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1935年的夏天,当滂沱大雨结束了一段漫长的干旱时,华北大平原上的农民们欢欣鼓舞。但是大雨也带来了危险,持续的大雨造成黄河水位上涨,由于黄河在此时已经成为地上河——在黄河下游淤积了河水从中游黄土高原上携带下来的大量泥沙,以至河床提高,造成大坝内侧水面高于大坝外侧的平原地面。每一年,黄河河道里的水位都会比前一年升高,有时,水位高度甚至超出周围平原地面达10米。因此一旦发生溃堤,后果不堪设想。在7月中旬的时候,黄河的堤坝溃决了,洪水淹
In the summer of 1935, peasants in the Great Plains of North China rejoiced when the torrential rains ended a long drought. However, heavy rains also brought danger. As a result of continuous heavy rains, the Yellow River water level rose. As the Yellow River has now become an aboveground river, silt deposits in the lower reaches of the Yellow River caused large amounts of sediment from the Loess Plateau in the middle reaches of the Yellow River and increased the riverbed, resulting in The water level inside the dam is higher than the ground level outside the dam. Each year, the water level in the Yellow River rises from the previous year, and sometimes the water level is even 10 meters above the level of the surrounding plains. Therefore, once a bankruptcy occurs, the consequences will be disastrous. In mid-July, the embankment of the Yellow River collapsed and flooded