RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN >> 2016, Vol. 25 >> Issue (12): 1894-1902.doi: 10.11870/cjlyzyyhj201612013

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DYNAMICS OF GROUNDWATER LEVEL AND LATERALLY HYDRAULIC CONNECTION BETWEEN LAKE AND GROUNDWATER IN POYANG LAKE AREA

LI Yun-liang1, ZHANG Xiao-lin2, ZHAO Gui-zhang3, YAO Jing1, ZHANG Qi1,4   

  1. 1. Key Laboratory of Watershed Geographic Science, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China;
    2. University of Chinese Academy of Sciences, Beijing 100049, China;
    3. North China University of Water Resources and Electric Power, Zhengzhou 450045, China;
    4. Key Laboratory of Poyang Lake Wetland and Watershed Research, Ministry of Education, Jiangxi Normal University, Nanchang 330022, China
  • Received:2016-05-04 Revised:2016-07-19 Online:2016-12-20
  • Supported by:
    National Basic Research Program of China(2012CB417003);National Natural Science Foundation of China(41401031);Collaborative Innovation Center for Major Ecological Security Issues of Jiangxi Province and Monitoring Implementation(JXS-EW-00);Key Laboratory of Watershed Geographic Science,Nanjing Institute of Geography and Limnology,Chinese Academy of Sciences(WSG2015004)

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Abstract: Study of the interactions and exchange fluxes between groundwater and lake water is an important prerequisite for understanding and preserving groundwater-lake water ecosystems. The objectives of this paper are to combine observed lake water level and groundwater level (during 2014) and statistical methods to analyze the dynamics of groundwater level response to the lake water level changes around Poyang Lake. Additionally, we further explored the laterally hydraulic connection between lake water and groundwater. Statistical results showed that the groundwater depth varies from -8.1 to -0.1 m in different delta wetlands of the Poyang Lake, and the lake water and groundwater had a fully hydraulic connection during the high lake water level periods (June-September). In addition, the variations of groundwater level in the typical delta wetlands were similar to those of the lake water level, suggesting a close hydraulic connection between the two. Statistical results also showed that the groundwater depth has a range of -10~-2.2 m in different lakeshores around the lake. Although the groundwater level in different lakeshores and the lake water level are obviously different at a daily scale in terms of the temporal dynamics, they appear to exhibit similar variation pattern at a monthly scale. The wavelet analysis demonstrated that both the lake water level and the groundwater level in different areas were of obvious 60 days significant oscillation periods with the positive correlations. This result indicates that, in generally, Poyang Lake water has a close hydraulic connection with the groundwater of different delta wetlands, but a relatively weak hydraulic connection between the two depended on the local water regime. The outcomes of this study will not only help improve our understanding of groundwater-lake water dynamics in the Poyang Lake area, but also can provide scientific basis for future groundwater management and water resources assessment.

Key words: lake water level, groundwater level, hydraulic connection, wavelet analysis, Poyang Lake

CLC Number: 

  • P641.6
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