平潭及闽江口水资源配置工程沿线径流演变规律

    Runoff evolution patterns along Pingtan and Minjiang River Estuary Water Resources Allocation Project

    • 摘要: 平潭及闽江口水资源配置(“一闸三线”)工程沿程水源的径流演变规律分析,对于优化福建省水资源空间均衡配置具有重大意义。基于工程沿线五大水源(永泰站、竹岐站、三溪口水库、东张水库、三十六脚湖水库)近60余年的长系列径流资料,综合运用Mann-Kendall趋势检验、Pettitt突变检测、小波分析、集中度和集中期分析等方法系统揭示了水源区径流的年际和年内演变规律,并基于Copula函数分析水源组合间的丰枯遭遇特性。结果表明:①在年际变化方面,永泰站全年及汛期径流呈显著下降趋势,并在2000年发生显著突变,竹岐站非汛期径流显著增加且径流突变点为1981年; ②周期分析表明各水源年径流与汛期径流存在8~18 a的主周期,非汛期为5~13 a; ③在年内分配方面,各水源年内径流集中于5~9月,集中度为0.40~0.53,分配较不均匀,其中永泰站和竹岐站的径流集中程度呈递减趋势,未来径流集中时间有推迟趋势; ④在丰枯遭遇方面,各水源径流间有较好的丰枯补偿规律,利于开展多水源联合调度,丰枯同步概率为0.47~0.65,丰枯异步概率为0.35~0.53。研究成果可为跨流域调水工程的多水源协同调度策略制定提供科学依据。

       

      Abstract: Analysis on the runoff evolution patterns of water sources along the Pingtan and the Minjiang River Estuary Water Resources Allocation Project (the "One Gate Three Lines" Project) is of great significance for optimizing the spatially balanced allocation of water resources in Fujian Province.Based on long-term runoff data spanning six decades from five major water sources along the project route (Yongtai Station, Zhuqi Station, Sanxikou Reservoir, Dongliu Reservoir, and Sanshiliujiao Lake), we employed the Mann-Kendall rank correlation test, Pettitt change-point detection, wavelet analysis, concentration degree (CD), and concentration period (CP) to systematically characterize inter-annual and intra-annual runoff distribution patterns among these water sources.In addition, a Copula function was used to analyze the wetness-dryness encounter characteristics among water sources.The results showed that: ① in terms of inter-annual variations, the annual and flood-season runoff at Yongtai Station exhibited a significant decreasing trend and experienced a significant abrupt change in 2000;whereas the non-flood-season runoff at Zhuqi Station showed a significant increasing trend, with its abrupt change point identified in 1981;② wavelet analysis revealed dominant periodicities of 8~18 years for both annual and flood-season runoff across all water sources, while non-flood-season runoff exhibited primary cycles spanning 5~13 years; ③ regarding intra-annual distribution, runoff at all water sources was concentrated from May to September, with CD values ranging from 0.40 to 0.53, indicating a relatively uneven distribution.Notably, the runoff CD at Yongtai and Zhuqi Stations exhibited a declining trend, while the CP showed a potential trend toward delay; ④ regarding wetness-dryness encounter characteristics, significant hydrological compensation patterns were observed among different water sources, which provide favorable conditions for implementing multi-source joint operations, with synchronous occurrence probabilities ranging from 0.47 to 0.65 and asynchronous probabilities ranging from 0.35 to 0.53.These findings can provide a scientific foundation for formulating coordinated multi-source operation strategies in trans-basin water transfer projects.

       

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