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在当前平原地区骨干河道还不可能全面提高排涝标准的情况下,田间治涝工程修建后,骨干河道的洪峰流量及洪水总量将会发生怎样的变化,是一个十分重要的问题。我们根据鲁西北地区的赵牛河水系及鲁西南地区
Under the current situation that it is not possible for the key rivers in the plain area to raise the water drainage standards in an all-round way, how the peak flow and the total flood volume of the backbone rivers will change after the construction of the field waterlogging prevention project is a very important issue. We are based on the northwest Shandong Zhao Niuhe river system and southwestern areas