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Chinese Journal of Applied Ecology ›› 2018, Vol. 29 ›› Issue (8): 2658-2666.doi: 10.13287/j.1001-9332.201808.013

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Evaluation and change of Danjiangkou Reservoir dynamic capacity.

LIU Hai1,2,3, WU Jing1, YIN Jie1, WANG Min1, CHEN Xiao-ling4,5*   

  1. 1Faculty of Resources and Environment Science, Hubei University, Wuhan 430062, China;
    2School of Remote Sensing and Information, Wuhan University, Wuhan 430079, China;
    3Jiangxi Province Engineering Research Center of Surveying, Mapping and GeoInformation, Nanchang 330209, China;
    4State Key Laboratory of Information Engineering in Surveying, Mapping and Remote Sensing, Wuhan University, Wuhan 430079, China;
    5Ministry of Education Key Laboratory of Poyang Lake Wetland and Watershed Research, Jiangxi Normal University, Nanchang 330022, China.
  • Received:2017-11-19 Online:2018-08-20 Published:2018-08-20
  • Supported by:

    This work was supported by the Collaborative Innovation Center for Major Ecological Security Issues of Jiangxi Province and Monitoring Implementation (JXS-EW-08), the Hong Lake Water Pollution Prevention and Control Special Fund Project [Hong Lake Ecological Security Investigation and Assessment (Phase ii) and Ecological Environmental Protection Pilot Performance Evaluation] and the Fund of Natural Science Foundation of Hubei University.

Abstract: Dynamics of storage capacity of the Danjiangkou Reservoir have important significance to guarantee water diversion middle route project. Aiming at the problems of complexity in measurement and short-term fluctuation in capacity in Danjiangkou Reservoir, we chose remote sensing data of Landsat series and HJ-1A/B, and DEM data, constructing a new method for extraction of dynamic storage capacity, extracting the monthly dynamic information of reservoir capacity in 2000-2016. We analyzed the factors that caused the dynamic change of storage capacity and its impacts on water diversion. The results showed that, in the past 17 years, the largest reservoir capacity of Danjiangkou was 19.216 billion m3 and the minimum was 7.974 billion m3, with an average of 11.204 billion m3. After the first phase of the middle route of south-to-north water transfer, the storage capacity of Danjiangkou Reservoir had been gradually increased. In terms of the monthly averages, the capacity from May to October increased gradually, from October through December showed fluctuate change, and decreased gradually from December to next May. The cyclical artificial storage and climate change were the driving forces for the changes of the storage capacity. The Danjiangkou Reservoir could meet the need for water transfer under the reasonable dispatching of the reservoir water.