The binary structure of the floodplain in the reaches of the Yangtze River is obvious and has unique hydrogeological features. In this paper, the hydrogeological survey of the floodplain area is carried out. It is found that the permeability coefficient of the floodplain area is gradually increasing from top to down, and is larger than that of the similar layer in other areas. The horizontal and vertical permeability coefficients are not much different. This hydrological survey results of this paper provide a certain reference for similar dewatering projects in the floodplain area of the lower reaches of the Yangtze River.
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