摘要
伴随清代“海势东迁”进程的加快,长江口近口段的河口水域环境变化明显,径流与潮流交互作用,造成了江阴常熟段沿江沙洲在清末以前的坍涨无常。长江口江阴常熟段的沙洲在清末至民国初年表现出大面积淤成且相对稳定的状态,还渐现向南岸归并的趋势。起初沙洲上的开垦者多由垦地为田来维持基本的生活,但由于沙洲本身抵御天灾人祸的能力较差,加上官方的行政干预也相对薄弱,沙洲民众走出了一条凭借商品化的农业生产与不同副业的拓展配合,实现更充分开发沙洲目标的路子。
With the acceleration of the "eastward migration of the coastline"process in the Qing Dynasty,the environmental changes in the mouth of the Yangtze River estuary were significant,and the interaction between runoff and tidal currents caused the collapse and instability of sandbars along the Changshu section of Jiangyin until the end of the Qing Dynasty.The sandbars in the Changshu section of Jiangyin at the mouth of the Yangtze River showed a large area of siltation and relatively stable state from the late Qing Dynasty to the early Republic of China,and gradually showed a trend of merging towards the south bank.At first,most of the cultivators on sandbars relied on land reclamation to maintain their basic livelihoods.However,due to the poor ability of sandbars to resist natural and man-made disasters,coupled with relatively weak official administrative intervention,sandbar residents embarked on a path to achieve more comprehensive development of sandbars through commercialized agricultural production and the expansion and cooperation of different sidelines.
作者
王日根
江俊皓
WANG Rigen;JIANG Junhao
出处
《学术月刊》
CSSCI
北大核心
2024年第3期184-195,共12页
Academic Monthly
基金
国家社会科学基金重大项目“清代海疆政策与开发研究”(13&ZD093)的阶段性成果。
关键词
江阴
常熟
沙洲
区域开发
开发路径
Jiangyin
Changshu
sandbar
regional development
development path
作者简介
王日根,厦门大学历史与文化遗产学院教授(福建厦门361005);江俊皓,厦门大学历史与文化遗产学院博士研究生(福建厦门361005)。
