State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan, 430072, China.
State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing, 100012, China.
Environ Sci Pollut Res Int. 2022 Aug;29(37):56739-56749. doi: 10.1007/s11356-022-19787-7. Epub 2022 Mar 26.
The impoundment of the Three Gorges Reservoir (TGR) and upstream cascade reservoirs (UCRs) has altered the hydrologic regime, with inevitable effects on phosphorus transport processes in the TGR. In order to investigate the effects of impoundment, long-term monitoring data of flow rate, suspended sediment (SS), and phosphorus fractions of six stations in the TGR basin were collected and divided into three periods, period 1 (P1) (1985-2002), period 2 (P2) (2003-2012), and period 3 (P3) (2013-2017), based on the periodic impoundment time. The results indicated that the impoundment of the TGR and UCRs considerably decreased the SS concentration. Efficient sediment interception by the UCRs led to a dramatic decline in the concentrations of total phosphorus (TP) and particulate phosphorus (PP) in the mainstream, while the total dissolved phosphorus (TDP) showed a general increasing trend from 2004 to 2017. Different phosphorus fractions in the mainstream exhibited seasonal variations; among them, the concentrations of TP and PP were highest in the wet season, while the highest TDP concentration occurred in the dry season. Further analysis indicated that the seasonal distribution of TP was significantly homogenized in P3. Additionally, the SS concentration was positively correlated with the concentrations of TP and PP in the mainstream, while the correlations in P3 were significantly lower than that in P2. The findings can provide a scientific reference for future investigations dedicated to the long-term effects of the UCRs on the eco-environment in the TGR as well as the downstream.
三峡水库(TGR)和上游梯级水库(UCR)的蓄水改变了水文情势,对 TGR 磷输移过程产生了不可避免的影响。为了研究蓄水的影响,收集了 TGR 流域六个站点的流量、悬浮物(SS)和磷形态的长期监测数据,并根据周期性蓄水时间将其分为三个时期,第一时期(P1)(1985-2002 年)、第二时期(P2)(2003-2012 年)和第三时期(P3)(2013-2017 年)。结果表明,TGR 和 UCR 的蓄水使 SS 浓度显著降低。UCR 的有效拦截作用导致主流总磷(TP)和颗粒态磷(PP)浓度急剧下降,而总溶解磷(TDP)则从 2004 年到 2017 年呈总体上升趋势。主流中不同的磷形态表现出季节性变化;其中,TP 和 PP 的浓度在雨季最高,而 TDP 的浓度在旱季最高。进一步分析表明,P3 中 TP 的季节分布明显均匀化。此外,SS 浓度与主流中 TP 和 PP 的浓度呈正相关,而 P3 中的相关性明显低于 P2。研究结果可为未来研究 UCR 对 TGR 及下游生态环境的长期影响提供科学参考。