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Spatio-temporal Response of Water Level in Poyang Lake to Runoff Change of Fiver Rivers
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Pei-pei ZHANG1, Tian-lin ZUO2, Hui-chao DAI3, Jing-qiao MAO1
Water Resources and Power | 2023, 41(2) : 19 - 22
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Water Resources and Power | 2023, 41(2): 19-22
HYDROLOGY, WATER RESOURCES AND ENVIRONMENT
Spatio-temporal Response of Water Level in Poyang Lake to Runoff Change of Fiver Rivers
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Pei-pei ZHANG1, Tian-lin ZUO2, Hui-chao DAI3, Jing-qiao MAO1
Affiliations
  • 1.College of Water Conservancy and Hydropower Engineering, Hohai University, Nanjing 210098, China
  • 2.PowerChina Beijing Engineering Corporation LTD, Beijing 100024, China
  • 3.China Three Gorges Corporation, Wuhan 430010, China
Published: 2023-02-25 doi: 10.20040/j.cnki.1000-7709.2023.20221394
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The water level of Poyang Lake is affected by both the Yangtze River mainstream and the Fiver Rivers (namely, Ganjiang River, Fuhe River, Xinjiang River, Raohe River and Xiushui River) in the lake basin. The runoff of the Five Rivers is the main inflow of Poyang Lake. In order to explore the temporal and spatial impact of the Five Rivers on the water level of Poyang Lake, the response of Poyang Lake level variation to the runoff change of the Five Rivers was quantitatively studied by data-driven simulation and sensitivity analysis. Firstly, the lake level prediction model was established by combining PSO-GA algorithm and support vector regression (SVR) technology. The temporal sensitivity of water level of Poyang Lake to runoff change of the Five Rivers was simulated. Then, based on this model, the spatial distribution characteristics of water level response of Poyang Lake to runoff change of the Five Rivers were studied using continuous model simulation. The results show that the most sensitive period that Poyang Lake level response to the runoff change of the Five Rivers is from May to July, especially in May. In terms of spatial distribution, water level in the middle part of Poyang Lake is most sensitive to the runoff change of the Five Rivers. For instance, based on the data in May 2010, when the runoff of the Five Rivers was increased by 40%, water level at Duchang station was averagely increased by 1.16 m within one week; Average water level increased at Xingzi station and Hukou station in the north lake area was 1.15 m and 1.03 m, respectively, and that at both Tangyin station and Kangshan station in the south lake area was 0.97 m. This study clarified the temporal and spatial response characteristics of water level of Poyang Lake to runoff of the Five Rivers, and provides scientific basis for water resources management and water projects optimization in the Poyang Lake basin.

Poyang Lake  /  water level prediction  /  inflow of five rivers  /  spatiotemporal characteristics  /  response relationship
Pei-pei ZHANG, Tian-lin ZUO, Hui-chao DAI, Jing-qiao MAO. Spatio-temporal Response of Water Level in Poyang Lake to Runoff Change of Fiver Rivers[J]. Water Resources and Power, 2023 , 41 (2) : 19 -22 . DOI: 10.20040/j.cnki.1000-7709.2023.20221394
Year 2023 volume 41 Issue 2
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Article Info
doi: 10.20040/j.cnki.1000-7709.2023.20221394
  • Receive Date:2022-07-09
  • Online Date:2026-01-27
  • Published:2023-02-25
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History
  • Received:2022-07-09
  • Revised:2022-08-09
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Affiliations
    1.College of Water Conservancy and Hydropower Engineering, Hohai University, Nanjing 210098, China
    2.PowerChina Beijing Engineering Corporation LTD, Beijing 100024, China
    3.China Three Gorges Corporation, Wuhan 430010, China
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表12种不同金属材料的力学参数

Family
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Number of
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种数
Number of
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种数
Number of
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鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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