长江流域资源与环境 >> 2025, Vol. 34 >> Issue (4): 803-812.doi: 10.11870/cjlyzyyhj202504009

• 自然资源 • 上一篇    下一篇

乐安河圩区水体碳氮磷浓度及对水文连通的响应

王丹阳1,2,3, 李艳红3, 蒋婕妤4, 汤显强1,2*   

  1. (1.长江科学院流域水环境研究所,湖北 武汉 430010; 2.流域水资源与生态环境科学湖北省重点实验室,湖北 武汉 430010; 3.江西省水利科学院江西省鄱阳湖水资源与环境重点实验室,江西 南昌 330029; 4.湖南省水利水电科学研究院,湖南 长沙 410007)
  • 出版日期:2025-04-20 发布日期:2025-04-29

Concentrations of Water Carbon, Nitrogen, and Phosphorus and Response to Hydrological Connectivity in Polders Along Le’an River

WANG Dan-yang1,2,3, LI Yan-hong1, JIANG Jie-yu4, TANG Xian-qiang2,3   

  1. (1.Jiangxi Province Key Laboratory of Water Resources and Environment of Poyang Lake, Jiangxi Institute of Water Science, Nanchang 330029, China; 2.Basin Water Environmental Department, Changjiang River Scientific Research Institute, Wuhan 430010, China; 3.Key Laboratory of Basin Water Resource and Eco-Environmental Science in Hubei Province, Wuhan 430010, China; 4.Hunan Institute of Water Resources and Hydropower Research, Changsha 410007, China)
  • Online:2025-04-20 Published:2025-04-29

摘要: 圩区拥有沟渠、池塘、稻田等众多水体,是重要的湿地资源,适宜的水体中生源要素浓度对其生态功能发挥至关重要。以鄱阳湖流域乐安河沿岸圩区为例,通过采样测试,明确了圩内外各类水体中溶解态生源要素浓度分布,发现溶解态有机碳(DOC)、氮(DTN)、磷(DTP)呈稻田>池塘>沟渠>外河的空间梯度,平均浓度分别为9.5/13.8/19.0/34.2 mg/L(DOC),0.6/1.1/0.82/8.8 mg/L(DTN),0.016/0.025/0.036/0.12 mg/L(DTP);进一步以换水周期表征各类水体水文连通条件,发现生源要素浓度与水文连通条件有较强相关性,后者最高可以解释前者变化的25.4%,随连通条件改善,换水周期缩短,生源要素停留时间减少,周转加快,浓度下降。综合考虑圩区防洪和用水需求,在不改变现有水系格局的前提下,控制各级涵闸启闭的时机、时长以增强水文连通,同时制定生源要素的浓度和排放标准并配以相应的监督管理措施,是控制圩区生源要素浓度的应有举措。

Abstract: Various waterbodies including ditches, ponds, and paddy fields are important components of  polders wetlands. Maintaining reasonable concentrations of key biogenic elements including carbon, nitrogen and phosphorus in polders is essential for the ecological function of wetlands. Taking the polders along the Le 'an River in Poyang Lake Basin as an example, this study explored the distribution pattern of concentrations of dissolved carbon (DOC), nitrogen (DTN), and phosphorus (DTP) in major waterbodies of polders, through field monitoring and sampling. A quantitative study was also conducted to reveal the effect of hydrological connectivity on element concentrations. All elements were distributed in the hierarchy of paddy field > pond > ditch, with mean concentrations of 9.5/13.8/19.0/34.2 mg/L (DOC),0.6/1.1/0.82/8.8 mg/L (DTN),0.016/0.025/0.036/0.12 mg/L(DTP), respectively. Concentration of biogenic elements was strongly correlated with hydrological connectivity, and the latter could explain up to 25.4% of the change of the concentrations. This finding implied that an improvement of connectivity could shorten the residence time of the elements and accelerate the turnover rates, and consequently resulted in decreased concentrations. The demand of flood control and water supply requires the necessary to control the concentrations of biogenic elements in polders. Therefore, in practice, it is suggested to manage the timing and duration of sluice gate opening/closing in order to restore an improved hydrological connectivity in polders.

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