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作 者:吕小琴 Lv Xiaoqin(Henan Normal University,Xinxiang 453007,China)
机构地区:[1]河南师范大学历史文化学院,河南新乡453007
出 处:《河南师范大学学报(哲学社会科学版)》2024年第5期103-109,共7页Journal of Henan Normal University(Philosophy and Social Sciences)
基 金:国家社会科学基金项目(23BZS072);教育部人文社会科学重点研究基地重大项目(23JJD70002)。
摘 要:食盐需求相对稳定,但无论是地质缓慢的演变,还是极端天气的巨大破坏,都会或长期或短期、程度不一地影响盐业生产,进而影响引地食盐的供给,继而催生引地调整的需求。河南解盐引地在明清五百余年间共经历四次调整。从表面上看,是灾害导致了引地食盐产量、质量和价格的变动,其深层原因则是在人为和自然长期相互作用下河东盐池环境变迁造成的负效应累积。引地是食盐专卖体制的基本制度,明清河南解盐引地调整,体现了明清盐业国家治理中“刚性”体制与“弹性”机制的有机结合。The demand for salt was relatively stable.However,whether it was the slow geological evolution or damage caused by extreme weather,they would affect salt production in varying degrees,in the long or short term,and thus affect supply of salt,which would stimulate the demand for adjustment.Henan xie-salt limit underwent four adjustments during more than 500 years of the Ming and Qing dynasties.On the surface,this was the result of changes in the production,quality,and price of salt in the affected areas caused by disasters.But the underlying reason was the accumulation of negative effects caused by the long-term interaction between humans and nature in the environmental changes of the Hedong Salt Lake.Salt limit was the basic system of the salt monopoly system.The adjustment of salt introduction in Henan reflected the organic combination of the“rigid”system and the“flexible”mechanism in the national governance of salt industry.
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