滦河流域TN浓度时空变化特征与影响因素分析

Spatiotemporal Distribution Characteristics and Influencing Factors of TN in Luan River Basin

  • 摘要: 水体中氮元素浓度过高是影响河流水环境的重要因素之一. 为深入了解滦河流域TN浓度时空变化特征,本研究基于2018—2022年滦河流域TN浓度逐月监测数据,通过空间聚类分析将该流域划分为源头区、中上游区和下游区,开展TN浓度时空分布特征及变化规律研究;通过探究TN浓度与降雨量、径流量、地下水埋深的关系,分析TN浓度变化的影响因素. 结果表明:①滦河流域TN浓度源头区水质状况良好,TN浓度保持在1.86 mg/L左右;中上游区TN浓度较高,浓度最高断面超过10 mg/L,这与该区域人口聚集、畜禽养殖及农业面源污染等问题有关;下游区受到潘大水库对中上游汇水的调节,TN浓度较中上游区有所下降,稳定在5 mg/L左右. ②滦河流域TN浓度受降雨量影响显著,月降雨量小于250 mm时,TN浓度与降雨量呈较强负相关,呈现TN浓度随降雨量增大而减少的趋势;月降雨量大于250 mm时,土壤中的氮素受到冲刷被释放,河流中TN浓度随降雨量的增大而升高. ③潘大水库的调蓄作用对水库下游的TN浓度影响显著,水库的大量泄水会极大增加河道径流,使水库底层沉积物中的氮素释放,从而增大河流中的TN浓度. ④滦河流域的丘陵地区,地势起伏大,地下水埋深较浅,枯水期地表水会受到地下水的侧向补给,造成地表水NO3-N浓度升高,进而导致TN浓度升高. 研究显示,滦河流域的TN浓度呈现出中上游区>下游区>源头区的趋势,降雨量和潘大水库的调蓄作用对TN浓度的影响显著,丘陵区枯水期地下水补给地表水是造成TN浓度升高的原因之一.

     

    Abstract: High concentration of nitrogen is one of the important factors affecting the river water environment. This paper aims to gain an in-depth understanding of the spatiotemporal variation characteristics of TN concentration in the Luan River Basin. Based on the TN concentration monitoring data in the Luan River Basin during 2018 and 2022, this paper applied spatial cluster analysis, divided the basin into source, upstream and downstream areas, and conducted research on the spatiotemporal distribution characteristics and variation of TN concentration. The influencing factors of TN concentration changes were explained by exploring the relationship between TN concentration and precipitation, runoff and groundwater depth. The results showed that: (1) TN concentration in the source area remained at about 1.86 mg/L, with a relatively low level. The TN nitrogen concentration in the upstream area was highest, with the highest concentration exceeding 10 mg/L, which is closely related to the population concentration, livestock and poultry farming, and agricultural surface pollution in the area. The downstream was regulated by the Panjiakou-Daheiting Reservoir, and the TN concentration was stable at about 5 mg/L. (2) The TN concentration in Luan River Basin was significantly affected by precipitation. When the monthly precipitation was less than 250 mm, TN concentration was strongly negatively correlated with precipitation, showing a decreasing trend of TN concentration as precipitation increased. When the monthly precipitation was greater than 250 mm, the nitrogen in the soil was washed and released, and the TN concentration increased with the increase in precipitation. (3) The regulatory role of the Panjiakou-Daheiting Reservoir significantly affected the reservoir downstream TN concentration. Large releases from reservoirs greatly increased river runoff, which causes the release of nitrogen from the sediment and increases the river TN concentration. (4) The hilly areas of the Luan River Basin has large undulations and shallow groundwater depth, and surface water was recharged laterally by groundwater during dry periods. This resulted in an increase in surface water NO3-N concentration and led to an increase in TN concentration. The study indicated that the TN concentration in the Luan River Basin showed the trend of upstream > downstream > source area trend. The precipitation and the regulation of the reservoir had a significant effect on TN concentration. Groundwater recharge of surface water during dry periods in hilly areas is one of the reasons for the increase in TN concentration.

     

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