长江流域资源与环境 >> 2025, Vol. 34 >> Issue (05): 1027-.doi: 10.11870/cjlyzyyhj202505009

• 自然资源 • 上一篇    下一篇

基于湿润程度的水位调控对鄱阳湖湿地耗水量的影响研究

彭佳雯1,贾忠华1,潘延鑫2,刘文龙1,陆培榕1,罗纨1*   

  1. (1. 扬州大学水利科学与工程学院,江苏 扬州 225009; 2. 南昌工程学院水土保持学院,江西 南昌 330099)

  • 出版日期:2025-05-20 发布日期:2025-05-22

Effect of Humidity-Based Water Level Regulation on Water Consumption of Poyang Lake Wetland

PENG Jia-wen1 ,JIA Zhong-hua1 ,PAN Yan-xin2 ,LIU Wen-long1 ,LU Pei-rong1 ,LUO Wan1#br#   


  1. (1. College of Hydraulic Science and Engineering , Yangzhou University , Yangzhou 2225009 , China;2. School of Resources and Environmental Sciences , Nanchang Institute of Technology , Nanchang 330099 , China)
  • Online:2025-05-20 Published:2025-05-22

摘要:  鄱阳湖流域持续加重的季节性干旱引发了一系列的湿地生态环境问题,解决途径之一是通过水位调控措施适时改善湖区内的湿润状况。为了确定水位调节对湿地净耗水量的影响,首先针对不同湿润目标,根据“调节水位-起调时间-持续时长”3个参数制定调节方案,然后根据水面和不同地下水埋深将整个湖区划分为不同的湿润区,分区计算对应的湿地面积及净耗水量变化。针对不同湿润年份(平均、干旱、湿润),调节方案包括3个调节水位(13、11与15 m),3个开始时间(自每年第1、280、320 d)及3个持续时间(90、40、40 d)。结果显示,与无调节本底情形比较,不同方案下的平均、干旱、湿润年湿地净耗水增量分别为1.48~4.12、1.49~3.04、1.46~3.15亿m3。虽然耗水增量相对于湿地总入流量(1 500亿m3)占比很低,分别只占0.10%~0.27%、0.10%~0.20%、0.10%~0.21%,但是相对于湿地目前的入流净消耗量(20亿m3),占比达到了7.42%~20.59%、7.42%~15.17%、7.30%~15.73%,影响显著。因此,在制定鄱阳湖湿地生态水位调控方案中,确定湖区净耗水量的变化,可以实现更精准的水资源调配。

Abstract: The increasingly frequent seasonal droughts in the Poyang Lake Basin have caused a series of ecological and environmental problems. One solution is to timely improve the humid conditions in the lake area through water level regulation measures. In order to determine the impact of regulation on the net water consumption of wetlands, this paper firstly defined the regulation scheme using three parameters: ‘regulation water level- start time- duration’ based on different wetting objectives. Then, the entire lake area was divided into different wet zones according to the water surface and different groundwater depths, and the corresponding wetland area and net water consumption changes were calculated for different zones. The regulation schemes included three controlled water levels (13, 11, and 15 m) for different humid years (average, dry, humid), three start times (from the 1st, 280 th, and 320 th day of each year), and three duration times (90, 40, and 40 days). The results showed that, compared with the unregulated background situation, net water consumption increments of wetlands in average, dry, and humid years under different schemes were 1.48-4.12, 1.49-3.04, and 1.46-3.15 ×108 m3, respectively. Although the water consumption increment was very low (0.10%-0.27%, 0.10%-0.20%, and 0.10%-0.21%) compared with the total wetland inflow (150 billion m3), they were significant compared to the current net inflow consumption of the wetland (2 billion m3), which was in the range of 7.42%-20.59%, 7.42%-15.17%, and 7.30%-15.73%. This study indicated that considering the changes in net water consumption was essential in proposing the proper ecological water level of Poyang Lake. Outcomes of this study provide technical support for a more rational water resource allocation.

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