| Issue |
E3S Web Conf.
Volume 715, 2026
2026 2nd International Conference on Eco-environmental Protection, Environmental Monitoring and Remediation (EPEMR 2026)
|
|
|---|---|---|
| Article Number | 01018 | |
| Number of page(s) | 6 | |
| Section | Environmental Monitoring, Assessment and Remediation | |
| DOI | https://doi.org/10.1051/e3sconf/202671501018 | |
| Published online | 03 June 2026 | |
Spatiotemporal Variability of Non-Point Source Pollution and Water Quality Response in a Typical Shallow Lake Basin
Laboratory of Water Disaster Prevention, Nanjing Hydraulic Research Institute, 210029 Nanjing, China
* Corresponding author: This email address is being protected from spambots. You need JavaScript enabled to view it.
Abstract
Shijiu Lake is a typical transboundary shallow lake connected to the Yangtze River in the lower Yangtze region, where water environmental management faces practical challenges due to complex pollution sources and difficulties in cross-jurisdictional coordination. This study systematically analyzed the spatiotemporal variability of non-point source (NPS) pollution loads in the Shijiu Lake basin and investigated the response relationships between major inflowing rivers and lake water quality at monitoring sections. The results indicated that: (1) the total annual total nitrogen(TN) load entering the lake was 2924.20 t and the total annual total phosphorus(TP) load was 109.68 t, of which trans-basin water conveyed through the Zhongliu River accounted for 69% and 67% of the total TN and TP inputs, respectively, representing the dominant source of pollutants entering the lake; (2) high TN load areas were mainly distributed in the eastern zones with dense population and industrial activities and in the southwestern agricultural areas, whereas high TP load areas were concentrated in the northeastern zones with intensive livestock farming and the southwestern agricultural areas; and (3) the Zhongliu River inflow significantly influenced water quality at the Shijiu Lake center, Gaochun, Dangtu, and Bowang monitoring sections, the Xinqiao River primarily affected the Lishui section, and the remaining inflowing rivers had limited influence confined to river-mouth areas.
© The Authors, published by EDP Sciences, 2026
This is an Open Access article distributed under the terms of the Creative Commons Attribution License 4.0, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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