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根据1993，1994年蚌湖与吴城修水站水位同步观测数据及1951－1987年该站的水位资料，通过地形调查、对比研究及数学分析，得出结论：典型湿地与鄱阳湖的水位存在高水位一致性、中水位相关性、低水位不相关性，此规律是由湿地地形与鄱阳湖水情所决定；三峡工程运行后湿地不会干涸；湿地水位相对鄱阳湖滞后效应不明显；利用湿地与鄱阳湖的水位关系及其历史水位资料等，可以对湿地的淹露状况进行定量分析。
According to the synchronous observation data of water level between Bangshu and Wuchengxiu water stations in 1993 and 1994 and the water level data of the station from 1951 to 1987, through the topographic survey, comparative study and mathematical analysis, it is concluded that the water level of typical wetlands and Poyang Lake has high water level Consistency, water level correlation and low water level. This law is determined by the wetland topography and the Poyang Lake water regime. The wetland will not dry up after the Three Gorges Project operation. The lag effect of the wetland relative to the Poyang Lake is not obvious. Lake water level and history of the water level data, etc., can be wetland wetlands quantitative analysis.