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Nitrate runoff loss and source apportionment in a typical subtropical agricultural watershed.
- Source :
-
Environmental science and pollution research international [Environ Sci Pollut Res Int] 2022 Mar; Vol. 29 (14), pp. 20186-20199. Date of Electronic Publication: 2021 Nov 02. - Publication Year :
- 2022
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Abstract
- Nitrate (NO <subscript>3</subscript> <superscript>-</superscript> ) loss and enrichment in water bodies caused by fertilization are a major environmental problem in agricultural areas. However, the quantitative contribution of different NO <subscript>3</subscript> <superscript>-</superscript> sources, especially chemical fertilizers (CF) and soil organic nitrogen (SON), to NO <subscript>3</subscript> <superscript>-</superscript> runoff loss remains unclear. In this study, a systematic investigation of NO <subscript>3</subscript> <superscript>-</superscript> 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 NO <subscript>3</subscript> <superscript>-</superscript> isotope ( <superscript>15</superscript>  N and <superscript>18</superscript> O) approaches were combined to estimate the NO <subscript>3</subscript> <superscript>-</superscript> 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 NO <subscript>3</subscript> <superscript>-</superscript> in runoff was mainly derived from nitrification of ammonium (NH <subscript>4</subscript> <superscript>+</superscript> ) 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 NO <subscript>3</subscript> <superscript>-</superscript> , 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 NO <subscript>3</subscript> <superscript>-</superscript> loss of 2.73 kg N ha <superscript>-1</superscript> . The net NO <subscript>3</subscript> <superscript>-</superscript> runoff loss of the watershed was 34.5 kg N ha <superscript>-1</superscript>  yr <superscript>-1</superscript> , accounting for 15% of the annual fertilization rate (229 kg N ha <superscript>-1</superscript>  yr <superscript>-1</superscript> ). Besides M&S (22%), fertilization and remineralization of SON (CF + SON) were the main sources for the NO <subscript>3</subscript> <superscript>-</superscript> runoff loss (78%), suggesting accelerated nitrification of NH <subscript>4</subscript> <superscript>+</superscript> from CF (24%) and SON mineralization (54%). Our study indicates that NO <subscript>3</subscript> <superscript>-</superscript> 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 NO <subscript>3</subscript> <superscript>-</superscript> pollution in subtropical China.<br /> (© 2021. The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature.)
Details
- Language :
- English
- ISSN :
- 1614-7499
- Volume :
- 29
- Issue :
- 14
- Database :
- MEDLINE
- Journal :
- Environmental science and pollution research international
- Publication Type :
- Academic Journal
- Accession number :
- 34725759
- Full Text :
- https://doi.org/10.1007/s11356-021-16935-3