摘要
漳河是海河水系重要的支流。历史时期,在自然环境与人为因素的共同作用下,漳河平原段具有易淤、易决与易徙等特征。本文以明清(1368-1911年)为研究时段,对漳河的变迁过程进行了尽可能具体、详细的复原和定位。并在此基础上,探讨了漳河变迁的特点与规律。
The Zhanghe River is one of the major branches of the Haihe River and the section on the Hebei Plain is featured of fast filling--up, frequent bank failure and water course diversion. Taking the Ming and Qing dynasties （1368-1911） as the time window, the author gives a specific and detailed restoration and location to the river course diversion process of it. Further, the vivid characteristics and regular rules of its diversion are generalized.
出处
《中国历史地理论丛》
CSSCI
北大核心
2006年第3期27-35,共9页
Journal of Chinese Historical Geography
关键词
明清时期
漳河平原段
河道变迁
“引漳济运”
the Ming and Qing Dynasties
the Plain Section of the Zhanghe River
Water Course Diversion
Water Diversion from the Zhanghe River into the Grand Canal
