Multiple stable isotopic approaches for tracing nitrate contamination sources: Implications for nitrogen management in complex watersheds

Feifei Wang; Lihua Liu; Wenfeng Xu; Yasong Li; Qizhen Ruan; Wenzhi Cao

doi:10.1016/j.ecoenv.2023.115822

Multiple stable isotopic approaches for tracing nitrate contamination sources: Implications for nitrogen management in complex watersheds

Ecotoxicol Environ Saf. 2024 Jan 1:269:115822. doi: 10.1016/j.ecoenv.2023.115822. Epub 2023 Dec 12.

Authors

Feifei Wang¹, Lihua Liu², Wenfeng Xu², Yasong Li³, Qizhen Ruan¹, Wenzhi Cao⁴

Affiliations

¹ Key Laboratory of the Ministry of Education for Coastal and Wetland Ecosystems, College of Environment and Ecology, Xiamen University, Xiamen, Fujian 361102, China.
² Fujian Xiamen Environmental Monitoring Central Station, Xiamen, Fujian 361022, China.
³ Fujian Provincial Key Laboratory of Water Cycling and EcoGeological Processes, Xiamen 361021, China; Key Laboratory of Groundwater Contamination and Remediation of Hebei Province and China Geological Survey, Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China.
⁴ Key Laboratory of the Ministry of Education for Coastal and Wetland Ecosystems, College of Environment and Ecology, Xiamen University, Xiamen, Fujian 361102, China. Electronic address: wzcao@xmu.edu.cn.

PMID: 38091679
DOI: 10.1016/j.ecoenv.2023.115822

Abstract

Nitrate (NO₃^-) contamination of surface water is a global environmental problem that has serious consequences for watershed ecosystems and endangers human health. It is crucial to identify influences of different sources of NO₃^-, especially the incoming water from upper reaches. A combination of hydrochemistry and multi-isotope tracers (δ¹¹B, δ¹⁵N-NO₃^-, and δ¹⁸O-NO₃^-) were used to determine NO₃^- sources and their transformation the North Jiulong River (NJLR), Southeast China. The findings revealed that NO₃^-, which accounted for an average of 87.1% of dissolved inorganic nitrogen (DIN), was the main chemical form of nitrogen species. The integration of dual stable isotopes of NO₃^-, δ¹¹B, and hydrochemistry showed that NO₃^- was primarily contributed by sewage, soil nitrogen (SN), and ammonium (NH₄⁺) via precipitation or fertilizers. The contributions from the sewage and soil nitrate source were almost equivalent and much higher than those from other sources in the NJLR watershed. The contributions from diverse sources varied seasonally and spatially. Manure and sewage (M&S) were the leading sources in the summer and autumn, accounting for 60.9 ± 8.5% and 47.3 ± 7.9%, respectively. However, NO₃^- fertilizers were the predominant source in the spring and winter. The NO₃^- inflow from upper reaches was proposed as an additional end-member to identify its contribution in the midstream and downstream in this study. The contributions of NO₃^- from the upper reaches were significant sources in the midstream and downstream, accounting for 27.2 ± 17.8% and 42.9 ± 21.9%, respectively. The obvious decline in local NO₃^-contribution shares from midstream to downstream implied structural changes in pollutant sources and regional environmental responsibility. Therefore, tracing nitrate sources and quantifying their contributions is critical for clarifying environmental responsibilities for precise local nitrogen management in watersheds.

Keywords: Bayesian mixing model; Biogeochemical processes; Hydrochemistry; Multiple stable isotopes; Nitrate source; Upper reach inflow.

MeSH terms

Bayes Theorem
China
Ecosystem
Environmental Monitoring
Fertilizers / analysis
Humans
Nitrates / analysis
Nitrogen Isotopes / analysis
Nitrogen* / analysis
Sewage
Soil / chemistry
Water
Water Pollutants, Chemical* / analysis

Substances

Nitrogen
Nitrates
Nitrogen Isotopes
Sewage
Fertilizers
Soil
Water
Water Pollutants, Chemical