济水千年变迁考  

Study on the Millennium Changes of the Ji River

作　　者：姜传岗 JIANG Chuan-gang(Jining Municipal Party School,Jining,272000 China)

机构地区：[1]中共济宁市委党校,山东济宁272000

出　　处：《聊城大学学报（社会科学版）》2024年第3期43-48,共6页Journal of Liaocheng University:Social Science Edition

摘　　要：济水是古代流经豫鲁两省的一条大河,其与江、河、淮并称"四渎"完全是古人根据当时的实际情况而定义的。现在学术界关于济水"以黄河水为源""不能独流入海""是黄河支流"等说法是不能成立的。自古以来,济水就是以济源的泉水为源头,又汇聚了豫北广大地区的地表水、独流入海而形成的一条大河。是清水,不是浊水,这同黄河水系有本质的区别。深入考察千年来豫北和鲁西南地区水系的衍变过程,才能真正找到济水消失的原因及其遗渎变迁的踪迹。The Ji River was a major river flowing through the provinces of Yu and Lu in ancient times.It,along with the Yangtze,Yellow,and Huai Rivers,was collectively known as the"Four Major Rivers,"a classification established by ancient people based on the prevailing geographical conditions of the time.The academic assertion that the Ji River"originates from the Yellow River","does not independently flow into the sea",or is a"tributary of the Yellow River"is untenable.Since ancient times,the source of the Ji River has been the springs of Ji Yuan,gathering surface water from the vast northern regions of Yu Province to form a major river that flows independently into the sea.It is characterized by clear water,dis-tinct from the sediment-laden Yellow River system.To truly understand the disappearance of the Ji River and the evolution of its tributaries over the millennia,a thorough investigation into the changes in the wa-ter systems of northern Yu and southwestern Lu regions is necessary.

关 键 词：济水 豫北地表水 济水遗渎 广济河 北清河 金堤河 

分 类 号：K928.4[历史地理—人文地理学]