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鄱阳湖水位变化及其归因量化研究

Quantitative Research on the Water Level Change and Its Attribution of Poyang Lake

  • 摘要: 近年来鄱阳湖枯水期水位屡创新低,导致流域经济社会发展和生态环境保护问题日益突出。为探明鄱阳湖水位变化规律,量化不同影响因素对鄱阳湖水位变化的贡献程度,研究采用Mann-Kendall检验方法和多项式回归分析方法对鄱阳湖水位变化趋势及成因进行量化分析。以星子站和湖口站分别作为鄱阳湖的水位和流量代表站,以九江站作为长江中下游干流代表站,首先选取1981-2021年长江流域和鄱阳湖同期长系列实测数据,通过相关性分析辨识了鄱阳湖代表站星子站水位变化的主要影响因素;进一步采用Mann-Kendall检验方法分析了鄱阳湖水位变化的趋势特征,最后基于水量关系量化了不同影响因素对枯水期鄱阳湖水位变化的贡献度。结果表明:从水量上看鄱阳湖水位变化受九江站和湖口站总水量变化影响较大;三峡建库前1981年开始,鄱阳湖最低水位呈显著下降趋势,建库后正常蓄水期鄱阳湖最低水位较初期蓄水期抬升了0.44 m,表明三峡水库枯水期消落补水调度在一定程度上缓解了鄱阳湖枯期水位下降趋势;蓄水期三峡工程蓄水并非影响鄱阳湖枯水期水位降低的关键因素(贡献度为35.4%),而主要受长江上游、三峡-九江区间来水减少、鄱阳湖流域天然来水减少以及河床下切等综合因素影响(贡献度为64.6%);此外消落期三峡水库补水对鄱阳湖枯期水位抬升有积极作用(贡献度为20%),河床下切、其他来水减少等因素贡献度为-120%。研究可为制定鄱阳湖枯水期低枯水位应对措施,提升湖区水资源与水环境承载力提供科学依据和指引。

     

    Abstract: In recent years,the water level in Poyang Lake has repeatedly reached a record low in dry seasons,which has led to increasingly prominent economic and social development and ecological and environmental protection issues. In order to identify the law of water level changes of Poyang Lake and quantify the degree of contribution of different influencing factors on the changes in the water level of Poyang Lake, this paper uses Mann-Kendall test and polynomial regression analysis methods to quantitatively analyze the change trend of water level of Poyang Lake and its causes. In this paper, Xingzi Station and Hukou Station are taken as the water level and flow representative stations of Poyang Lake respectively, and Jiujiang Station is taken as the representative station of the mainstream of the middle and lower reaches of the Yangtze River. First, the long-term observed data of the Yangtze River Basin and Poyang Lake from 1981 to 2021 are selected for case studies. The main influencing factors of the water level changes of Xingzi Station on the Poyang Lake are identified by correlation analysis.The trend characteristics of the water level of Poyang Lake are analyzed by the Mann-Kendall test method. Finally, the degree of contribution to the changes in the water level of Poyang Lake during the dry season is quantified based on the water volume relationship. The results show that the changes in Poyang Lake′s water level from the perspective of water volume are mainly affected by the total water volume of Jiujiang Station and Hukou Station. In 1981 before the Three Gorges Reservoir was built, the lowest water level of Poyang Lake had shown a significant downward trend. After the reservoir was built, the lowest water level of Poyang Lake in the normal storage period rose by 0.44 m compared with the initial storage period, indicating that the water supply regulation of the Three Gorges Reservoir in the dry season alleviated the downward trend of the water level of Poyang Lake in the dry season to some extent. Impoundment of the Three Gorges Project is not a key factor affecting the decrease in water level in the dry season of Poyang Lake, with a contribution of 35.4%, but is mainly affected by the comprehensive factors such as decreased water and cutting under the river bed, with a contribution of 64.6%. In addition, the water supplement of the Three Gorges Reservoir has a positive effect on the increase in water level of Poyang Lake in the dry season, with a contribution of 20%, and the contribution of factors such as the cutting of the riverbed and the reduction of other incoming water is-120%. The study can provide scientific basis and guidance for formulating countermeasures for low and dry water levels of Poyang Lake in the dry season and improving water resources and water environment carrying capacity of the lake area.

     

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