明清时期吴江蓄泄水环境与田土变化  

The Environment respecting Storage and Discharge of Water and Farmland Change in Wujiang in Ming and Qing

作　　者：敬淼春 胡火金[2] JING Miaochun;HU Huojin

机构地区：[1]复旦大学历史地理研究中心,200433 [2]苏州大学社会学院,215006

出　　处：《史林》2023年第2期116-125,219,共11页Historical Review

基　　金：国家社会科学基金重大招标项目“9—20世纪长江中下游地区水文环境对运河及圩田体系的影响”(项目批准号:18ZDA178)阶段性成果。

摘　　要：明清时期太湖泄水总体趋向东南,改变了吴江水环境的蓄泄状况,陆域被水网密集分割,形成以亚江、亚湖及诸多荡、漾、港为主体的水网环境。水网密化使得河湖水域的蓄泄功能逐渐明显,水流与泥沙动力条件的变化导致田土格局发生变化。在官民对待围田态度及相关做法的博弈中,留淤促成田土扩张。密集水网造成的普遍化坍涨使得田土布局与面积呈现不定性变化,明代田土增加较多,清代趋于稳定。以蓄泄状况考察历史时期吴江水环境与田土变化的关系,对目前江南水乡农田基本建设及保护具有镜鉴意义。The present paper points out that,due to the increasingly complicated network of rivers in Wujiang region,the discharge and storage of water were functionalized and consequently brought changes to the existing farmland.Generally,according to the paper,farmland increased rapidly in Ming and then in Qing it was gradually stabilized.

关 键 词：吴江 蓄泄水环境 田土变动 

分 类 号：K248[历史地理—历史学]