长江流域资源与环境 >> 2021, Vol. 30 >> Issue (10): 2471-2481.doi: 10.11870/cjlyzyyhj202110015

• 生态环境 • 上一篇    下一篇

鄂西长江喀斯特小流域氮磷输出特征

梁爽1,陈敏1,2*,肖尚斌1,2,罗怡君3,虞之锋1,许浩霆1   

  1. (1. 三峡大学水利与环境学院,湖北 宜昌 443002;2. 三峡库区生态环境教育部工程研究中心 湖北 宜昌 443002;3.长江勘测规划设计院,湖北 武汉 430000)
  • 出版日期:2021-10-20 发布日期:2021-11-05

Characteristics of Nitrogen and Phosphorus Output in the Small Karst Watershed of the Yangtze River in Western Hubei

LIANG Shuang1, CHEN Min1,2, XIAO Shang-bin1,2, LUO Yi-jun3, YU Zhi-feng1, XU Hao-ting1   

  1. (1.College of Hydraulic & Environmental Engineering, China Three Gorges University, Yichang 443002, China; 2.Engineering Research Center of Eco-environment in Three Gorges Reservoir Region, Yichang 443002, China; 3.Changjiang Institute of Survey, Planning, Design and Research, Wuhan 430000, China)
  • Online:2021-10-20 Published:2021-11-05

摘要:  以鄂西长江中上游分界处的喀斯特小流域下牢溪为研究对象,于2019年对河道内15个观测点进行了间隔半月的现场水环境因子监测、水样采集和室内营养盐分析,以探讨河流氮磷浓度及输出负荷的时空变化特征。结果表明:下牢溪总氮和总磷浓度分别为1.46±0.05和0.02±0.04 mg/L,普遍低于长江流域内其他河流。氮素浓度呈现春夏高、秋冬低的年内变化特征,磷素浓度总体表现为丰水期高于枯水期,与降雨密切相关。河流上游氮磷浓度均较高,受控制流域内农业活动影响较大。流域氮素浓度空间分布差异性较为明显,磷素浓度对河流附近人为活动及生活污染的响应敏感。流域中全年氮磷输出负荷分别为 26.57和0.25 t,主要集中在春、夏季,贡献了全年氮负荷的82.0%、磷负荷的83.9%。硝氮和溶解态总磷分别为最主要的氮磷流失形态。夏季受降雨冲刷影响,颗粒态磷流失负荷占总磷负荷的比重显著高于其他季节。

Abstract: This study focuses on a small karst watershed named Xialaoxi in the junction zone of the middle and upper reaches of the Yangtze River in western Hubei, and in-site measurements of aquatic environmental factors, water sample collection and indoor experiments were conducted biweekly in 2019 for 15 observation sites, to investigate the spatial and temporal patterns of nitrogen and phosphorus concentrations and output loads from the watershed. The results showed that the total nitrogen and total phosphorus concentrations in Xialaoxi were (1.46±0.05) mg/L and (0.02±0.04) mg/L, respectively, which were generally lower than those in other rivers of the Yangtze River Basin. The nitrogen concentration was higher in spring and summer while lower in autumn and winter, and the phosphorus concentration was higher in wet season than that in dry season, which was closely related to rainfall. Nitrogen and phosphorus concentrations were higher in the upper reaches of the river, which were greatly affected by agricultural activities in the controlled watershed. There was significant spatial heterogeneity of nitrogen concentrations within the watershed. Phosphate concentrations were sensitive to human activities and domestic pollution near the river. The annual nitrogen and phosphorus loads of the watershed were 26.57 t and 0.25 t, respectively. They were mainly concentrated in spring and summer, contributing 82.0% of the annual nitrogen load and 83.9% of the annual phosphorus load separately. Nitrate and dissolved total phosphorus were the main forms of nitrogen and phosphorus loads, respectively. The proportion of particle phosphorus load to total phosphorus load in summer was significantly higher than that in other seasons due to rainfall erosion.

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