4.7 Article

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

Journal

ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH
Volume 29, Issue 14, Pages 20186-20199

Publisher

SPRINGER HEIDELBERG
DOI: 10.1007/s11356-021-16935-3

Keywords

Nitrogen isotopes; Oxygen isotopes; Source identification; Bayesian isotope mixing model; Nitrogen fertilization; Agricultural watershed

Funding

  1. National Natural Science Foundation of China [41571130051, 41877010, 41771251]
  2. University of Chinese Academy of Sciences (UCAS)

Ask authors/readers for more resources

The study revealed that the loss of NO3- in subtropical agricultural watersheds is primarily caused by nonpoint source pollution from fertilization, with soil organic nitrogen (SON) playing a more significant role than chemical fertilizers (CF). It also highlighted the importance of considering the contribution of sewage in NO3- pollution mitigation strategies.
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.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available