三峡水库出水氮磷通量变化及来源解析

    Variation trend and source analysis of nitrogen and phosphorus flux at outlet of Three Gorges Reservoir

    • 摘要: 三峡水库出水氮磷通量对中下游水环境、水生态具有重要影响。为此,研究了1998~2023年三峡水库出水氮磷浓度和通量变化及区域来源特征。结果表明:① 1998~2023年,三峡水库出水总氮浓度和通量皆呈先升后降的趋势。②三峡水库成库前的1998~2002年,三峡水库出水总磷(TP)浓度和通量相对较高且年际波动大。成库后的2006~2023年呈先升后降的趋势,尤其是2019年后下降幅度最大。2021~2023年总磷通量(2.384万t/a)仅为1998~2002年(9.147万t/a)的26%。③三峡水库成库和金沙江下游段梯级水库的建成都使得颗粒态磷(PP)浓度和通量大幅下降。2021~2023年,PP浓度均值(0.016 mg/L)仅为1998~2002年(0.120 mg/L)的13%,PP年通量(0.716万t/a)仅为1998~2002年(6.635万t/a)的11%。三峡水库出水中的磷已由成库前颗粒态为主转变为目前溶解态为主。④三峡水库出水溶解态磷(DP)浓度和年通量在2014年达到峰值(0.116 mg/L,4.757万t/a),之后显著下降。⑤三峡水库出水TP、PP、DP浓度和通量皆为丰水期显著高于枯水期。总氮通量亦为丰水期显著高于枯水期,总氮浓度季节变化程度小于总磷。⑥氮磷年通量与年径流量波动节律具有一定类似性。⑦三峡水库氮磷负荷主要来源于长江上游,其次是嘉陵江和乌江。三峡坝区茅坪溪和高家溪两条支流氮磷污染仍然严重,建议进行小流域综合治理。

       

      Abstract: The nitrogen and phosphorus flux from the Three Gorges Reservoir (TGR) has a significant impact on the water environment and aquatic ecology in the middle and lower reaches.The changes in nitrogen and phosphorus concentration and flux in the effluent of the Three Gorges Reservoir from 1998 to 2023 as well as the regional source characteristics were studied.The results indicated that: ① From 1998 to 2023, the total nitrogen (TN) concentration and flux in the effluent of TGR showed a trend of first increasing and then decreasing.② From 1998 to 2002 (the pre-TGR operation period), the interannual fluctuations in total phosphorus (TP) concentration and flux were stronger than those in TN, and the concentration and flux of TP in the effluent of TGR were relatively high and fluctuated greatly between years.From 2006 to 2023, they showed a trend of first rising and then falling, especially after 2019 the decrease was more significant.The TP annual flux in 2021~2023 (23, 840 t/a) was only 26% of that in 1998~2002 (91, 470 t/a).③ The construction of TGR and the cascade reservoirs in the lower reaches of the Jinsha River resulted in a significant decrease in the concentration and flux of particulate phosphorus (PP).From 2021 to 2023, the average concentration of PP (0.016 mg/L) was only 13% of that in the period 1998~2002 (0.120 mg/L), and the annual flux of PP (0.716 million t/a) was only 11% of that in the period 1998~2002 (6.635 million t/a).The phosphorus in the effluent of TGR has been transformed from a mainly particulate state before reservoir formation to a mainly dissolved state at present.④ The concentration and annual flux of dissolved phosphorus (DP) in the effluent of TGR reached their peak in 2014 (0.116 mg/L, 475, 700 t/a), and then significantly decreased.⑤ The concentrations and fluxes of TP, PP and DP in the effluent of TGR were significantly higher during wet seasons than that during dry seasons.The TN flux was significantly higher during wet seasons than that during dry seasons, and the seasonal variation of TN concentration was less than that of TP.⑥ The fluctuation rhythm of annual N and P flux was similar to that of annual runoff, but not completely consistent yet.⑦ The N and P load in TGR mainly comes from the upper reaches of the Changjiang River, followed by the Jialing River and the Wujiang River.The N and P pollution in two tributaries of Maoping Creek and Gaojia Creek at downstream of the TGR area is still severe, so it is recommended to carry out small-scale watershed system pollution control.

       

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