三角淀的形成与淤废过程研究  

Research on the Process of Formation and Dispearance of the Sanjiaodian

作　　者：王长松[1] 尹钧科[2] 

机构地区：[1]对外经济贸易大学公共管理学院,北京100029 [2]北京社会科学院历史研究所,北京100101

出　　处：《中国农史》2014年第3期104-111,共8页Agricultural History of China

基　　金：国家自然科学基金重点项目(41230634);国家自然科学基金项目(批准号41071074);教育部人文社会科学研究青年基金项目(13YJCZH166)

摘　　要：三角淀位于北运河、永定河、凤河等河流交汇的位置。元代三角淀开始形成;明代中期至清初,是三角淀的盛涨时期;清代中期,清廷对永定河下游筑堤束水,导致三角淀逐渐淤废。至民国年间,三角淀已经失去蓄洪沉沙的作用。三角淀的形成与消失的过程,是人与自然相互作用影响的经典历程。三角淀作为区域发展与开发自然过程中的一个焦点,它不仅在中国水利史上,而且在当今生态涵养修复的实践中,都拥有重要的历史与现实意义。Sanjiaodian is located at the confluence of Beiyun River, Yongding River and Feng River. Itstarted to form from Yuan Dynasty, reached its peak time during Mid-Ming Dynasty and Qing Dynasty, declined in Mid-Qing Dynasty because of the building of dikes on its downstream, and finally lose the function of flood storage during the Republic of China period. The process of its formation and disappearance is the result of interaction between human beings and nature. As a focus during the process of regional social development and the exploitation of nature, Sanjiaodian has great significance not only for the history of water conservancy, but also for the practice of today＇s ecological remediation.

关 键 词：三角淀 永定河 筑堤束水 淤积 

分 类 号：S-09[农业科学] K207[历史地理—历史学]