摘要
间歇性洪涝灾害与持续性泥沙淤积是民国时期洞庭湖政区变动与边界类型构建的关键因素。民国时期长江上游泥沙淤积至洞庭湖中部、西南部、东部,新淤洲土引发利益纠纷。为解决纠纷,1947年,南京国民政府决定仿清末设置南洲直隶厅的经验来筹设东湖设治局,但因湘、资二水影响而设置未成。在边界类型构建上,民国洞庭湖政区边界可以分为以河为界、以堤为界、以湖为界、以高辨识度的地物为界四种类型,而这无疑是民国洞庭湖区空间地理基础与人为政治过程不断互动调适的结果,也是洞庭湖区“地理特性”的重要象征。
Intermittent flood disasters and persistent sediment stasis are the key factors for changes in the administrative district of Dongting Lake during the Republic of China period.During this period,the siltation of sediment from the upper reaches of the Yangtze River accumulated in the central,southwestern and eastern part of Dongting Lake,and the newly silted continental soil triggered disputes on interests.In order to solve the dispute,the Nanjing national government decided to set up the East Lake Administration Bureau in 1947,following the experience of setting up the Nanzhou directly affiliated authority in the late Qing Dynasty,but it failed due to the influence of Xiang and Zi waters.In terms of the construction of the border type,the boundary of the Dongting Lake administrative District of the Republic of China can be divided into four major types:river as boundary,dike as boundary,lake as boundary,and highly recognisable features as boundary,which is undoubtedly the result of the continuous interaction and adaptation between the spatial geographic basis and man-made political process of Dongting Lake area during the Republic of China period,and also an important symbol of the "geographic characteristics" of Dongting Lake area.
作者
粟黎源
王春霞
SU liyuan;WANG Chunxia(College of History of Renmin University of China,BeiJing,100872,China;Law School of Zhejiang University of Finance and Economics,Hangzhou,Zhejiang 330100,China)
出处
《城市学刊》
2024年第3期85-94,共10页
Journal of Urban Studies
关键词
民国
洞庭湖
政区变动
边界类型
Republic of China
Dongting Lake
changes in administrative districts
boundary types
作者简介
粟黎源(1997-),男,湖南泸溪人,硕士研究生,主要从事历史政区地理研究;王春霞(1975-),女,浙江杭州人,副教授,硕士生导师,主要从事社会(工作)史研究。
