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近代以前,治河方略大致经历了以下几个时期和转变:大禹疏导和不与水争时期及向宽河调洪的转变;王景筑堤束水宽河调洪时期及向以水攻沙的转变;潘季驯筑堤束水以水攻沙时期及向上中下游治理的转变;李仪祉上中下游治理时期。大禹治水传说甚广,王景治水史载不详,只以治功见世。唯潘季驯与李仪祉均因其科学地回答了治河的理论基础、治河方法而对后世产生了巨大的影响。他们都认为黄河危害的根源在于泥沙。潘季驯主张以水攻沙,而李仪祉提
In modern times, the strategy of governing the river generally experienced the following periods and transitions: the change of Dayu to divert and not to flood and the flood diversion to the Kuan River; Transition; Pan Ji tamer embankment water to attack the sand and up the middle and lower reaches of governance changes; Li Yizhi upper and lower reaches of the governance period. Dayu flood legend is very wide, Wang Jingzhi water history is not known, only to see success. Only Pan Ji-tai and Li Yi-shek both had a huge impact on future generations because of their scientific answer to the rationale for governing the river. They all think the root cause of the Yellow River damage is sediment. Pan Taming advocated water attack sand, and Li Yi Zhi mention