镇江水环境变动与城市空间演进(1805—1928)  

Changes of Water Environment and Urban Spatial Evolution in Zhenjiang from 1805 to 1928

作　　者：王硕 Wang Shuo(College of Humanities,Shanghai Normal University,200234)

机构地区：[1]上海师范大学人文学院,上海200234

出　　处：《中国历史地理论丛》2024年第4期101-111,共11页Journal of Chinese Historical Geography

基　　金：国家社会科学基金重大项目“7—20世纪长江三角洲海岸带环境变迁史料的搜集、整理与研究”(20&ZD231)。

摘　　要：通过对近代镇江水环境与城市空间演变过程进行历时性复原发现,清初已降,随着长江镇扬河段主泓逐渐北徙,江道南侧发生持续性的泥沙落淤与沙洲并岸现象,导致镇江城市水网与沿江河道不断淤浅,丰水环境彻底改变。为保障商贸活动正常运转,镇江沿岸港口设施与商业活动被迫向下游迁移,进而引发城市江岸活动空间自西向东扩展。近代镇江城市江岸空间东移反映了水环境要素变动对城市空间演进的影响,揭示了长江主泓周期摆动下人类活动的响应过程。Through the diachronic restoration of water environment and urban spatial evolution process of Zhenjiang(镇江)in modern times, this paper found that the phenomenon of continuous sediment deposition and bank consolidation occurred in the south side of the river in the early Qing dynasty with the gradual northward movement of the main flow of Zhenyang Reach of the Yangtze River. It resulted in continuous silting of urban water network and river channels along the river in Zhenjiang, and the thorough change of water environment. In order to ensure the normal operation of commercial activities, the port facilities and commercial activities along the Zhenjiang River were forced to move downstream, which led to the expansion of urban activity space from westward to eastward. The eastward movement of urban riverbank space in Zhenjiang reflected the influence of water environment elements changes on urban spatial evolution, and revealed the response process of human activities under the cyclic swing of the Yangtze River.

关 键 词：镇江 城市空间 镇扬河段 水环境 

分 类 号：K928[历史地理—人文地理学]