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作 者:张忠广[1,2] 尹建龙 Zhang Zhongguang;Yin Jianlong
机构地区:[1]安徽大学历史学院,合肥230039 [2]铜陵学院会计学院
出 处:《学海》2023年第5期211-216,共6页Academia Bimestris
基 金:国家社会科学基金重大项目“民国时期淮河流域灾害文献搜集、整理与数据库建设”(项目号:18ZDA196)的阶段性成果。
摘 要:早在西汉时期就有黄河入淮的相关文字记载,此后黄河入淮大致经历了从泛淮、侵淮到夺淮的过程。自1128年杜充决口黄河后,黄河开始了长达727年的夺淮进程,这一进程打乱了江淮地区原有水系,并对江淮地区水系进行了重新塑造。就河流环境而言,黄河夺淮使得江淮地区淮河、长江和运河水系发生变动,淮河入海水道和废黄河的形成均是黄河在江淮地区留下的印迹。就湖泊环境而言,黄河夺淮改变了江淮地区的湖泊环境,致使洪泽湖等湖泊潴水新生,也导致射阳湖等湖泊淤废消亡。As early as the Western Han dynasty,the Yellow River into the Huaihe River related written records,since then the Yellow River into the Huaihe River has roughly experienced from pan-huaihe,the invasion of Huaihe River to capture the Huaihe River continued to deepen the process.The 727-year-old 1128 of the Yellow River,which began when it burst at the mouth of Du Chong,disrupted the Jianghuai river system and reshaped the Jianghuai river system.In terms of river environment,the seizure of the Huaihe River caused changes in the Jianghuai Huai River River,the Yangtze River and the canal system.The formation of the Huai River River channel and the Waste Yellow River are both imprints of the Yellow River in the Jianghuai region.In terms of lake environment,the seizure of the Huai River by the Yellow River has changed the lake environment in the Jianghuai region,resulting in the rebirth of water retention in lakes such as the Hongze Lake River and the siltation and extinction of lakes such as Sheyang Lake.
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