摘要
明清时期,通州是大运河北端的漕运枢纽,漕运物资悉经通州码头转运至北京。由于通州一带土质松软,水道迁徙频繁,对漕运码头影响巨大。在自然水道自身变化和人力整治的叠加作用下,通州运河水系格局屡有变迁,位于通州附近的运河码头分布和功能也随着水系格局改变而迁移和调整。本文从分析明清时期通州运河水系格局变迁入手,梳理通州码头兴衰起伏和迁移分布过程,以阐述河道变迁与通州漕运码头之间的依存关系。通州码头变迁实际上是人与自然之间互相作用,互相影响的结果。
Tongzhou was the pivot of water transportation of grain to Beijing at the north end of the Great Canal during Ming and Qing dynasty. Because the change of water system in Tongzhou area took place frequently,which played an important role on wharfs in tongzhou, wharf group changed in Tongzhou accordingly. This article has a study of changes of the water system in Tongzhou and the rise and decline of wharf group and its distribution . This article arrives at the conlusion that changes of wharf group in Tongzhou during Ming and Qing dynasty was impeted by both human activities and natural transformance of water system.
出处
《中国历史地理论丛》
CSSCI
北大核心
2013年第1期107-116,共10页
Journal of Chinese Historical Geography
关键词
明清
通州
水系变化
码头
迁移
Ming and Qing dynasty
Tongzhou
change of water system
wharf
ditribution
