从良田到泽薮:南四湖“沉粮地”的历史考察

发布时间：2017-12-31 15:13

本文关键词：从良田到泽薮:南四湖“沉粮地”的历史考察　出处：《中国历史地理论丛》2014年04期 　论文类型：期刊论文

更多相关文章： 沉粮地 缓征地 南四湖 历史时期

【摘要】："沉粮地"前身是清康熙、乾隆时期的"沉地"、"沉田"、"水沉地亩"或"水深难涸地亩",民国初年始见"沉粮地"的称谓。"沉粮地"是官方认定的免税地,乾隆中期两次豁免赋税,赋予了其法定免税的财政属性。与"沉粮地"相对的是"缓征地",后者虽未经认定,仍保有纳税之名,但实际上也不纳税。"沉粮地"的形成深受黄运地区水环境变迁以及国家漕运政策、河工建设等因素的影响,其形成过程与南四湖的塑造过程同时进行,由此而发生的土地利用方式的变化,都是适应这一地区生态系统变化的结果。
[Abstract]:"sunk grain land" was the predecessor of the Qing Dynasty Kangxi, Qianlong period of the "deep land", "Shen Tian", "water sink mu" or "water difficult to dry acres." In the early years of the Republic of China, the title of "the land of grain sink" was first seen. "the land of heavy grain" was officially recognized as a duty-free place, and in the middle of Qianlong, there were two exemptions from taxation. It has given it the financial attribute of legal tax exemption. In contrast to the "land of sunk grain", the latter has retained the name of tax payment although it has not been identified. But in fact, there is no tax. The formation of "grain sink land" is deeply influenced by the changes of water environment, national water transport policy, river construction and other factors in the Yellow River transport area, and its formation process is carried out at the same time as the shaping process of the Nansihu Lake. The change of land use mode is the result of adapting to the change of ecosystem in this area.
【作者单位】：淮阴师范学院历史文化旅游学院;聊城大学运河学研究院;
【基金】：国家社科基金“明清黄运地区的河工建设与生态环境变迁研究”(11BZS078)
【分类号】：K29
【正文快照】： 。山东西南部的南阳、昭阳、独山、微山四湖,总称南四湖,但直到清代才连成一片。这一湖面扩展的过程,伴随着大量农田的淹没,造成了济宁、鱼台境内大片的“沉粮地”。关于“沉粮地”问题,早在20世纪40年代,侯仁之的硕士论文《续〈天下郡国利病书〉山东之部》,将其作为一条重要

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