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鄱阳湖流域水沙变化及出湖水沙模拟研究

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自20世纪50年代以来,鄱阳湖流域气候发生显著变化,人类活动日益频繁,降水、产流能力和产沙能力都发生了明显变化.基于鄱阳湖流域"五河"入湖控制站以及湖口水文站数据,运用Mann-Kendall检验法和双累积曲线法确定了年输沙量突变时间点,再利用累积量斜率变化分析法量化降水、产流能力和产沙能力对鄱阳湖入湖沙量的影响;在此基础上,提出了变分模态分解、LSTM神经网络和完全逐步抽样技术等多方法耦合的水沙模拟模型及其评价方法,并建立了研究区域鄱阳湖湖口站水沙模拟模型.研究结果表明:不论是"五河"入湖沙量变化,还是湖区泥沙淤积量变化,以降水变化为代表的气候变化因素对其影响较小,主要影响还是来自人类活动因素;但在具体的变化规律上却存在差异,人类活动对入湖沙量的贡献率呈上升趋势,但对同期鄱阳湖湖区淤积沙量的影响贡献率则呈现先降后升的趋势.水沙模拟分析表明,湖口站出湖月径流量、出湖月输沙量的模拟过程与实测过程较为吻合,取得了较高模拟精度,湖口、星子站水位对模拟精度的提升贡献较小.
Study on water-sediment variation in Poyang Lake Basin and simulation of water-sediment out of Lake
Since the 1950s,the climate of Poyang Lake Basin has changed,human activities have become increasingly frequent,precipitation,runoff capacity and sediment yield capacity have changed significantly.Based on the data of the control stations for"five rivers"entering the lake and the Hukou hydrological station in the lake controlling water and sediment out of the lake,the Mann-Kendall test method and the double cumulative curve method were used to determine the time point of the annual sediment load mutation,and then the cumulative slope variation analysis method was used to quantify the influence of precipitation,runoff yield capacity and sediment yield capacity on the sediment load of Poyang Lake.On this basis,a multi-method coupling water and sediment simulation model based on variational mode decomposition,LSTM neural network and complete stepwise sampling technique and its evaluation method were proposed,and a specific water-sediment simulation model for the Hukou Station was established.The results show that the climate change factors represented by precipitation change have little effect on the change of sediment discharge into the lake or the change of sediment deposition in the lake area.The main influence is from the human ac-tivity factors.However,the specific influences from human activity are diverse.The contribution rate of human activities to the a-mount of sediment entering the lake is on the rise,but the contribution rate to the amount of sediment deposited in the Poyang Lake area during the same period shows a firstly decreasing then increasing trend.The water-sediment simulation analysis shows that the simulation process of monthly runoff and sediment discharge at Hukou Station was in good agreement with the measured process,and high simulation accuracy was obtained.The water levels of Hukou and Xingzi Stations have little contribution to the improvement of simulation accuracy.

water-sediment variationwater-sediment simulationattributional analysisPoyang Lake

香天元、孙思瑞、王超、吴绍飞

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长江水利委员会 水文局,湖北 武汉 430010

长江水利委员会水文局 长江中游水文水资源勘测局,湖北 武汉 430010

南昌工程学院,江西 南昌 330099

水沙变化 水沙模拟 归因分析 鄱阳湖

长江科学院开放研究基金资助项目国家自然科学基金长江水科学研究联合基金项目国家自然科学基金长江水科学研究联合基金项目长江水利委员会水文局科技创新基金项目

CKWV2021886/KYU2240224U2240206SWJ-CJX23Z08

2024

人民长江
水利部长江水利委员会

人民长江

CSTPCD北大核心
影响因子:0.451
ISSN:1001-4179
年,卷(期):2024.55(3)
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