujiang County, Jiangxi Province, China. A semi-monthly sampling was performed at the inlet and outlet from March 2018 to February 2019. Hydrochemical and dual NO3- isotope ((15) N and O-18) approaches were combined to estimate the NO3- runoff loss and quantify the contribution of different sources with a Bayesian isotope mixing model. Source apportionment by Stable Isotope Analysis in R (SIAR) suggested that NO3- in runoff was mainly derived from nitrification of ammonium (NH4+) mineralized from SON (37-52%) and manure/sewage (M&S) (25-47%), while the contribution of CF was relatively small (14-25%). The contribution of various sources showed seasonal variations, with a greater contribution of CF in the wet growing season (March to August). Compared with the inlet which contributed 37-40% to runoff NO3-, SON contributed more at the outlet (49-52%). Denitrification in the runoff was small and appeared to be confined to the dry season (September to February), with an estimated NO3- loss of 2.73 kg N ha(-1). The net NO3- runoff loss of the watershed was 34.5 kg N ha(-1) yr(-1), accounting for 15% of the annual fertilization rate (229 kg N ha(-1) yr(-1)). Besides M&S (22%), fertilization and remineralization of SON (CF + SON) were the main sources for the NO3- runoff loss (78%), suggesting accelerated nitrification of NH4+ from CF (24%) and SON mineralization (54%). Our study indicates that NO3- runoff loss in subtropical agricultural watersheds is dominated by nonpoint source pollution from fertilization. SON played a more important role than CF. Besides, the contribution of sewage should not be neglected. Our data suggest that a combination of more rational fertilizer N application (CF), better management of SON, and better treatment of domestic sewage could alleviate NO3- pollution in subtropical China.
引用
收藏
页码:20186 / 20199
页数:14
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